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Ill., maps (some color), photographs; Includes financial documents, organization chart, photographs, maps, water quality reports, and agricultural economics; Includes index; Title covers: calendar years ...
Citation Citation
- Title:
- Project history: Klamath Project, Oregon-California, 1964
- Author:
- United States. Bureau of Reclamation
- Year:
- 1964, 2008, 2006
Ill., maps (some color), photographs; Includes financial documents, organization chart, photographs, maps, water quality reports, and agricultural economics; Includes index; Title covers: calendar years for 1963-; Some issues are missing.; Description is based on: Project history: Klamath Project, Oregon-California 1963; Dates of the beginning year(s) of publication are derived from the May 1, 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project annual history for 1945, dated December 1, 1946
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Title from Web page (viewed on October 12, 2004).; "July 2004." ; Includes bibliographical references.
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"March 2005." ; "GAO-05-283."
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"Reprinted May 2003."; Includes bibliographical references; Also available at http://eesc.oregonstate.edu/agcomwebfile/edmat/html/sr/sr1037/sr1037.html
Citation Citation
- Title:
- Water allocation in the Klamath Reclamation Project, 2001 : an assessment of natural resource, economic, social, and institutional issues with a focus on the Upper Klamath Basin
- Author:
- Braunworth, William S.
- Year:
- 2003, 2004
"Reprinted May 2003."; Includes bibliographical references; Also available at http://eesc.oregonstate.edu/agcomwebfile/edmat/html/sr/sr1037/sr1037.html
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SUMMARY AND CONCLUSIONS Klamath Project is a $13 million Federal investment in water resource development, About 200,000 acres are irrigated and gross crop production (has exceeded $17 million each year ...
Citation Citation
- Title:
- Reclamation accomplishments, 1905-1953, Klamath Project, Oregon-California
- Author:
- Strantz, Maurice K.
- Year:
- 1953, 2005
SUMMARY AND CONCLUSIONS Klamath Project is a $13 million Federal investment in water resource development, About 200,000 acres are irrigated and gross crop production (has exceeded $17 million each year over the past 7 years. The Project encompasses the largest single block of irrigated land in the area and includes nearly half the three-county total irrigated area and one quarter of the cropland. Agriculture and manufacturing directly contribute half the three-county personal income and provide half the jobs. Klamath Project accounts for five-sixths of the gross income from crops, and half the total agricultural production in the three-county area. Personal income from project crops is estimated at $10.6 mil1ion in 1948. Recent crop production on the project supports directly or indirectly about $25 million in local personal income. Federal contribution for irrigation to repay costs without interest to date amounts to about $10.8 million. Annual personal income generated by project in the postwar years equals this assistance Project gross crop production of nearly $300 million over 46 years. Project farm income supports substantial portion of area retail trade and contributes to transportation and other services. Project agriculture in past 10 years increased its support to the economy and has helped offset the declines in the lumber industry. Without the project only about 50,000 irrigated acres would have been developed and the agricultural economy would have produced crops worth only about l/7th as large as at present. Reclamation development tends to maintain a stable prosperous economy in the three-county area.
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Pamphlet, compiled by the Klamath County Agricultural Agent, describing the history and status of the Klamath Project
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Foreword The Soil Survey of Klamath County, Oregon, Southern Part, is the product of many soil scientists, plant specialists, soil engineers, extension specialists, land owners, and others who worked ...
Citation Citation
- Title:
- Soil survey of Klamath County, Oregon, southern part
- Author:
- Cahoon, Joe
- Year:
- 1985, 2006, 2005
Foreword The Soil Survey of Klamath County, Oregon, Southern Part, is the product of many soil scientists, plant specialists, soil engineers, extension specialists, land owners, and others who worked and cooperated as a team to complete this project. In this report are many kinds of basic information about the soils in the area. This information can be helpful in making decisions about the management of irrigated soils for optimum crop production, in planning land uses for urban and suburban areas, and in determining the needs for many other uses, for example, forestry, range, wildlife, and recreation. This soil survey has been prepared for many different users. Farmers can use it to help select the most suitable crop for the kind of soil; ranchers can use it to determine amount of forage production and the kinds of plants most suited to range or woodland; foresters can use the survey to find information about kinds of trees, potential for tree growth, and special soil features.
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Thesis (B.A.) -- Whitman College, 2002; Includes bibliographical references (leaves 79-83)
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Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's ...
Citation Citation
- Title:
- Farming practices and water quality in the Upper Klamath Basin : final report to the California State Water Resources Control Board : 205j program
- Author:
- Danosky, Earl; Kaffka, Stephen
- Year:
- 2002, 2007, 2006
Summary The Upper Klamath Basin (UKB) is a high desert region straddling the California-Oregon border east of the Cascade Range. Irrigation and other agricultural practices in the U. S. Bureau of Reclamation's Klamath Project may result in impaired surface water quality, reducing its use for wildlife and fish in important national wildlife refuges that receive drainage water from farms, and in the Klamath River. By 2004, a system of total maximum daily loads (TMDL) for nutrients must be established for the Klamath River. To investigate the relationships among agricultural practices and surface water quality in the Upper Klamath Basin, a two year reconnaissance survey of surface water and agricultural tile drain locations, focusing on nitrogen and phosphorus concentrations and mass transfers was conducted. Data was collected at 18 surface locations and 10 tile drain locations. Triplicate samples were taken every ten days during the growing season (April through October) and one or two times a month during the remainder of the months, depending on opportunity. No samples were taken from tile drains during the winter months because there was no irrigation and drainage during that period. Water samples were analyzed for phosphorus (total P, soluble reactive P, total filterable P, and particulate P) and nitrogen (total N, soluble N, Soluble organic N, total filterable N, particulate N, and ammonia N), temperature, pH and electrical conductivity, a measure of salinity or total dissolved solids. Analyses of data, including data quality, estimates of the transfer of nutrients in surface waters in the region, and hypotheses about the relationship between agriculture and water quality are reported. 1. The salt and nutrient content of surface waters increases nearly threefold as water moves through the watershed from the Lost River and J canal diversion to the Klamath Straits Drain. Mean ECW levels in input waters at the J canal diversion were approximately 250 \iS cm1, while water sampled at the D pump increased to 600 ^S cm"1 on average over the sample period. By the time water reenters the Klamath River, salt concentrations have increased to approximately 700 jaS cm1. 2. The ECW values observed in subsurface tile drains were higher on average than in input waters and surface waters elsewhere in the region, especially in the Lease Lands area of the Tulelake Irrigation District (TID). ECW values averaged approximately 2,500 ^S cm"1 . Recycling irrigation water through soils in the TID increases the salinity of the water, especially by the time it reaches and is reused in the Lease Lands area of the Tulelake National Wildlife Refuge (TLNWR). Soils in this part of the Klamath Project area are naturally high in salt. 3. Water temperatures in agricultural subsurface tile drains were significantly lower than surface water temperatures during the growing season when tile drains were active. pH values in tile drains were lower than surface water values. The temperature and pH of tile drains does not influence surface water values. 1. 4. For total phosphorus (TP) input waters at the J canal irrigation diversion for the TED averaged approximately 0.27 mg L1 for the two years reported. Water leaving the Tulelake Sumps at the D pump increases to 0.33 mg L1. Water leaving the Lower Klamath National Wildlife Refuge (LKNWR) sampled at the start of the Klamath Straits Drain, averaged 0.33 mg L1, similar to those at the D pump. TP increased further to 0.40 mg L"1 a the end of the Klamath Straits Drain. The overall increase in P concentration in surface waters was much less than for salt, suggesting that processes other than simple enrichment are occurring, particularly those associated with the exchange of sedimentary P and aquatic plant species. TN increases from 2.3 mg L"1 to 4.0 mg L1 over the same pathway. Atomic ratios (TN:TP) of surface water samples remain constant at approximately 10:1 throughout the system, suggesting that the amount of sediment and other small particulate matter in surface waters affects the values observed. The amount of sediment is influenced in part by the agitation of surface water as it passes through pumps and over weirs. 5. The average seasonal TP value in tile drains beneath farm fields is approximately 0.34 mg L"1 . While average total P values in subsurface tile drains were not different from those found at the D pump and the LKNWR outlet, the range in values was great (0.1 to 0.8 mg L1). Similarly, high NO3 -N values were observed at times in tile drains. Very high values in tile drains lead to the inference that some fertilizer N and P is lost in drainage water, combined with nutrients derived from decaying soil organic matter. The amount estimated as lost is much less than the amount of surplus fertilizer P applied and the amount of P surmised to be mineralized from decaying soil organic matter. P from fertilizer and decaying organic matter appears to be accumulating in soils and lake sediments in the region. 6. Ammonia N concentrations are at or below the limit of detection in subsurface agricultural tile lines and one to two orders of magnitude below the values observed in surface soils. Un ionized ammonia increases with temperature. Values above 0.25 mg L1 were observed in late summer at several locations. 7. Some leaching of soluble salts and nutrients is unavoidable when crops are irrigated. P fertilizer is applied at rates higher than crop removal, while fertilizer n is applied at rates less than crop removal. Reduced fertilizer use can help bring P inputs and outputs into balance and may reduce further any avoidable losses of P. This objective should be the subject of an agronomic research program in the region. 8. Surface waters entering the TDD, the TLNWR, and the LKNWR are already enriched with N and P. It seems unlikely that reducing N and P losses from farming in the TID, if possible, would influence surface water quality sufficiently to make them significantly less eutrophic. For P, the hypothesized threshold concentration limiting algae growth in fresh waters is 5 to 25 times smaller than the values observed in waters entering the TID for irrigation use. The addition of 1. nutrients from agriculture probably does not influence significantly surface water quality in the region. Wetland sediments, large amounts of organic matter in soils, and water introduced for irrigation contain essentially unlimited amounts of nutrients for aquatic plant growth. It is not clear how this circumstance could be changed under any reasonable time frame, if ever. 9. Using a TMDL approach may not result in reduced amounts of nutrients returned to the Klamath River because wetlands and farming practices in the southern portion of the Klamath Project result in the net removal of nutrients from the waters diverted for irrigation on a yearly basis, compared to allowing the same amount of water simply to flow down the river unused. Because of large errors of estimation for the amounts of water transferred, combined with smaller errors associated with estimating nutrient concentrations in water samples, and with year to year climate variation, TMDLs may not be an effective or efficient means of reducing nutrients in return flows to the Klamath River. Rational confidence limits for TMDLs may have to be too broad to be effective. Recycling of some drainage water for irrigation would reduce the amount of nutrients returned to the river more effectively than implementing a TMDL program.
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EXECUTIVE SUMMARY This document describes the rationale for and implementation of an Integrated Land Management (ILM) Plan for the Tule Lake National Wildlife Refuge (NWR). The proposal is the recommendation ...
Citation Citation
- Title:
- Integrated land management on Tule Lake Wildlife Refuge: an alternative management strategy developed by the Integrated Land Management Working Group: promoting productive wetland habitats and sustainable agriculture on Tule Lake National Wildlife Refuge
- Author:
- Integrated Land Management Working Group (Tule Lake National Wildlife Refuge, Calif.)
- Year:
- 2000, 2006, 2005
EXECUTIVE SUMMARY This document describes the rationale for and implementation of an Integrated Land Management (ILM) Plan for the Tule Lake National Wildlife Refuge (NWR). The proposal is the recommendation of 5 representative stakeholders in the Tule Lake area. During the 1950fs, 1960fs, and early 1970's, Tule Lake NWR was considered the single most important waterfowl refuge in North America when peak populations exceeded 2.5 million ducks and 1.0 million geese. The Kuchel Act of 1964 was enacted to preserve these waterfowl values as well as the local agricultural economy dependent on Refuge lands. However, restrictive management of wetlands and water levels under the Kuchel Act has eliminated the ecological processes critical to the Refuge's sustained wetland diversity and productivity. Currently, Tule Lake NWR supports a fraction of its past waterfowl use, species diversity has declined, and its value to endangered species has diminished. Agricultural sustainability is also thre
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12. [Image] Empire building
Article on the history and future of the agricultural settlement of the desert regions of the western United States. Includes a black and white photograph of Thousand Springs, Idaho.Citation -
SUMMARY To provide a basis for negotiations of a repayment contract with an irrigation district representing the water users of the Tule Lake Division of the Klamath Project, this report has been prepared. ...
Citation Citation
- Title:
- Report on payment capacity for Tule Lake irrigation district, Klamath Project
- Author:
- Best, R.R.
- Year:
- 1948, 2004
SUMMARY To provide a basis for negotiations of a repayment contract with an irrigation district representing the water users of the Tule Lake Division of the Klamath Project, this report has been prepared. It covers past, present, and anticipated future agricultural and economic conditions and substantiates the proposed district's capacity to repay construction costs for irrigation water as well as to meet operation and maintenance charges It has been prepared according to procedures and policies established pursuant to the Federal Reclamation laws (Act of June 17, 1902, 32 Stat. 388, and acts amendatory thereof and supplementary thereto.) In general, a representative farm budget method of analysis was employed to determine the payment capacity* Gross income of the land was based upon average per acre yields in the area and 1939-44 prices received. Prices of certain crops were adjusted further in accordance with long term outlook for these crops. From the gross income, all farm operating and retention expenses, including cultural and harvesting costs, taxes, insurance, depreciation and replacement, interest on investment, and a reasonable allowance for family living predicated upon the same base period (1939-44) have been subtracted to arrive at payment capacity. Individual consideration has been given to the block of land entered prior to 1948 (the major portion of the area), the lands of the Coppock Bay Area which are principally Class 2, and the undeveloped lands of the area just south of Malin, Oregon, Area C, Plate 1. The annual payment capacity of the irrigable lands entered prior to 1914-8, is determined to be approximately $50 per acre. The Class 2 lands of the Coppock Bay Area are shown to have a payment capacity of $21 per acre, as a result of slightly higher operating costs and probable lower yield or quality of certain crops. For the undeveloped area just south of Malin, Area C of Plate 1, the payment capacity is determined at $18 per acre after development to the extent expected under settlement and development plans currently being formulated The weighted average payment capacity for these areas is calculated to be $26.25 per acre. There is no need for a development period for the lands of the Tule Lake Division, except for the latter area as indicated above. Furthermore, after liberal allowance for farming costs and a reasonable family living, the resulting payment capacities appear to be well in excess of any annual installments likely to be considered necessary for repayment of the District's construction obligation and operation and maintenance charges.
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14. [Image] Evaluation of instream fish habitat restoration structures in Klamath River tributaries, 1988/1989
Annual Report For Interagency Agreement 14-16-0001-89508 EVALUATION OF INSTREAM FISH HABITAT RESTORATION STRUCTURES IN KLAMATH RIVER TRIBUTARIES 1988/1989 by A.D.Olson and J.R. West USDA-Forest Service, ...Citation Citation
- Title:
- Evaluation of instream fish habitat restoration structures in Klamath River tributaries, 1988/1989
- Author:
- Olson, A. D.
- Year:
- 1989, 2008, 2006
Annual Report For Interagency Agreement 14-16-0001-89508 EVALUATION OF INSTREAM FISH HABITAT RESTORATION STRUCTURES IN KLAMATH RIVER TRIBUTARIES 1988/1989 by A.D.Olson and J.R. West USDA-Forest Service, Klamath National Forest 1312 Fairlane Road, Yreka, CA 96097 ABSTRACT Ten instream fish habitat techniques were evaluated to determine which most effectively restored salmonid spawning and/or rearing conditions. Structure stability was estimated based on how intact each structure remained (by percent) and its age, we then projected useful life for each structure type. Cost in 1989 dollars was used to determine cost per unit habitat area provided. Observed use by spawners was used to estimate total number of redds per structure (over its life). Cost of providing spawning habitat (cost per redd) was calculated by dividing estimated total redds by structure cost. Habitats resulting from instream structures were classified using the modified Bisson method and we determined the influence zone of each structure using physical variables to define habitat area. Structures were biologically sampled using direct underwater observation techniques described by Hankin and Reeves1 (1989). Two person dive teams used a "two-pass" method to enumerate and classify salmonids by species and age-class (0+, 1+ or older juveniles, and adults), noting the presence of other species. Fish use of structure affected habitat (post-modification) was compared to use of habitats like those present prior to structure placement (pre-modification). Comparison of "pre-modification" and "post-modification" fish standing crops resulted in a "net fish difference" which was divided by structure cost, yielding "cost per fish reared11. Boulder weirs, the most expensive structures investigated, did not affect enough surface area to make cost per unit of affected habitat reasonable. Cabled cover logs and digger logs (lowest cost structures) were very cost effective at altering physical habitat condition. We believe cost of physically modifying habitat area is only one factor that is important enough to effect success or failure of a large scale habitat restoration program. Assuming all other factors are of equal weight, lowest cost structures can provide the "best value". Modification prescribed to restore stable spawning habitat needs close scrutiny. We believe it is essential to know how the existing habitat is used by spawners by conducting spawning area use surveys which identify redd location and quantify habitat available during each spawning period. Boulder deflectors were best utilized by Chinook salmon spawners, however chinook spawner use of "traditional" structures (weirs backfilled with gravel) was disappointing. Backfilling of instream structures with suitable gravel is a practice that should be discontinued. Steelhead spawner use of structures which result in "pocket water" type spawning areas were heavily used. This habitat configuration proved most desirable when woody object cover was readily available to the spawners. The highest steelhead spawner use was associated with boulder groups with wood and boulder/rootwad groups. We found rearing structures which provided high habitat and cover diversity received the best response from juvenile fish. We observed fish use over one summer and saw dramatic unpredictable use changes even through this short time period. Fish rearing needs during other seasons may differ substantially from summer needs, therefore, suitability of modified habitat probably also changes. Digger logs, one of the least costly and simplest structures, provided the best increase in fish standing crop (fish/m2) for the lowest cost. We believe digger logs were well used by rearing fish because they are one of the most natural restoration structures investigated. Other structures which were well used (small weirs, deflectors, and boulder groups with attached wood) also seem to closely duplicate naturally productive habitats. Higher velocity habitat types associated with boulder groups with wood, boulder rootwad groups, and boulder deflectors were selected by juvenile steelhead and chinook salmon. Providing overhead cover, especially if it extends into the water where it may also be used as object cover, seemed most valuable for juvenile steelhead and salmon if it was placed in a habitat type which would normally receive high fish use. Placement of object cover in slow velocity areas (pool and glide edges) had questionable value for summer rearing habitat restoration, however we do not know what value these structures may have during colder water high flow periods when fish seek slow velocity, densely-covered habitats. We defined the most cost effective method as one meeting restoration objectives, providing the greatest increase in fish use (per surface area or volume), over the longest time period, for the lowest cost. We rank structures evaluated in this study (from most cost-effective to least cost effective) as follows: Digger Logs, Boulder deflectors, Small Boulder Weirs, Boulder Groups with Woody Cover, Free Boulder Weirs, Large Boulder Weirs, Boulder Groups, Boulder/Rootwad Groups, Boulder/Rootwad Deflectors, Small Boulder Weirs, and Cabled Cover Logs.
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15. [Image] Upper Klamath Basin : opportunities for conserving and sustaining natural resources on private lands
1 i California Oregon Cover Photo: Lower Klamath National Wildlife Refuge at sunset Tupper Ansel Blake/ USFWS Map Detail Area: Upper Klamath River Basin ii T he Klamath River Basin presents numerous ...Citation Citation
- Title:
- Upper Klamath Basin : opportunities for conserving and sustaining natural resources on private lands
- Author:
- United States. Natural Resources Conservation Service
- Year:
- 2004, 2005
1 i California Oregon Cover Photo: Lower Klamath National Wildlife Refuge at sunset Tupper Ansel Blake/ USFWS Map Detail Area: Upper Klamath River Basin ii T he Klamath River Basin presents numerous challenges as well as opportunities for its many water users. For years, farmers and ranchers in the basin have recognized the vital role they play in the health of their watershed. Working with conservation districts, the Natural Resources Conservation Service ( NRCS) and others, land managers continue to proactively find ways to enhance natural resources in the basin, benefiting wildlife and the environment. However, as it has across the western United States, drought hit home in the Klamath for those who depend on every drop of water to sustain their livelihood, culture and community. In the spring of 2001, the combination of drought and the impact of the Endangered Species Act triggered a shutdown of irrigation water during the growing season, drying up water resources to more than 2,000 farms and ranches. NRCS, in cooperation with local conservation districts, provided a quick infusion of technical assistance and $ 2 million in cost- share funding for cover crops through the Emergency Watershed Protection Program. As cover crops took hold, the seeds of a long- term solution took root in the NRCS/ conservation district partnership. The ability of the local office to receive funding, engage community members and other partners, plan resource improvements, implement actions, and monitor success proved to be an invaluable asset for the community. Helping private landowners develop and apply practical, common- sense solutions to complex resource issues will be the challenge of the conservation partnership well into the future. USDA, in concert with the locally led conservation districts, will continue to play a critical role by delivering technical and financial assistance to Klamath Basin farmers and ranchers. The Rapid Subbasin Assessments that follow are the first step in that process. The assessments are designed to help local decision- makers determine where investments in conservation will best benefit wildlife habitat, agriculture and other land uses in a compatible manner. It is our goal to provide a comprehensive overview of resource challenges and opportunities in the basin, and help decision- makers to prioritize their investments in areas that will best sustain multiple use of natural resources in the basin now and in the future. Sincerely, Robert J. Graham Charles W. Bell, State Conservationist State Conservationist Oregon NRCS California NRCS iii iv Table of Contents Map of the Upper Klamath Basin ................................ i Letter from OR and CA State Conservationists .......... ii Overview of the Upper Klamath Basin ........................ 1 Background ................................................................................... 1 Upper Klamath Basin Description ............................................ 2 The Role of Agriculture in the Basin ........................................ 3 Rapid Subbasin Assessments ...................................................... 4 Private Lands Conservation Accomplishments ...................... 6 Summary of Conservation Opportunities ............................... 7 Water Conservation ...................................................................... 8 Improving Water Quality ........................................................... 10 Increasing Water Storage/ Yield ............................................... 11 Enhancing Fish and Wildlife Habitat ...................................... 12 Overview of Conservation Effectiveness .............................. 13 Comparative Benefit: Water Demand ..................................... 15 Comparative Benefit: Water Quality ....................................... 15 Comparative Benefit: Water Storage/ Yield ............................ 16 Comparative Benefit: Habitat/ Fish Survival .......................... 16 Sprague River Subbasin .............................................. 18 Resource Concerns & Conservation Accomplishments ...... 19 Conservation Opportunities ..................................................... 20 Williamson River Subbasin ......................................... 22 Resource Concerns & Conservation Accomplishments ...... 23 Priority Conservation Opportunities ....................................... 24 Upper Klamath Lake Subbasin .................................. 26 Resource Concerns & Conservation Accomplishments ...... 27 Priority Conservation Opportunities ....................................... 28 Upper Lost River Subbasin ......................................... 30 Resource Concerns & Conservation Accomplishments ...... 31 Priority Conservation Opportunities ....................................... 32 Middle Lost River Subbasin ....................................... 34 Resource Concerns & Conservation Accomplishments ...... 35 Priority Conservation Opportunities ....................................... 36 Tulelake Subbasin ...................................................... 38 Resource Concerns & Conservation Accomplishments ...... 39 Priority Conservation Opportunities ....................................... 40 Butte Valley Subbasin ................................................. 42 Resource Concerns & Conservation Accomplishments ...... 43 Priority Conservation Opportunities ....................................... 44 Upper Klamath River East Subbasin .......................... 46 Resource Concerns & Conservation Accomplishments ...... 47 Priority Conservation Opportunities ....................................... 48 1 Overview of the Upper Klamath Basin Upper Klamath Basin Quick Facts • The Upper Klamath Basin includes the Klamath, Williamson, Sprague, Lost, and Wood rivers, among others • Several state and federal wildlife refuges are a part of the Upper Klamath Basin • Migratory birds like the American White Pelican and the Red- necked Grebe use croplands in the Klamath Basin as a stop on the Pacific Flyway • Deer and elk graze on wheat and barley fields and pheasants use both crop and rangelands for their nesting and feeding grounds Background In a landscape formed by seemingly endless cycles of drought and flood, it’s no wonder that for hundreds of years, competition for water has dominated the landscape of the West. Stretching across southern Oregon and northern California, the Klamath Basin has become synonymous with the water challenges that western water users face. As one example, agricultural commodities that need irrigation water to thrive – providing Americans with the cheapest domestic food supply in the world, face competition from the critical water needs of sucker fish, salmon and other threatened and endangered species. While that competition is understandable, more and more, conservation leaders in all industries have come to recognize that these water needs aren’t necessarily at odds with one another, and can in fact be compatible. While an example of the challenges today’s agricultural producers and conservationists face, the Klamath Basin has emerged as an example of how diverse interests can work together successfully. 2 Overview of the Upper Klamath Basin Upper Klamath Basin Description The Upper Klamath Basin is an area of high desert, wetlands, and the Klamath River. The river extends 250 miles from its headwaters at Upper Klamath Lake in south central Oregon to the west coast of northern California. The Upper Klamath Basin includes the US Bureau of Reclamation’s ( USBR) Klamath Project Area and the drainage area above Irongate Dam on the Klamath River. The basin’s lakes, marshes, and wetlands host an abundance of plant and animal species and include national wildlife refuges, parks, and forests. Agricultural production began around the turn of the 20th century, and with the creation of the Klamath Irrigation District in 1905, water diversions for irrigation began in earnest. A portion of these irrigated lands are in the USBR’s irrigation project. The ‘ project area,’ as it is commonly called, includes 188,000 of the 502,000 acres of private irrigated land in the basin. This includes lands leased from the various wildlife refuges that are supplied with water by the USBR. Privately irrigated acreages can vary from year to year, depending on USBR contracts and annual cropping cycles. In comparison, the majority of the private irrigated land - about 314,000 acres - in the basin is located outside the project area. Upper Klamath Basin Quick Facts: • Over 2.2 million acres are privately owned in the Upper Klamath Basin • 188,000 of the irrigated acres are in the US Bureau of Reclamation’s Irrigation Project • Approximately 502,000 acres of privately owned lands are irrigated • 314,000 acres of irrigated lands are outside the Project area 3 Overview of the Upper Klamath Basin The Role of Agriculture in the Basin Agricultural lands play a key role in a healthy ecosystem. Located on the Pacific Flyway, migratory birds like the American White Pelican and the Red- Necked Grebe use croplands in the Klamath Basin as an important feeding and resting stop. Deer graze on wheat and barley fields, and pheasants use both crop and rangelands for their nesting and feeding grounds. Progressive conservation leaders recognize that farming and fish and wildlife habitat are not mutually exclusive. Well- maintained farmland creates fish and wildlife habitat, contributing to a healthy watershed. They also recognize that opportunities will always exist to improve the condition of natural resources in the basin. To address those opportunities, conservation leaders in Oregon’s Klamath Falls Soil and Water Conservation District and California’s Lava Beds/ Butte Valley Resource Conservation District have proactively identified four key priorities tied to natural resource conservation. The districts asked experts at the USDA’s Natural Resources Conservation Service to help them develop a plan to determine what could be done on- farm to conserve water, increase water storage, improve water quality, and enhance fish and wildlife habitat. While so much of the attention to date in the Klamath Basin has been focused on water demand, these conservation leaders recognize demand is only one piece of the puzzle. Comprehensive solutions must also address water quality, storage and wildlife habitat. Conservation District Priorities 1) Conserve Water 2) Increase Water Storage 3) Improve Water Quality 4) Enhance Fish & Wildlife Habitat 4 Rapid Subbasin Assessments Conserving natural resources is the ultimate goal throughout the basin, and its success hinges on long- term solutions. At the request of local conservation districts, NRCS undertook an 18- month study of resource concerns, challenges and opportunities throughout the Upper Klamath Basin. The study was not intended to provide a detailed, quantitative analysis of the impacts of conservation work, but rather, to provide an initial estimate of where conservation investments would best address the districts’ four priority resource concerns. Beginning in the spring of 2002, NRCS planners collected information to enable the conservation districts, agencies, organizations, farmers, ranchers and others to make informed decisions in a timely manner about conservation and resource management in the basin. These Rapid Subbasin Assessments are intended to help leaders set priorities and determine the best actions to achieve their goals. As a part of the rapid subbasin assessment process, eight subbasins were delineated ( see map at left). A watershed planning team traveled through each subbasin, inventorying agricultural areas, identifying conservation opportunities and current levels of resource management, and estimating the impacts of these opportunities on the Conservation in the Upper Klamath Basin 5 Conservation in the Upper Klamath Basin conservation districts’ priority resource concerns. They focused their recommendations on areas that would provide the best benefit to the wide array of stakeholders in the Upper Klamath Basin. They also identified a number of socio- economic factors that must be taken into consideration when helping producers adapt to new management styles and conservation activities. Through NRCS, conservation districts and other federal, state and local entities, private land managers are working to identify ways they can more efficiently use – and share – the water they need. In the face of increasingly complex and politically polarized circumstances, a clear purpose and direction has arisen. The commitment of the local conservation partnership to identify the impacts of water shortages and to find solutions that will improve natural resource conservation will be key to the long- term viability of both endangered species and industries in the Upper Klamath Basin. The information that follows provides a summary of the conservation challenges and opportunities that NRCS staff found in their assessment. Recommendations for where financial and other resources can best be invested to improve natural resources, while sustaining the economy of the Upper Klamath Basin, are also identified. 6 Conservation in the Upper Klamath Basin Private Lands Conservation Accomplishments One component necessary to understanding future conservation opportunities in the basin is to recognize the current conservation work of private land managers. An indicator of these efforts is the work that has been undertaken in partnership with NRCS and the local conservation districts. In federal fiscal years 2002 and 2003, Upper Klamath Basin farmers and ranchers improved resource conditions on 18,877 acres of privately owned agricultural lands, with assistance from NRCS and the conservation districts. During this time, private land managers have worked with the conservation districts in the basin to: • improve the condition of 11,800 acres of grazing lands • conserve water and improve water quality on 13,656 acres • restore and establish 4,138 acres of wetlands and riparian areas • improve 281 acres of forest stands • establish resource management systems on 1,351 acres of cropland These conservation efforts were accomplished with a combination of private, state and federal funding. 7 Conservation in the Upper Klamath Basin Summary of Conservation Opportunities In addition to recognizing current conservation activities, the assessments define what can be accomplished with a strong conservation partnership in the Upper Klamath Basin. All too often, the debate about multi- use of water in the basin has focused on ways to reduce water demand. However, the basin’s many water users - including fish and wildlife - benefit just as much from improvements to water quality, water storage and wildlife habitat. Taken together, the recommendations that follow seek to utilize a comprehensive approach to all four resource priorities - with the goal of contributing to a sustainable, multi- use water system. While quantification of the results of conservation work in these four areas is difficult, there is no question that a comprehensive approach to natural resource improvement in the Upper Klamath Basin will result in accumulative long- term benefits for endangered fish species, wildlife habitat, agriculture, urban and other water uses. Agriculture cannot undertake these efforts alone. Private landowners and the general public both benefit from natural resources conservation in the Upper Klamath Basin. Because of this, public and private sources of funding from in and outside the region are necessary. Solutions of this magnitude also come with other social, political, and cultural costs. Upper Klamath Basin Quick Facts: • 1,400 farm families live in the Upper Klamath Basin • The Upper Klamath Basin is home to sucker fish, bull trout and redband trout 8 Conservation in the Upper Klamath Basin For example, all stakeholders in the Upper Klamath Basin need to identify and address social, economic, and cultural resource- based values they have historically enjoyed. Politically, there must be resolution and agreement on water rights, endangered species, and water quality. Water Conservation Because few water use measurements have been taken in the past, it is difficult to quantify where specific water efficiencies can be gained. Throughout the Upper Klamath Basin, water that leaves one irrigated field generally re- enters streams or enters the groundwater, providing the opportunity for it to be utilized again later. Because of this, water delivery systems both in and outside the USBR project area are generally efficient. As a result, the most significant benefit of reducing water demand on individual farms is an improvement in water quality and reduction in water temperatures, rather than an increase in available water. 9 Conservation in the Upper Klamath Basin Conservation measures that reduce water demand on private agricultural lands can be accomplished in a variety of ways. New technologies for managing when and where water is applied on crop and pasture lands will help to ensure that water is only applied when it is of the best benefit to the plant. Water conservation opportunities include improving irrigation water-use efficiency, retaining and conserving drainage water, and making use of new technologies that more accurately forecast the impacts of drought and floods. The subbasin assessments indicate an opportunity to conserve water and improve water quality on 130,000 acres of irrigated lands within the USBR project. Outside the project area there is an opportunity for water conservation on approximately 220,000 irrigated acres. If all potential conservation practices are implemented on all irrigated lands, on- farm water use efficiency could increase by up to 25 percent in the Upper Klamath Basin. A potential two to five percent increase in water yield could be achieved by increasing management in upland range and forestland areas. In all cases, these are preliminary estimates and require validation. This estimate does not account for evaporation, transpiration, seepage or other loses that may occur at the sites receiving conserved water nor does it evaluate irrigation delivery or conveyance efficiencies. Tupper Ansel Blake/ USFWS 10 Conservation in the Upper Klamath Basin This level of water conservation cannot be reached without a concerted federal/ state/ private partnership that works together to apply water conservation practices in targeted areas throughout the Upper Klamath Basin. Improving Water Quality Water quality has a direct impact on many fish and wildlife species. Within the Upper Klamath Basin, most rivers and lakes do not meet federally mandated Clean Water Act standards for temperature, dissolved oxygen, pH, or other pollutants. Water quality is affected by water temperature, low in- stream flows and the condition of adjacent land riparian areas, among other items. Private landowners are just one of many groups who have an opportunity to improve water quality throughout the basin. Water quality improvement opportunities on private agricultural lands in the basin range from improving the management of livestock near streams and rivers to utilizing new technologies that track pest and weed cycles to ensure that pesticides are only applied when they will be most effective. Water conservation practices that reduce tailwater runoff from irrigated fields can provide extensive improvements in water quality. 11 Conservation in the Upper Klamath Basin Increasing Water Storage/ Yield In recent years, drought has been a large contributing factor to reduced water levels in the Upper Klamath Basin. One solution to address low water flows would be to store water for times of water shortage. There are at least two challenges to this solution: finding a place to store water and finding water to store. To evaluate this option, potential storage values were calculated for 41 years of record from 1961 to 2002. This analysis reinforced the observation that, as has been seen in recent years, drought years normally occur in a multi- year cycle. Because of this, in the years where extra water is most needed, it is often not available from previous years to store. One promising, small- scale, water storage solution may lie in subsurface irrigation water storage in suitable locations, such as the Tulelake Subbasin. In this scenario, there exists a potential to store water in the soil profile and reduce irrigation water demand during the irrigation season. Another option for subsurface storage of water includes the restoration of streams and their surrounding wetlands and riparian areas. This can increase the “ sponge” effect allowing for the slow release of water through the long, dry summer months. Tupper Ansel Blake/ USFWS 12 Conservation in the Upper Klamath Basin Enhancing Fish and Wildlife Habitat The Upper Klamath Basin is home to a wide variety of aquatic and terrestrial species of wildlife and fish. Much of the water used in the Klamath wildlife refuges and associated marshes, ponds, streams and wetlands originates in the Upper Klamath Lake Subbasin. The Klamath Basin wildlife refuges provide a stopover for 85 percent of the ducks, geese, and other birds that migrate through the Pacific Flyway from Alaska to South America. Streams in the Upper Klamath Basin provide spawning and rearing habitat to threatened and endangered suckers and bull trout, as well as redband trout, which is listed as a species of concern by the US Fish and Wildlife Service. Several streams are highly valued “ catch and release” sport fisheries. There is high landowner and public interest in restoring and maintaining riparian habitat along these streams. Many of the conservation opportunities outlined under water conservation and water quality provide direct benefits to fish and wildlife as well. In addition, creating and restoring wetland areas, planting trees and developing wildlife habitat along the edges of crop fields all contribute to enhancing wildlife habitat in the basin. Tupper Ansel Blake/ USFWS 13 Conservation in the Upper Klamath Basin Overview of Conservation Effectiveness In order for the Upper Klamath Basin to successfully move forward with solutions, agriculturists, environmentalists, Tribes, government agencies, organizations, and others need to develop unified leadership to arrive at a common vision for the future. In addition, stakeholders and others must commit to a long- term investment of public and private funding as well as other resources. Based on the Upper Klamath Basin Rapid Subbasin Assessments, the Oregon and California NRCS planning staff rated the potential benefit of recommended conservation practices and resource management systems based on the conservation districts’ four resource priorities. Many state and federal agencies have invested in conservation work throughout the basin. While the recommendations in this document focus on private land and agriculture, the assessments can also be applied to help prioritize conservation practices on other land uses basin- wide. Overall, based on the planning team’s analysis, conservation activities in the Sprague River Subbasin would produce the greatest benefit, and conservation practices in the Upper Klamath River East Subbasin would yield the least Tupper Ansel Blake/ USFWS overall benefit based on the conservation district’s priorities. 14 Conservation in the Upper Klamath Basin While recognizing that any science- based conservation focus in the Upper Klamath Basin would be beneficial, the charts on pages 18- 19 specifically focus on work that can be accomplished on private lands. They provide a breakdown of recommended conservation practices on each of the conservation districts’ priorities by subbasin. For example, the water demand chart shows that investing in conservation practices in the Sprague River Subbasin has the greatest potential for reducing agriculture’s water demand by implementing improved irrigation practices. The Sprague also provides the best opportunity to address water quality and wildlife habitat. Investment in conservation activities in the Tulelake and the Upper Klamath Lake subbasins offers the greatest potential to address water storage/ yield. Investing in Conservation: Enabling farmers, ranchers and other private land managers to successfully address the four resource priorities will require: • The adoption of conservation on 350,000 acres of private farmland, range, and forests, • Financial resources estimated at $ 200 million for installation and another $ 27 million annually to operate, and • Twenty or more years to complete with the current financial and technical resources available. Tupper Ansel Blake/ USFWS 15 Water Demand Comparative Benefit of Applied Conservation Practices by Subbasin Upper Klamath River East Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Williamson Upper Klamath Lake Upper Lost River Butte Valley Middle Lost River Tulelake Sprague Sprague Upper Klamath Lake Williamson Butte Valley Tulelake Middle Lost River Upper Lost River Upper Klamath River East Water Quality Comparative Benefit of Applied Conservation Practices by Subbasin Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Comparative Benefit: Water Demand The chart at left provides an overview of the comparative benefit by subbasin of various conservation practices that reduce water demand. Based on research completed by NRCS planning staff, the greatest potential to reduce water demand exists by implementing irrigation and riparian/ wetland conservation practices in the Sprague Subbasin. This is followed by implementing agronomic and irrigation conservation practices in Tulelake. There is no measurable water demand benefit achieved by implementing conservation practices in the Upper Klamath River East Subbasin. Comparative Benefit: Water Quality The chart at left provides an overview of the comparative benefit by subbasin of various conservation practices that improve water quality. Based on research completed by NRCS planning staff, the greatest potential to improve water quality occurs when riparian/ wetland, grazing and irrigation conservation practices are implemented in the Sprague Subbasin. In comparison, no measurable water quality benefits are achieved by implementing conservation practices in Butte Valley or the Upper Klamath River East subbasins. Conservation in the Upper Klamath Basin 16 Wildlife Habitat Comparative Benefit of Applied Conservation Practices by Subbasin Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Williamson Sprague Butte Valley Tulelake Middle Lost River Upper Lost River Upper Klamath Lake Upper Klamath River East Upper Klamath River East Williamson Sprague Upper Klamath Lake Tulelake Middle Lost River Upper Lost River Butte Valley Water Storage Comparative Benefit of Applied Conservation Practices by Subbasin Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Comparative Benefit: Water Storage/ Yield The chart at right provides an overview of the comparative benefit by subbasin of various conservation practices that enhance water storage and yield. Based on research completed by NRCS planning staff, the greatest potential to enhance water storage and yield occurs by implementing riparian/ wetland, forest and range conservation practices in the Upper Klamath Lake Subbasin. In comparison, the Tulelake Subbasin gains water yield through agronomic practices like subsurface drains to allow for winter irrigation. Overall, implementing forest and range practices in most subbasins will result in greater water yield within the soil profile and water table. Comparative Benefit: Habitat/ Fish Survival The chart at right provides an overview of the comparative benefit by subbasin of various conservation practices that improve wildlife habitat and fish survival. Based on research completed by NRCS planning staff, the greatest potential to improve habitat is in the Sprague Subbasin, using wetland/ riparian, forest, range and irrigation practices. In comparison, no measurable habitat benefits are achieved by implementing additional conservation practices in the Middle Lost River, Tulelake, Butte Valley or Upper Klamath River subbasins. Conservation in the Upper Klamath Basin 17 Tim McCabe/ NRCS 18 The Sprague River Subbasin is located 25 miles northeast of Klamath Falls and covers approximately 1.02 million acres. Forested mountain ridges enclose the Sprague River Valley, which includes large marshes, meadows and irrigated pasture. Juniper and sagebrush steppes dominate rangeland. Irrigated Pasture is the predominant land use in the Sprague River Valley. Approximately 65 percent of the water used for irrigation is diverted from streams, and 35 percent is pumped from wells. Flooding is the most common form of irrigation. Most diversions do not have fish screens and lack devices to measure water deliveries. Overall irrigation application efficiencies are low. Private forest and rangelands in the Sprague River subbasin are generally used for livestock grazing. Most forest stands are significantly overstocked with trees, and rangeland has been heavily encroached by Western Juniper. Pasture condition is generally poor to fair. The riparian areas within pastures have little to no riparian vegetation and high, eroding banks. Wildlife habitat in most of the upper reaches of the Sprague River and its major tributaries appears to be fairly stable, indicating good watershed condition. However, there are considerable habitat improvements that can be made in the lower portion of the basin. Sprague River Subbasin Water & Wetlands: 2,949 Range: 137,869 Irrigated Pasture/ Grass Hay: 81,650 Forest/ Mixed: 240,050 Sprague River Subbasin Agricultural Land Use/ Cover 19 Resource Concerns Water quality is the major resource concern in the Sprague River Subbasin, directly impacting fish and wildlife habitat throughout the Upper Klamath Basin. Lost River and shortnose suckers, interior redband and bull trout are key fish species present in the subbasin. All species are listed as Endangered Species Act threatened, candidate, or species of concern. The Sprague River has been identified as an important stream for both spawning and rearing habitat for suckers. Loss of riparian habitat, fish entrapment and fish migration impediments have also been identified as resource concerns in the Sprague River Subbasin. Conservation Accomplishments In the Sprague River Subbasin during the last two years, significant conservation progress has been made. With assistance from NRCS and local conservation districts, land managers have improved the condition of 2,153 acres of grazing land, improved irrigation water management on 903 acres of irrigated land, and have restored 1,644 acres of riparian and wetlands areas. Fencing and riparian area restoration has been initiated or installed by private land managers with assistance from NRCS, US Fish & Wildlife Service and others on approximately 50 miles of stream and several thousand additional riparian and wetland acres. Sprague River Subbasin Land Ownership Private Lands 448,200 Public Lands 573,100 Total Land Area: 1,021,300 Irrigated Acres USBR Project: 0 Non- USBR: 61,600 Total: 61,600 20 Conservation Opportunities Water Quality & Wildlife Habitat: Riparian restoration can be accomplished by converting pastures to permanent riparian wildlife lands or establishing riparian vegetation. Riparian pasture units should be managed as a part of an overall grazing plan with cross- fencing and off- stream water for livestock. Forest stands should be managed to ensure optimum health of both the trees and grazed understory. Thinning overstocked trees and controlling juniper on rangelands are both effective management opportunities. Water Demand: Irrigation water management, including measuring water use and scheduling irrigation will help managers to maintain base river flows through late summer and early fall. Efficiencies can also be gained by leveling land, lining or piping irrigation ditches and incorporating tailwater recovery systems. Conversion from flood to sprinkler irrigation is also beneficial. Sprague River Subbasin Sprague River Subbasin Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Storage Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land ............ 34,500 Range & Forestland 164,400 Wildlife Habitat ........... 2,400 Estimated Installation Cost Irrigated Land .......................$ 10,948,000 Range & Forestland .......................$ 31,305,000 Wildlife Habitat .........................$ 4,779,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land .........................$ 1,768,000 Range & Forestland .........................$ 1,665,000 Wildlife Habitat ............................$ 133,000 * Based on conservation need and projected participation rates. 21 Tim McCabe/ NRCS 22 Covering about 928,000 acres, the Williamson River Subbasin is the principal tributary for Upper Klamath Lake. Combined, the Williamson and Sprague River subbasins make up 79 percent of the lake’s total drainage area. The Winema National Forest and Klamath Falls National Wildlife Refuge account for most of the public land in the subbasin. Irrigated pasture is the dominant private agricultural land use. Pasture is almost entirely flood irrigated. Ninety percent is diverted from streams, while groundwater supplies ten percent. Most diversions do not have fish screens and lack devices to measure water deliveries. Although overall irrigation application efficiency is low, additional water in the water table helps to subirrigate pastures. In addition, the proximity of these pastures to rivers and streams allows most excess diverted water to return to the system for reuse. Private forest and rangelands make up most of the private land in the basin. Approximately 80 percent of forestlands are used for grazing. Private forestland is in poor to fair condition; over half of the stands are significantly overstocked with trees. Wildlife habitat has faced considerable degradation in the past. Of the 48 miles of stream that are degraded in the subbasin, restoration efforts have been initiated on approximately 23 miles. Williamson River Subbasin Water & Wetlands: 19,700 Range: 2,600 Irrigated Pasture/ Grass Hay: 81,650 Forest/ Mixed: 225,300 Williamson River Subbasin Agricultural Land Use/ Cover Irrigated Alfalfa: 1,100 23 Water quality relating to elevated stream temperatures is a major resource concern in the Williamson River Subbasin, directly impacting fish and wildlife habitat throughout the Upper Klamath Basin. In 1988, when the Lost River and Shortnose suckers were listed as endangered, the Williamson and Sprague River runs were estimated to have declined by as much as 95 percent during the previous twenty- year period. Important sucker habitat has diminished by nearly 50 percent in the lower reaches and near the mouth of the Williamson River. This has reduced the amount of larval sucker spawning and rearing habitat. Conservation Accomplishments Significant conservation progress has been made in this subbasin. Land managers have improved 500 acres of grazing lands, 1,000 acres of irrigated lands, 235 acres of forestlands and have restored 112 acres of riparian and wetland areas. Heightened landowner awareness of resource concerns and increasing agency, organization, and individual efforts will help this trend to continue. Of the 48 miles of stream that are degraded in the subbasin, private land managers are working with the US Fish and Wildlife Service and others to restore 23 miles. The Nature Conservancy is restoring approximately 3,200 acres of wetlands, and plans to restore another 3,411 acres at the mouth of the Williamson River. Williamson River Subbasin Resource Concerns Land Ownership Private Lands 309,400 Public Lands 618,800 Total Land Area: 928,200 Irrigated Acres USBR Project: 0 Non- USBR: 65,100 Total: 65,100 24 Williamson River Subbasin Williamson River Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Storage Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Wildlife Habitat & Water Quality: Riparian area and wetland habitat restoration and management provide the best opportunity to improve water quality in the Williamson River Subbasin. This can be accomplished by converting lands from irrigated agriculture to wildlife habitat or creating riparian pasture systems. Wetland and riparian areas still utilize water. However, this work may reduce total water demand depending on how lands are managed. Water Demand: Thinning forest stands and managing grazing areas by adding cross fences and off- stream water for livestock can yield more water to meet downstream needs. This will also result in enhanced wildlife habitat and improved water quality in area streams. In addition, forest stand improvements reduce the potential for catastrophic fire. Priority Conservation Opportunities Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land ............ 52,300 Range & Forestland ... 71,200 Wildlife Habitat .............. 200 Estimated Installation Cost Irrigated Land .......................$ 12,863,000 Range & Forestland .......................$ 17,290,000 Wildlife Habitat ............................$ 338,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land .........................$ 2,663,000 Range & Forestland ............................$ 669,000 Wildlife Habitat ..............................$ 11,000 * Based on conservation need and projected participation rates. 25 Tupper Ansel Blake/ USFWS 26 The Upper Klamath Lake Subbasin covers 465,300 acres from Crater Lake to the outlet of Upper Klamath Lake into the Link River. Historically, some 43,000 acres of wetlands surrounded Agency and Upper Klamath Lake. Today, 17,000 acres have been preserved as part of the Upper Klamath Lake National Wildlife Refuge. Another 11,000 acres have been acquired for restoration. Irrigated agriculture is primarily pasture. Livestock are generally stocker cattle, who graze between April and November. Pasture condition is generally fair. Most livestock obtain water from streams and ditches. Irrigation water is diverted from streams or pumped from the lake. Most diversions do not have fish screens or devices to measure water. Although overall irrigation application efficiency is low, the additional water raises the water table and subirrigated pastures. Some acreages of hay and cereal crops are grown, and irrigation efficiencies are higher than for pasture. However, most require maintenance and re- leveling. Forestlands are primarily pine and mixed fir and hemlock. Most private lands in the subbasin are forest or rangelands, with approximately 80 percent used for grazing. More than half of the forest stands are significantly overstocked with trees. Wildlife habitat varies in condition. Of 70 total miles, 21 miles of streamside riparian areas are in good condition and another 12 miles are being restored. Upper Klamath Lake Subbasin Water & Wetlands: 76,568 Range: 2,404 Irrigated Pasture/ Grass Hay: 48,856 Forest/ Mixed: 100,311 Upper Klamath Lake Subbasin Agricultural Land Use/ Cover Irrigated Crop/ Alfalfa: 3,396 27 Resource Concerns Water quality in the Upper Klamath Lake is a major resource concern, affecting subbasin fish survival, with phosphorus loading as the greatest factor. The loss of wetland vegetation around the lake has also been linked to lower survival rates for endangered suckers. The lower reaches of the Wood River and Sevenmile Creek provide some rearing habitat for larval and juvenile suckers. The Wood River, Sevenmile Creek and their tributaries support populations of bull and interior redband trout. A highly valued “ catch and release” sport fishery occurs on the Wood River and several of its tributaries. There is significant interest in enhancing riparian habitat along these streams to protect and promote these fisheries. Conservation Accomplishments In the Upper Klamath Lake Subbasin during the last two years, some conservation progress has been made. With assistance from NRCS and local conservation districts, land managers have improved 12 acres of grazing lands and improved water quality and quantity on 12 acres of irrigated land. Several thousand more acres of wetland restoration are in the process of being planned or implemented around Upper Klamath Lake. Upper Klamath Lake Subbasin Land Ownership Private Lands 235,100 Public Lands 230,200 Total Land Area: 465,300 Irrigated Acres USBR Project: 0 Non- USBR: 52,300 Total: 52,300 28 Priority Conservation Opportunities Water Quality: The most effective conservation includes practices that restore riparian areas, improve grazing management and increase irrigation efficiency. This can be accomplished by either converting pastures to permanent wildlife habitat or by creating riparian pastures. While most pastures are being inefficiently irrigated, conditions do not warrant extensive changes from current flood irrigation systems since water is reused or enters the soil profile Water Storage: In the Upper Klamath Lake Subbasin, the potential for non- traditional water storage presents a unique conservation opportunity. Restoring drained wetlands, still farmed around Upper Klamath Lake, could produce positive benefits for all four resource concerns. By actively managing areas for both seasonal wetlands and farming, water can be both filtered to improve water quality and stored in wetland areas for future use. Upper Klamath Lake Subbasin Upper Klamath Lake Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Storage Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land ............ 42,500 Range & Forestland ... 36,300 Wildlife Habitat ........... 2,900 Estimated Installation Cost Irrigated Land .......................$ 10,462,000 Range & Forestland .........................$ 7,254,000 Wildlife Habitat .........................$ 4,113,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land .........................$ 2,017,000 Range & Forestland ............................$ 308,000 Wildlife Habitat ............................$ 130,000 * Based on conservation need and projected participation rates. 29 Table of Contents Tupper Ansel Blake/ USFWS 30 Irrigated Crop 4,209 The Lost River Subbasin originates above Clear Lake and passes through several agricultural valleys, ending in Tulelake. The valley once supported a vast network of wet meadows and marshes. This subbasin covers approximately 1.2 million acres and is split from the Middle Lost River Subbasin near Olene. Irrigated agriculture generally occurs in the warmer valleys. Flood is the most common pasture irrigation method, with about 50 percent of the water coming from the USBR project. Pasture condition is fair, and most pastures have not been renovated or re- leveled for some time. Maintenance would increase the efficiencies of 60 to 80 percent of the systems. Alfalfa is customarily sprinkler- irrigated and well- managed. Although irrigation efficiencies are higher than for pasture, many sprinkler systems still need upgrading. Several irrigated crops are grown in the subbasin including cereal grains, potatoes, and strawberry plants. Forestland, range and pasture are grazed by livestock. Rangelands are comprised of juniper and sagebrush steppes. Forestlands are generally mixed conifer. Livestock operations include cow/ calf, stockers and dairies. Confined livestock operations are located throughout the subbasin. The location and duration of confinement may pose a potential risk to water quality. Seven dairies located within the subbasin have existing liquid and dry livestock waste storage facilities. Upper Lost River Subbasin Water & Wetlands 13,250 Range 72,630 Irrigated Pasture/ Grass Hay 41,352 Forest/ Mixed 204,420 Upper Lost River Subbasin Agricultural Land Use/ Cover Irrigated Alfalfa 38,943 31 Resource Concerns Wildlife habitat and water quality are two of the major resource concerns in the subbasin. High water temperatures are usually linked to lack of shade, irrigation return flow or other warm water inputs. As measured by total phosphorus, water quality appears to be gradually improving over the last 10 to 20 years. While agriculture is the dominant land use in this subbasin, other sources of phosphorus and other pollutants exist. Sewage treatment outfalls, on- site sewage disposal systems, wildlife, and natural inputs also contribute nutrients and other pollutants to the system. While historically the river had significant fish runs, it currently supports only a small population of Shortnose and Lost River suckers. Conservation Accomplishments In the Upper Lost River Subbasin during the last two years, significant conservation progress has been made. With assistance from NRCS and local conservation districts, land managers have improved resource conditions on 234 acres of croplands and 5,282 acres of grazing lands, and have improved their management of irrigation water on 5,596 acres of irrigated lands. In addition, 846 acres of riparian and wetland areas have been restored. Upper Lost River Subbasin Land Ownership Private Lands 407,500 Public Lands 771,300 Total Land Area: 1,178,800 Irrigated Acres USBR Project: 40,400 Non- USBR: 44,100 Total: 84,500 32 Priority Conservation Opportunities Water Quality: Rotating livestock through smaller pastures will increase forage production, reduce soil compaction and improve water quality. On cropland, integrated pest management, irrigation scheduling, increasing crop residue or installing filter strips will minimize risks associated with some pesticides used on cereal grains, potatoes, onions and other crops. Implementing practices like diverting clean water before it flows through livestock confinement areas near water sources, will reduce the risk of polluted runoff. Water Demand: On both surface-irrigated pastures and cropland areas, there are opportunities for land leveling or smoothing, lining or piping irrigation delivery ditches, upgrading irrigation systems and developing tailwater recovery systems to improve water use efficiency. Upper Lost River Subbasin Upper Lost River Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Storage Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land ............ 58,100 Range & Forestland 147,400 Wildlife Habitat ........... 1,200 Estimated Installation Cost Irrigated Land .......................$ 10,993,000 Range & Forestland .......................$ 20,397,000 Wildlife Habitat .........................$ 1,945,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land .........................$ 3,667,000 Range & Forestland .........................$ 1,384,000 Wildlife Habitat ..............................$ 66,000 * Based on conservation need and projected participation rates. 33 Gary Kramer/ NRCS 34 The Middle Lost River Subbasin covers 454,500 acres and is the center of the USBR Klamath Project. Farms near Klamath Falls tend to be smaller, indicating part- time or hobby operations. The area includes 12 irrigation districts and leased lands on the Lower Klamath Wildlife Refuge that receive water supplied by the USBR Klamath Project. Public lands include the refuge, and parts of Modoc and Klamath national forests. Irrigated agriculture includes pasture, alfalfa, cereal grain, potatoes, onions and mint. Roughly 70 percent is irrigated with USBR- supplied water; the rest is obtained from groundwater, individual surface water rights or special USBR contracts. Many fields are either flood or sprinkler irrigated depending on the year and crop. Most farm irrigation diversions lack a means to measure water delivery. Livestock operations include several dairies and cattle feeding operations. Substantial range acreage is used for livestock grazing. Pasture condition is fair and most pastures have not been renovated or re- leveled for some time. Pastures associated with smaller livestock operations in and around Klamath Falls appear to be in the most need of improved pastures and irrigation systems. Wildlife habitat: Ten river miles are in relatively good riparian condition given the river is used for conveying irrigation water. Some 13 miles of stream lack adequate riparian vegetation and streambank protection. Middle Lost River Subbasin Water & Wetlands 10,766 Range 121,713 Irrigated Pasture/ Grass Hay 40,230 Middle Lost River Subbasin Agricultural Land Use/ Cover Irrigated Alfalfa 34,866 Irrigated Crop 41,837 35 Resource Concerns The primary concern is maintaining a reliable water supply that meets the needs of all users. Drought conditions and increased competition for available water have increased economic, social, political and environmental concerns and uncertainty over the future. Habitat and water quality are two additional major resource concerns in the subbasin. High water temperatures are usually linked to lack of shade, irrigation return flow or other warm water inputs. As measured by total phosphorus, water quality appears to be gradually improving. Agriculture is the dominant land use in this subbasin, but other pollutant sources exist. While the river had significant historic fish runs, it currently supports only a small sucker population. Conservation Accomplishments In the last two years, the Middle Lost River Subbasin has seen significant conservation progress. With assistance from NRCS and local conservation districts, land managers have improved the condition of natural resources on 489 acres of cropland and 3,521 grazing land acres. In addition, 564 acres of riparian and wetland areas have been restored, and water use efficiency has been increased on 3,731 acres of irrigated lands. Middle Lost River Subbasin Land Ownership Private Lands 272,900 Public Lands 181,600 Total Land Area: 454,500 Irrigated Acres USBR Project: 84,700 Non- USBR: 32,300 Total: 117,000 36 Priority Conservation Opportunities Water Demand: Providing irrigators with water measurement tools and training on irrigation scheduling would improve their ability to apply irrigation water more efficiently. Highly effective conservation measures on hay and cropland should focus on updating existing irrigation systems and improving irrigation water management. Water Quality: The use of grazing systems that rotate livestock through smaller pastures will increase forage production, reduce soil compaction and improve water quality. While fishery benefits from restoring riparian areas are minimal, streamside buffers will improve water quality and provide habitat for other wildlife. On cropland, integrated pest management, irrigation scheduling, increasing crop residue or installing filter strips will minimize risks associated with some pesticides used on cereal grains, potatoes, onions and other crops. Middle Lost River Subbasin Middle Lost River Subbasin Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Storage Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land ............ 80,400 Range & Forestland ... 85,200 Wildlife Habitat .............. 400 Estimated Installation Cost Irrigated Land .......................$ 18,859,000 Range & Forestland .........................$ 6,797,000 Wildlife Habitat ............................$ 195,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land .........................$ 5,585,000 Range & Forestland ............................$ 902,000 Wildlife Habitat ................................$ 8,000 * Based on conservation need and projected participation rates. 37 38 The Tulelake Subbasin covers 296,600 acres, bordered by the J Canal and the Lava Beds National Monument. The Tulelake Irrigation District and the Tulelake National Wildlife Refuge receive water from the USBR Klamath Project. Tulelake is a remnant of historic Lake Modoc that once connected the subbasin with both Lower and Upper Klamath Lake. The Lost River watershed was once a closed basin. Runoff flowed into Tulelake and evaporated. Pumping plants and drains constructed as a part of the project have provided an outlet from Tulelake, which now functions as an open basin. Irrigated agriculture is generally supplied by the USBR. Alfalfa, grain, potatoes, onions, mint and pasture are the principal crops. Fields are flood or sprinkler irrigated depending on the year and crop. Often diversions lack devices to measure water delivery. Pasture condition is fair, and most have not been renovated for some time. Groundwater provides 40- 50 percent of water for irrigated pastures, and most excess water is reused. Rangeland is the other significant land use. Most ranches are cow/ calf operations that have winter holdings in the subbasin. Rangelands are generally encroached with juniper. Wildlife habitat along the Lost River has reeds and bullrush, providing some habitat for waterfowl and songbirds. Suckers have been located in the river and Tulelake; however, it is not known whether they are successfully reproducing. There are few opportunities to improve habitat along this heavily manipulated reach of the river. Tulelake Subbasin Water & Wetlands 13,285 Range 36,229 Irrigated Pasture/ Grass Hay 4,050 Tulelake Subbasin Agricultural Land Use/ Cover Irrigated Alfalfa 12,334 Irrigated Crop 48,481 Forest/ Mixed 4,492 39 Resource Concerns The Tulelake Subbasin is at the tail- end of the USBR Klamath Project. Irrigators depend on water- use decisions made by fellow irrigators and resource managers for their irrigation needs. Drought and increased competition for water leads to the primary resource concern in the basin - a reliable supply of water to meet agriculture, wildlife and other resource needs. Water quality deteriorates as it moves through the USBR project. As measured by total phosphorus, water quality appears to be gradually improving. Agriculture is the dominant land use in this subbasin, but other sources of phosphorus and other pollutants exist. The presence of ESA- listed suckers creates concerns for improving habitat and water quality. The two national wildlife refuges support large waterfowl populations. Farmland on the refuges is leased to farmers to supply grain for waterfowl and shorebirds. These populations depend on refuges, leased lands and adjacent farms during the fall and spring migratory periods. Both refuges depend upon tailwater from the USBR project to maintain their marshes and ponds. Conservation Accomplishments In the Tulelake Subbasin during the last two years, significant conservation progress has been made. With assistance from NRCS and local conservation districts, local land managers have improved the condition of natural resources on 72 cropland acres and 1,854 irrigated land acres, and have restored 21 acres of riparian and wetland areas. Tulelake Subbasin Land Ownership Private Lands 131,600 Public Lands 165,000 Total Land Area: 296,600 Irrigated Acres USBR Project: 62,600 Non- USBR: 2,200 Total: 64,800 40 Priority Conservation Opportunities Water Demand: On hay and croplands, upgrading existing irrigation systems and improving irrigation water management will decrease water demand. Subsurface drainage could be added before re- establishing alfalfa stands, permitting better control of water table and soil moisture levels. During years that alfalfa fields are rotated to grain, winter flooding or pre- season irrigation could be used to reduce water demand. Water Storage/ Yield: Adding subsurface drainage may be the most significant practice to implement on cropland acres. Subsurface drains would allow farmers to winter flood or pre-irrigate fields, thereby reducing their demand for water during the irrigation season. If pre- irrigated, farmers could grow a cereal crop even if water deliveries are cut off during drought years. In addition, juniper control on rangelands will yield additional water to meet downstream needs. Tulelake Subbasin Tulelake Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Storage Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land ............ 45,400 Range & Forestland ... 28,500 Wildlife Habitat ........... 1,700 Estimated Installation Cost Irrigated Land .......................$ 18,263,000 Range & Forestland .........................$ 1,741,000 Wildlife Habitat ............................$ 298,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land .........................$ 2,590,000 Range & Forestland ............................$ 257,000 Wildlife Habitat ..............................$ 25,000 * Based on conservation need and projected participation rates. 41 Tupper Ansel Blake/ USFWS 42 The Butte Valley Subbasin lies southwest of Lower Klamath Lake. While part of the Upper Klamath Basin, it is an internal drainage basin with only an artificial outlet. Groundwater flows from west to east out of the subbasin under the Mahogany Mountains toward the lake. A channel and pump plant were built to remove floodwaters. This channel is used infrequently and for only short durations. The Klamath National Forest, Butte Valley National Grassland, and the Butte Valley Wildlife Area make up the majority of the public lands. Irrigated agriculture includes alfalfa hay as the predominate crop. Cereal grains, potatoes and strawberry plants are also grown. Crops are usually sprinkler irrigated, and sprinklers are well maintained. Few irrigators measure water applied or schedule irrigation. Cattle operations graze irrigated pastures and meadows scattered throughout the subbasin along with range and forestlands. Pastures are generally flood irrigated and are supplied by streams. Most farm irrigation diversions lack water measuring devices. Mixed conifer forests are found at higher elevations and are generally operated as industrial forests. Range sites are dominated by Western Juniper and are generally in poor condition. Wildlife habitat is generally wetlands in the state wildlife refuge or on national grasslands. Approximately 26 miles of streams on private lands have inadequate riparian vegetation. Butte Valley Subbasin Water & Wetlands 9,488 Range 73,891 Irrigated Pasture/ Grass Hay 10,355 Butte Valley Subbasin Agricultural Land Use/ Cover Irrigated Alfalfa 30,361 Irrigated Crop 11,490 Forest/ Mixed 52,031 43 Butte Valley Subbasin Resource Concerns The expense of deepening wells and pumping from deeper elevations for irrigation water is a major resource concern. Generally, streams in the upper portions of the subbasin support good populations of Brown and Rainbow trout. The Tulelake National Wildlife Refuge and Lower Klamath Lake National Wildlife Refuge support large populations of migratory and permanent waterfowl. Farmland on the refuges is leased to area farmers to supply grain for the waterfowl and shorebirds. The large bird populations depend on the refuges, leased lands and adjacent farms throughout the fall and spring migratory periods for habitat. Both refuges depend upon tailwater from the USBR project to maintain their marshes and ponds. Conservation Accomplishments In the Butte Valley Subbasin during the last two years, some conservation progress has been made. With assistance from NRCS and local conservation districts, local land managers have restored 27 acres of riparian and wetland areas in the last two years. Land Ownership Private Lands 188,400 Public Lands 199,700 Total Land Area: 388,100 Irrigated Acres USBR Project: 0 Non- USBR: 52,300 Total: 52,300 44 Butte Valley Subbasin Butte Valley Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Storage Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Priority Conservation Opportunities Water Demand: Butte Valley is an internal drainage basin. Other than limited contributions to groundwater in the Upper Klamath Basin, reductions in water demand only benefit the subbasin. Sprinkler- irrigated hay, cereal crops and row crops dominate land use on the better soils. Highly effective conservation on hay and cropland should focus on improving the overall irrigation efficiency of existing systems. This can be accomplished by upgrading systems and scheduling irrigation. An estimated 40 percent of the existing systems would benefit from maintenance. On controlled flood irrigated pastures, there are opportunities for land leveling or smoothing, lining or piping delivery ditches, and recovering tailwater. Additional water savings and water quality benefits could be gained by converting existing surface irrigation to sprinklers if power is available and affordable. On rangelands, juniper control and improved grazing management are the primary conservation opportunities. Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land ............ 35,000 Range & Forestland ... 49,400 Wildlife Habitat ................ 55 Estimated Installation Cost Irrigated Land .........................$ 6,652,000 Range & Forestland .........................$ 5,243,000 Wildlife Habitat ............................$ 109,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land .........................$ 1,569,000 Range & Forestland ............................$ 625,000 Wildlife Habitat ................................$ 3,000 * Based on conservation need and projected participation rates. 45 46 The Upper Klamath River East Subbasin covers the Klamath River drainage between Iron Gate and Keno dams. Nearly half of the area is in public ownership. Iron Gate and Copco reservoirs are used extensively for recreational fishing, boating and camping. Whitewater rafting and kayaking are popular below the KC Boyle Dam. The KC Boyle, Copco and Iron Gate dams are used and regulated for power generation. Irrigated agriculture occurs on only 4,000 acres of pasture. Only a few isolated ranches are located in this subbasin. Cattle operations rotate grazing of irrigated pastures with significant acreage of grazed range and forest. Pastures are surface irrigated with a mix of controlled and flood irrigation. All irrigation water is diverted from the river or tributary streams. Most farm irrigation diversions lack devices to measure water. Even though overall irrigation application efficiency is low, the proximity of irrigated pastures to the river allows most excess water diverted to be reused downstream. Private forest and rangelands make up most of the private land, nearly all of which is used for livestock grazing. Much of the rangeland is in poor condition, with heavy juniper encroachment. More than half of the forest stands are overstocked with trees. Wildlife habitat along riparian areas is generally in good condition. Of the 12 miles of riparian areas surveyed, five would benefit from some restoration. Upper Klamath River East Subbasin Water & Wetlands 4,552 Forestlands 195,516 Irrigated Pasture/ Grass Hay 4,044 Upper Klamath River East Subbasin Agricultural Land Use/ Cover Range 52,366 47 Upper Klamath River East Subbasin Resource Concerns The need to increase water availability to downstream users is the main resource concern along this stretch of the river. Water withdrawals are insignificant along this stretch of the river. Salmon and steelhead are blocked at Iron Gate Dam from upstream passage. Several resident trout species exist, supporting a recreational fishery. Conservation Accomplishments In the Klamath River East Subbasin during the last two years, some conservation progress has been made. With assistance from NRCS and local conservation districts, land managers have improved the condition of natural resources on 56 acres of cropland, 332 acres of grazing land, and 560 acres of irrigated lands. They have also improved forestland health on 46 acres and have restored 924 acres of riparian and wetland areas. Land Ownership Private Lands 256,500 Public Lands 162,900 Total Land Area: 419,400 Irrigated Acres USBR Project: 0 Non- USBR: 4,000 Total: 4,000 48 Upper Klamath River East Subbasin Upper Klamath River East Comparative Benefit of Applied Conservation Practices Water Demand Wildlife Habitat Water Quality Riparian/ Wetland Agronomic Forest & Range Grazing Irrigation Conservation Practices Priority Conservation Opportunities Water Demand/ Yield: Juniper control, thinning forest stands, managing grazing lands by cross- fencing and providing off- stream water for livestock will improve hydrologic conditions, yielding more water to meet downstream needs. This will also improve forage production, habitat condition and water quality in area streams, as well as reduce the opportunity for a catastrophic fire. There are opportunities for land smoothing and tailwater recovery systems to improve overall irrigation efficiency and effectiveness. Additional water savings and water quality benefits would be gained by converting from surface irrigation to sprinklers if power is available and affordable. Conservation Investment Projected Conservation Acres to be Treated* Irrigated Land .............. 1,700 Range & Forestland ... 44,800 Wildlife Habitat .................. 5 Estimated Installation Cost Irrigated Land ............................$ 454,000 Range & Forestland .........................$ 4,769,000 Wildlife Habitat ..............................$ 13,000 Estimated Annual Operation, Maintenance & Management Cost Irrigated Land ..............................$ 86,000 Range & Forestland ............................$ 406,000 Wildlife Habitat .......................................$ 0 * Based on conservation need and projected participation rates. 49 USDA Nondiscrimination Statement “ The U. S. Department of Agriculture ( USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, sex, religion, age, disability, political beliefs, sexual orientation, and marital or family status. ( Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information ( Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at ( 202) 720- 2600 ( voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326- W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250- 9410, or call ( 202) 720- 5964 ( voice or TDD). USDA is an equal opportunity provider and employer.” 50 Upper Klamath Basin 51 Developed by the USDA Natural Resources Conservation Service September, 2004
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17. [Image] The doctrine of prior appropriation : effects upon water rights in the Upper Klamath Basin
Undergraduate student project, Geomatics 466, Boundary Law IICitation -
18. [Image] Settler's guide
This brochure was probably published by the United States Bureau of Reclamation. It was compiled to provide information on the requirements and recommendations regarding homesteading on Tule Lake.Citation Citation
- Title:
- Settler's guide
- Author:
- United States. Bureau of Reclamation
- Year:
- 1948, 2004, 2005
This brochure was probably published by the United States Bureau of Reclamation. It was compiled to provide information on the requirements and recommendations regarding homesteading on Tule Lake.
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CONTENTS Page S. 1988 1 Committee Print of S. 1988 2 Departmental reports: Agriculture 9 Budget 10 Interior 4 STATEMENT Brown, Edmund G., Governor, State of California 26 Butcher, ...
Citation Citation
- Title:
- Tule Lake, Lower Klamath, and Upper Klamath National Wildlife Refuges : hearing before the Subcommittee on Irrigation and Reclamation of the Committee on Interior and Insular Affairs, United States Senate, Eighty-seventh Congress, second session, on S. 1988 ... February 23, 1962
- Author:
- United States. Congress. Senate. Committee on Interior and Insular Affairs
- Year:
- 1962, 2005
CONTENTS Page S. 1988 1 Committee Print of S. 1988 2 Departmental reports: Agriculture 9 Budget 10 Interior 4 STATEMENT Brown, Edmund G., Governor, State of California 26 Butcher, Deveraux, editor, National Wildlands News 158 Cushman, Lester M., vice president; Alvin Landis, counsel; Howard Stoddard, consulting engineer; Edwin Lance, engineer and manager; and Ivan Rose, director, Tulelake Irrigation District 116, 132 Douglas, Philip A., executive secretary, Sport Fishing Institute 144 Dugan, Harold P., regional director, Bureau of Reclamation, Sacramento, Calif., Department of the Interior 60 Elser, William P., president, California Fish and Game Association 137 Gordon, Seth, California Duck Hunters Association 138 Gutermuth, C. R., vice president, Wildlife Management Institute, Wash ington, D.C 148 Henzel, Richard, president, board of supervisors, Klamath Drainage Dis trict 84 Horn, Everett E., California Duck Hunters Association 142 Janzen, Daniel H., Director, Bureau of Sport Fisheries and Wildlife, Fish and Wildlife Service; accompanied by Richard Dittman, engineer; Richard Griffith, chief, Regional Wildlife Division, Portland, Oreg.; Robert Russell, refuge manager, Klamath and Tule Lake Wildlife Refuges; and Jean Branson, staff assistant, regional office, Fish and Wildlife Service, Department of the Interior 40 Johnson, Hon. Harold T., a Representative in Congress from the State of California 114 Kimball, Thomas L., executive director, National Wildlife Federation 146 Kuchel, Hon. Thomas, a U.S. Senator from the State of California 27 Landis, Alvin, counsel, Tulelake Irrigation District 116 Langslet, Chester L., representing the Klamath Basin Water Users' Protective Association, Klamath Sportsmen's Association, and Oregon Wildlife Federation 64, 83 Metcalf, Hon. Lee, a U.S. Senator from the State of Montana 25 Penfold, Joe, Izaak Walton League of America 152 Proctor, George H., counsel, Klamath Drainage District 90 Smith, Dr. Spencer M., Jr., secretary, Citizens Committee on Natural Resources 158 Stearns, James G., supervisor, Modoc County, Calif 110 Stoddard, Howard, consulting engineer, Tulelake Irrigation District 129 Udall, Hon. Stewart L., Secretary of the Interior, accompanied by Robert M. Paul, Special Assistant to the Assistant Secretary, Office of the Assistant Secretary for Fish and Wildlife 18
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A monthly natural flow history was determined for the 1949 to 2000 period at the Keno gage of the Upper Klamath River basin in south-central Oregon. Included within the evaluation is an assessment of natural ...
Citation Citation
- Title:
- Undepleted natural flow of the upper Klamath River : natural inflow to, natural losses from, and natural outfall of Upper Klamath Lake to the Link River and of Lower Klamath Lake to the Klamath River at Keno
- Author:
- United States. Bureau of Reclamation. Denver Office. Technical Service Center
- Year:
- 2005, 2004
A monthly natural flow history was determined for the 1949 to 2000 period at the Keno gage of the Upper Klamath River basin in south-central Oregon. Included within the evaluation is an assessment of natural flows for the same period at the outfall of Upper Klamath Lake, which forms the head of the Link River at Klamath Falls, Oregon. Flow past the Link River gage is tributary to the Klamath River above Lower Klamath Lake. These natural flows were determined using standard and accepted methods. Records used in developing this analysis were derived from stream-gaging records and from climatic records for stations within and adjacent to the study area. Information was also obtained from published maps and reports, and file documents of the Klamath Area Office. Currently, received comments are being addressed and evaluation of elements related to these comments is in progress. The objective of this report is to provide a representative estimate of the monthly natural flow of the Upper Klamath River. Such an estimate is of the natural flow that would typically have occurred without the water-resources developments in the Upper Klamath Basin. A water-budget assessment was used in the determination of the natural flows. The assessment includes results from an evaluation of present-day irrigation depletions, and losses from reclaimed marshland, that have changed the natural inflow to, and resulting natural outfall from, Upper Klamath Lake. Also evaluated were losses to the natural inflow that would have been incurred due to pre-development marshland and evaporation associated with Upper Klamath Lake. The natural outfall from the lake comprised the natural flow of the Link River at Klamath Falls and also the consequent natural inflow to Lower Klamath Lake. Therefore, a similar evaluation was also completed for Lower Klamath Lake to estimate the natural flow of the Klamath River at Keno. The water-budget assessment was designed to simulate each lake as a natural water body within a stream-connected two-lake system. Much of the assessment was completed using Excel.
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21. [Image] EPA 314 clean lakes program: phase I diagnostic/feasibility project: Upper Klamath Lake, Oregon
SUMMARY PROBLEM DEFINITION Upper Klamath Lake, a 90,000 acre body of water located in south-central Oregon, is eutrophic and has reached a stage where summer algal and macrophyte productivity causes ...Citation Citation
- Title:
- EPA 314 clean lakes program: phase I diagnostic/feasibility project: Upper Klamath Lake, Oregon
- Author:
- Klamath Consulting Service, Inc
- Year:
- 1983, 2006, 2005
SUMMARY PROBLEM DEFINITION Upper Klamath Lake, a 90,000 acre body of water located in south-central Oregon, is eutrophic and has reached a stage where summer algal and macrophyte productivity causes severe aesthetic problems and often renders the lake unusable as a recreational site. The problem is a natural one; it has not been caused by man's carelessness and cannot be turned around by regulation. Upper Klamath Lake is quite shallow, warming rapidly in the summer, and the waters carry a naturally occurring high nutrient load. Algal growth is extensive, predominently APHANEZOMENON FLOS-AQUAE, a blue-green algae prevalent in eutrophic waters. These organisms form dense mats that become very odorous as they decay. Numerous macrophytes (aquatic weeds) are indigenous to the lake, but the major problem is with P0TAM06ET0N CRISPUS, which forms long floating fonds that tangle boat motors and prevent passage. The Pelican Bay channel has an extensive growth of this weed.
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Ill., maps (some color), photographs; Includes fiscal year financials, maps, photographs, agricultural economics and crop yield, some grazing financial information with cost of water usage, tables for ...
Citation Citation
- Title:
- Annual project history: Klamath Project, Oregon-California, 1962
- Author:
- United States. Bureau of Reclamation
- Year:
- 1962, 2008, 2006
Ill., maps (some color), photographs; Includes fiscal year financials, maps, photographs, agricultural economics and crop yield, some grazing financial information with cost of water usage, tables for irrigation and drainage and water storage and distributions, list of steam gaging stations, weather conditions, list of evaporation stations, quality of irrigation water at pumping plants, etc.; Title covers: calendar years for 1954-1962; Description is based on: Annual project history: Klamath Project, Oregon-California 1954; Dates of the beginning year(s) of publication are derived from May 1, 1903 to December 31, 1912, History of the Klamath Project and from the volume information on later volumes (v. 35) Klamath District and Klamath Project annual history for 1945, dated December 1, 1946
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- 7' -, > \ UNITED STATES DEPARTMENT OF THE INTERIOR B U R E A U O F R E C L A M A T I O N U N I T E D S T A T E S G O V E R N M E N T P R I N T I N G O F F I C E W A S H I N G T O N : 1936 FEDERAL RECLAMATION ...
Citation Citation
- Title:
- Klamath Federal Reclamation Project : Oregon-California
- Author:
- United States. Bureau of Reclamation
- Year:
- 1936, 2005
- 7' -, > \ UNITED STATES DEPARTMENT OF THE INTERIOR B U R E A U O F R E C L A M A T I O N U N I T E D S T A T E S G O V E R N M E N T P R I N T I N G O F F I C E W A S H I N G T O N : 1936 FEDERAL RECLAMATION PROJECT OREGON - CALIFORNIA n )> >> GENERAL STATEMENT THEKla m- ath reclamation project comprises practically all of the agricultural land in the Klamath Basin, except a small area adjacent to Upper Klamath Lake, and is situated in southern Oregon and northern California. The extent of the area irrigated, or that may be irrigated by reason of Bureau of Reclamation activities, is approxi-mately 140,000 acres. This includes about 20,000 acres suitable only for pasture and approximately 12,000 acres of good land in the Tule Lake division not yet opened for settlement. Within the older developed sections of the project the soil is mostly of a sandy loam . type that is particularly suitable for growing potatoes and summer vegetables as well as all of the ordinary crops that thrive in a cool, tem-perate climate. The price of this type of land ranges from $ 100 to $ 200 per acre. The water- right cost, which origi- Klamath Falls, Oregon, the prolect office headquarters nally was about $ 55 per acre, is approximately half paid up. The balance has an average of about 25 years to run without interest. Operation and maintenance costs usually run about $ 1.25 an acre per annum. I R R I G A B L E L A N D S The Tule Lake division of the project, which will eventually comprise about 32,000 acres of agricultural land and about 5,000 acres of thin soil land good only for pasture, carries a construction charge of $ 88.35, with 40 years in A! Klamath : desert. Looking~ southwest up Lan Valley from a point 4 miles west of Lorella, Ore which to pay without interest. No payments have been required to date, but the Secretary of the Interior will soon issue public notice announcing the commencement of pay-ments, which will be approximately $ 2.20 per acre each year. In addition to the construction charge, there is an operation and maintenance charge which will probably run between $ 1.50 and $ 2 un acre a year. These lands are of lacustrian origin and are very fertile. They are particularly adapted to the growth of small grains, alfalfa, and pasture grasses. Patented land in this division sells for $ 50 to $ 100 per acre. Patented lands in private ownership, where of goc; d quality, well improved and conveniently situated, can be purchased for from $ 150 to $ 200 per acre. Good lands not so well improved nor so desirably located sell at around $ 100 per acre. There is very little undeveloped, privately owned good land on the project. Small tracts of 5, 10, or 20 acres, located along paved highways and within 6 to 8 miles of Klamath Falls, are obtainable at from $ 200 to $ 400 per acre. W A T E R S U P P L Y The Klamath project is ! ortunate in having an abundant water supply for all lands susceptible of irrigation. The map on the inside of the back cover page shows the location of the three reservoirs and their immediate proximity to the lands they serve. The irrigable project lands lie between elevations of 4,035 and 4,070 feet above sea level and occupy the Klamath Basin and the Valley of Lost River, situated in south central Oregon and north central California, about 150 miles east of the Pacific coast. The average annual pre-cipitation is 12.51 inches. SCHOOLS Klamath County schools are run on the county unit basis Public School in Klamath Falls and are fully up to standard. Busses run at county expense transport rural children to and from school, and there is no lost time on account of bad weather. Within the county there are 9,242 children of school age, 4,107 of these within the city of Klamath Falls. The high school enrollment for Klamath Falls is 1,156, and for the remainder of the county is 459. There are 9 high schools in the county that employ 62 teachers. The grade schools employ 185 teachers, of whom' 76 are in the city of Klamath Falls. : let of concrete flume, Canal C, of the main project structures R E C R E A T I O N No part of the United States affords more interesting and attractive recreational areas than are found near at hand and in all directions from the Klamath project. From 1 to 2 hours in any kind of an automobile is sufficient to land one on the banks of a cold mountain stream inhabited by many wary trout or alongside the shores of any one of a half dozen crystal lakes, where boating and bathing may be enjoyed to the full. Some of the lakes that are conven-iently located with reference to the project, and where many summer camps as well as extensive hotel and camp accommodations already exist, are Upper Klamath Lake, Lake of the Woods, Crater Lake, Diamond Lake, Crescent I., ake, Ode11 Lake, and Paulina Lake. The most distant of the lot, Paulina Lake, can be reached in 3 hours' driving from Klamath Falls. Some of the important recreational areas lying in convenient distances from the project are shown in the ilh~ strationsa ccompanying this chapter. The principal water supply is in Upper Klamath Lake, where regulation provides a possible storage of about 524,800 acre- feet, and this with the natural inflow insures the lands served from this source an adequate water supply at all times. Under the terms of the contract dated February 24, 1917, between the United States and the California- Oregon Power Co., the power company was given the right to regulate the outflow of Upper Klamath Lake, subject to existing rights and the prior rights of the Klamath project for water for irrigation. To regulate the outflow, the company, in 1921, constructed the Link River Dam at a cost of about $ 310,000. Storage for the lands on the west side of Langell Valley and a portion of the lands in the Horsefly irrigation district is provided by Clear Lake Reservoir. This reservoir, lying just across the line in California, is the source of Lost River and has a total capacity of 454,000 acre- feet, most of which was made available during 1931 by the construction of a channel from the outlet works to the deeper portion of the reservoir, a distance of about 6 miles. The reservoir is also used for flood storage for the protection of lands in the Tule Lake division. Gerber Reservoir, on Miller Creek, a tributary of Lost River, has a storage capacity of 94,000 acre- feet and fur-nishes a water supply for the lands on the east side of Lost River in the Langell Valley division. This reservoir also provides for the storage of flood water for the protection of lands in the Tule Lake division. Water from Upper Klamath Lake is diverted to the main or " A" canal from the east side of Link River, the outlet of the lake, several hundred feet below the lake and a few I I / Klamath River near Klamath Falls k River diversion dam Alfalfa field near Malin, Oreg. Two cuttings are grown, which yield 2- 4 tons per acre on the older project lands, and 3- 6 in Tule Lake section hundred feet above Link River Dam. Water for all lands in the main and pumping divisions and for a portion of the lands in the Tule Lake division are diverted through the " A" canal. Additional water for the lands in the Tule Lake division is diverted from the Klamath River, through the Lost River diversion channel ( reversing the direction of flow), and spilled into Lost River, frcm which it is diverted to the " J" canal at a point about 3 miles southeasterly from Merrill, Oreg. At this point the river level is raised about 12 feet by means of the lower Lost River diversion dam, a concrete structure of the Ambursen type, with a crest length of 204 feet. The Lost River diversion channel leads off from Lost River at a point about 10 miles southeast of Klamath Falls, Oreg., immediately above a hollow U- shaped concrete dam which raises the river level about 23 feet. Prior to the Irrigating a 65- acre field of potatoes; showing application of m irrigation season the flow of Lost River is diverted to the Klamath River and wasted; however, after the spring flood flow of Lost River has passed and water for irrigation in the Tule Lake division is required, the flow of Lost River is ~ assed through the dam and down to the " J" canal. This flow is augmented, when demand is heavy, from Klamath River as indicated ahve. Lands on the east side of Langell Valley division are served by the north canal, which diverts water from Miller Creek at the Miller Creek Dam, located about 6 miles below Gerber Dam. At this point the water surface in Miller Creek is raised by placing flashboards against wooden trestles, the grade of the canal and that of the stream being substan-tially the same elevation. The lands on the west side of Lost River in the Langell Valley division are served by the West Canal, which diverts water from Lost River at the Malone Dam, located about 42 miles southeasterly from Klamath Falls, Oreg. At this point the level of Lost River is raised about 18 feet by means of an earth diversion dam. Clear Lake Reservoir provides storage for the West Canal. TOWNS Klamath Falls, Merrill, Malin, and Bonanza are project towns, the first named being the principal city in southern, Oregon east of the Cascades. It has a population of approximately 16,000 and is the distributing center for a large territory. Klamath County has a population of 32,400, one- half residing in the city of Klamath Falls and perhaps 4,000 more in suburban districts only a few miles away. Merrill and Malin are small towns within the irrigated area with populations of six or seven hundred each. In Klamath Basin are some 1,800 farms and approximately as many farm families. LUMBERING Approximately 30 mills and box factories are in operation, this district being the largest manufacturing center of box shook in the United States. The Klamath district contains the heaviest stand of yellow pine left in the United States. Throughout the spring, summer, and fall all lumber com-panies maintain large pay rolls both in the plants and in the lumber camps. Lumber contributes greatly to the heavy traffic originating at K! amath Falls, making this city the second largest shipping point in Oregon. The majority of the mills and box factories are located in or near Klamath Falls. T R A N S P O R T A T I O N Two main- line railways, the Southern Pacific and Great Northern, enter Klamath Falls and traverse the project throughout its longest dimension. Hard- surfaced highways radiate from Klamath Falls in all directions, connecting with Portland, Sun Francisco, and Salt Lake. These high-ways supplemented by county market roads penetrate all sections of the project, with the result that few farms are more than a mile from a hard- surfaced outlet. CLIMATE The Klamath Basin has a remarkably pleasant and healthful climate. Winters are not cold, and summers are not hot. Precipitation, which amounts to about 12): inches a year on the average, falls mainly from November to April. Late and early frosts are to be expected, and occasionally light frosts occur even in the summer months. me on the Main division of the project A G R I C U L T U R E The principal crops grown are potatoes, alfalfa, small grains, and vegetables. The yield of small grains in the Tule Lake area is unusually high. Oats frequently make 100 bushels per acre; barley runs from 60 to 80; and any good wheat field will thresh out more than 40 bushels per acre. Potatoes, when conditions are right, are par excelience the big money crop. A good yield of tubers is considered to be around 150 sacks of U. S. No. 1' s per acre, and every year a few fields are reported with yields of double that amount. The price for potatoes is unstable, depending on the market demand, and ranges from about 50 cents to $ 1.50 a sack. The quality of Klamath potatoes on the Sun Francisco market is recognized as the best, and the price usually ranges from 10 to 20 cents a sack higher than is paid for Washington and Idaho production. Flock of 6,000 turkeys being fattened for market L I V E S T O C K Cattle. On account of its geographical location, sur-rounded as it is with immense areas of sagebrush plateaus and forest ranges, the Klamath project is, and probably always will be, essentially a stock country. Its cheap forage, abundant water and mild winters offer ideal con-ditions for the wintering of range stock and the fattening of mature animals for market. Favorable feeding- in- transit rates for both grass and feed lot cattle have resulted in the fattening, locally, of thousands of range and outside cattle. The beef industry alone returns approximately $ 900,000 annually. There are several killing and manu-facturing plants located in Klamath Falls. Sheep. Approxinately 150,000 ewes are maintained in the Klamafh Basin with an average annual output of about three- quarters of a million dollars. From 75,000 to 100,000~ lambs~ afraet tened for market each year on the project. Sun Francisco js the principal market. licken ranch. The production of eggs chickens is an important industry A project Holstein dairy her Dairying. The dairying industry is increasing steadily on the project. There are now about 8,000 milk cows in the district. Klamath Falls, with its large industrial popu-lation, furnishes a good market for milk, butter, and cheese. Two local cooperative cheese manufacturing plants and four privately owned creameries operate in the district. The value of the dairy industry is approximately $ 600,000 annually. Local dairy prices for butterfat are maintained at l> e to 2 cents above the State average cwing to the favored position of the project-- half- way between Portland and Sun Francisco. This district offers many opportunities for increased dairying production, as costs are compara-tively low and climatic conditions are favorable. Ewes and lambs on Tule Lake leased lands OREGON - CALIFORNIA MAP NO. 27606 Scale of Miles 1 -- 0 1 2- 3 4 6 1
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An article written by the first representative of the Reclamation Service after the Reclamation Act of 1902 was passed. This article includes a photo of the author, a map of the Yuma Project and two photos ...
Citation Citation
- Title:
- Operations of the Reclamation Service in California
- Author:
- Lippincott, J.B.
- Year:
- 1906, 2005, 2004
An article written by the first representative of the Reclamation Service after the Reclamation Act of 1902 was passed. This article includes a photo of the author, a map of the Yuma Project and two photos of the Yuma Project "Boating into camp at Laguna Dam" and "Construction work, Yuma Project"
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25. [Image] Natural flow of the upper Klamath River
Executive Summary Executive Summary This report presents details of the investigation and results in estimating the natural flow of the upper Klamath River at Keno, Oregon. The area investigated includes ...Citation Citation
- Title:
- Natural flow of the upper Klamath River
- Author:
- United States. Bureau of Reclamation. Klamath Basin Area Office
- Year:
- 2005, 2008
Executive Summary Executive Summary This report presents details of the investigation and results in estimating the natural flow of the upper Klamath River at Keno, Oregon. The area investigated includes the Klamath River Basin above Keno, Oregon, primarily in Klamath County, with some areas of Siskiyou and Modoc Counties in California. The study area includes the Sprague, Williamson, and Wood River basins, as well as Upper Klamath and Lower Klamath Lakes. Objectives The current purpose of this study is to provide an estimate of the monthly natural flows in the upper Klamath River at Keno. This estimate of the natural flow represents typical flow without agricultural development in the Upper Klamath River Basin, including its tributaries. Study Approach This study used a water budget approach to assess the agricultural depletions and alterations to the natural flow. The approach was to evaluate the changes of agriculture from predevelopment conditions, estimate the effects of these changes, and restore the water budget to natural conditions by reversing the effects of agricultural development. Records used in this empirical assessment were derived from both stream gaging flow histories and from climatological records for stations within and adjacent to the study area. Water Budget Description The water budget assessment of the watershed as a natural system includes an evaluation of hydrological changes related to agricultural development above the Keno gage. The water budget assessment includes: ? Natural inflow from the Sprague, Williamson, and Wood Rivers to Upper Klamath Lake ? Predevelopment evapotranspiration losses from marshes surrounding Upper Klamath Lake ? Predevelopment evaporation losses of the Upper Klamath Lake ? Natural flow at the outlet of Upper Klamath Lake into the Link River at Klamath Falls ? Resulting natural flow at Keno The processes developed in the water budget to evaluate the natural outflow of Upper Klamath Lake accounts for factors related to water resources developments XI Natural Flow of the Upper Klamath River in the watershed that have affected inflow to the lake, and for losses due to natural condition of the lake. The water budget assessment of the watershed as a natural system includes an evaluation of hydrological changes related to agricultural development above the Keno gage. The results of the water budget assessment are given as average annual flows for two important stream gages, one located on the Link River at Klamath Falls and the other on the Klamath River at Keno. Evaluation of Predevelopment Conditions An evaluation of predevelopment conditions included an evaluation of changes to Upper Klamath Lake, agricultural developments in the Wood River, Sprague River, and Williamson River watersheds. Several basic elements were considered in this study: ? How had development changed the system ? Was information available about conditions before the changes occurred ? Were data available to assist in estimating changes to the natural system Evaluation of Current Conditions Period of Record The period of record considered in this investigation is the 52 years from 1949 to 2000. This period of record was chosen because hydrologic and climatological data were limited for the pre-1949 period and data beyond 2000 were not available when the study began. The water year convention (October through September) is used in this report. Crop and Marshland Evapotranspiration Analysis The modified Blaney-Criddle method was used to determine potential net evapotranspiration (ET) from crops, marshlands, and riparian zones. The method is empirical and the calculated values were adjusted based on other recent study findings and water limiting considerations. To estimate net ET water consumption by this method requires the following data: ? Location of irrigated lands, marshlands, and riparian zones ? Types of crops and number of acres for each crop ? Types and acreages of marshland and riparian vegetation, both existing and predevelopment ? Monthly precipitation and monthly average temperature for the period of record for each area Methods to Estimate Natural Flows Natural streamflow development included adjustment of gaged streamflow to natural flow, restoration of missing streamflow and climate data, making natural streamflow estimates in ungaged watersheds, assessing groundwater XII Executive Summary contributions, and estimating transit losses. Not all of these procedures were appropriate or possible in all subbasins of the study area. Records of historic flow may be adjusted to natural flow using crop net consumptive use and marshland evapotranspiration: natural flow = gaged flow + crop net consumptive use - reclaimed natural marshland net evapotranspiration Correlation analysis was used to restore missing values from monthly-value data records used in this study. The method is different from linear least-squares regression estimation. Data records used in this study include precipitation and average temperature histories, in addition to hydrologic records of streamflow and lake stage. Also, natural streamflow histories are required in ungaged watersheds to assess the natural inflow to Upper Klamath Lake. Sparse monthly flow records for streams heading on the east flank of the Cascades and flowing into the Wood River Valley or Pelican Bay area of Upper Klamath Lake required estimation techniques that used gaged histories from nearby river basins. These data were evaluated in statistical applications to yield natural flow estimates for these ungaged portions of the Klamath Basin. In a similar vein, groundwater contributions required temporal adjustments attributable to the climate signature evident in longer term records for similar groundwater discharges in neighboring watersheds. Transit losses for both surface water and groundwater contributions were also estimated in this study. Natural Lake Simulations Implementation of a water budget for Upper Klamath Lake required developing information about (1) the storage and inundation surface area characteristics of the lake, and (2) the discharge characteristics at the outflow point of the lake. These characteristics were evaluated in relation to the elevation, or stage, of the water surface of the lake. Additionally, discharge from the lake was also related to the stage. Estimating the outflow of a natural lake is accomplished using a water budget approach. A monthly summation of all elements in the water budget may be stated by the general form of the hydrologic equation: i = o + As where i = inflow to the lake o = outflow from the lake and As = change in storage of the lake XIII Natural Flow of the Upper Klamath River For Upper Klamath Lake, the month-to-month water budget accounts for natural inflow, storage of water within each lake, resulting estimated lake stage, and discharge from each lake. In addition, open water surface evaporation and groundwater discharge to the lake from the regional aquifer were estimated. The water budget assessment was designed to simulate the lake as a natural water body. Materials and Data Researched and Used Data Sources Records used in this analysis were derived from both stream gaging flow histories and from climatological records for stations within and adjacent to the study area. Information was also developed from published reports, file documents, and maps. Supporting information included documents from: ? Archives of the Bureau of Reclamation Klamath Basin Area Office ? Numerous U.S. Geological Survey (USGS) Water Supply Papers regarding stream gaging records ? Compact disk databases containing digital records of gaged flow, lake stage records, and meteorological data Anecdotal items from newspaper articles or clipped from magazines were also reviewed. These sources consisted of narratives of past events or conditions, transcripts of interviews, newspaper accounts, books, diaries, and historical journals. These provided an impression of predevelopment conditions that can be compared to the empirical and scientific information gleaned from other sources. Other reviewed materials included unpublished and out-of-print scientific reports, historical maps, letters, books, journals, and photographs. Modeling Tools Results of the water budget assessment were accomplished using Excel?, a sophisticated spreadsheet available in the Microsoft Office for Windows software package. This model was chosen over other models because this study is unique. The computational modules built as the study developed represent a custom application of Excel? to the solution of estimating the natural flow conditions in the Upper Klamath River Basin. Klamath River at Keno Gaging Station For the simulation period, 1949 to 2000, the water balance for the Upper Klamath River Basin at Keno is described below. The natural outflow (discharge) from Upper Klamath Lake at Link River was computed in the water balance. Discharge at Keno was then calculated using a correlation relationship developed between historic measured Link River and Keno flows. Table S-l presents the estimated water balance and outflow developed for the Link River and Keno gages. XIV Executive Summary Table S-1. Estimated inflow and outflow developed for Link River and Keno gages Upper Klamath Lake Acre-feet Average annual natural inflow Average annual natural net loss 1,605,000 210,000 Resulting average annual natural outflow 1,395,000 Link River to Keno Average annual natural inflow 1,485,000 Resulting average annual natural outflow at Keno gage 1,306,000 Other Factors Considered The focus of this study is agricultural development in the Upper Klamath River Basin and its effects on natural flow conditions. Other watershed factors have changed since predevelopment. Some of these factors were considered, but are unaccounted-for in the assessment, such as changes in forest conditions or an extension of the flow histories before 1949. Model Review and Sensitivity Analysis Although this study uses best available hydrologic methods and data to either measure or estimate all inflows and outflows to the system, additional concerns have arisen in completing the work. Relationships regarding the significance of uncertainty are likely to be spatially and temporally variable. The key factor is the relative importance of each module in the transit losses suffered by inflows to the natural system. The significance of these influences to model sensitivity is related to time of year or length of time over which flows are evaluated. Model sensitivity is related to uncertainty in data regarding the most significant transit losses; namely, marsh evapotranspiration and open water evaporation. The natural flows developed at Keno are realized, in part, through a statistical rule based model rather than a physically based model. This construct within the model is for the segment from the Link River gage below Upper Klamath Lake, to the Keno gage below Lower Klamath Lake. Thus, sensitivity in testing the spatial and temporal variables within the Link River to Keno reach that affect the flow at Keno is problematic. xv Natural Flow of the Upper Klamath River Summary Development of the natural flows at the Keno gage was accomplished using a spreadsheet modeling approach to resolve the water budget for the Upper Klamath River Basin under undeveloped watershed conditions. The resulting flow duration for simulated natural average monthly flows for Keno gage are described in Table S-2. The percentiles represent the flow exceedence ranges in monthly natural flow estimates at Keno solely due to record length. These percentiles are estimates for modeled baseline conditions and do not reflect data uncertainties for possible changes in evaporation, evapotranspiration, or other factors. Table S-2. Summary of simulated monthly flows at Keno in cfs % Time <= Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sept Annual % Time >= 10 648 1088 1216 1408 1647 1577 1670 1408 1168 631 520 560 1188 90 20 769 1159 1352 1472 1767 1689 2017 1721 1358 822 578 616 1429 80 30 857 1255 1453 1667 1925 1907 2125 2051 1664 964 706 720 1528 70 40 974 1342 1625 1845 2016 2040 2477 2280 1890 1228 767 746 1607 60 50 1033 1455 1698 1964 2343 2133 2595 2649 2039 1349 873 854 1773 50 60 1131 1523 1803 2072 2410 2360 3009 2827 2388 1478 998 955 1903 40 70 1224 1576 1984 2196 2615 2703 3146 3131 2657 1706 1154 1049 2169 30 80 1304 1739 2049 2399 2829 3115 3615 3385 3104 2210 1351 1210 2347 20 90 1488 1815 2319 2659 3294 3367 3877 3707 3460 2923 1684 1412 2511 10 A simplified flowchart depicting the overall sources of included inflow and outflow variables has been completed as figure S-l, with average annual values shown from each source. XVI
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26. [Image] Nitrogen and phosphorus loading from drained wetlands adjacent to Upper Klamath and Agency Lakes, Oregon
Two maps digitized separately; Includes bibliographical references (p. 44-49)Citation -
27. [Image] Nutrient loading of surface waters in the Upper Klamath Basin : agricultural and natural sources
Abstract Implementation of the Federal Clean Water Act and Oregon Senate Bill 1010 is proceeding under two simultaneous processes in Oregon. The Oregon Department of Environmental Quality is responsible ...Citation Citation
- Title:
- Nutrient loading of surface waters in the Upper Klamath Basin : agricultural and natural sources
- Author:
- Rykbost, K. A.
- Year:
- 2001, 2004
Abstract Implementation of the Federal Clean Water Act and Oregon Senate Bill 1010 is proceeding under two simultaneous processes in Oregon. The Oregon Department of Environmental Quality is responsible for developing Total Maximum Daily Load (TMDL) allocations for water-quality limited water bodies. The Oregon Department of Agriculture is striving to develop Management Area Plans to provide guidance for management of private agricultural lands to meet Clean Water Act objectives. Both processes seek input from local advisory committees comprised of landowners and other stakeholders, and technical review committees. Klamath Lake and Klamath River have been designated water quality impaired for several parameters including nutrients. Researchers have attempted to determine the extent of agriculture's contributions to nutrient enrichment of surface waters in the Upper Klamath Basin. Two United States Geological Survey (USGS) studies focused attention on drainage of agricultural lands adjacent to Klamath Lake as a significant source of nutrient loading in the lake. A preliminary draft report by the Klamath River TMDL committee identified the outlet for drainage waters from the Klamath Irrigation Project to the Klamath River at the Straits Drain as a point source for nutrient loading. Preparation of a final TMDL for this sub-watershed was tabled pending development of a TMDL for Klamath Lake and its tributaries. Insufficient data are available to determine the relative contributions of agricultural activities, natural background sources, and other potential sources of nutrient enrichment to establish numerical limits for nutrient loading from agricultural lands. From 1998 through 2000, the Klamath Experiment Station has investigated nutrient loading from drainage of agricultural lands adjacent to Klamath Lake, natural background sources including major springs and several artesian wells, and loading to the Klamath Irrigation Project from diversions out of Klamath Lake and Klamath River. Findings indicate contributions from agricultural lands adjacent to Klamath Lake have been overestimated, and the Klamath Irrigation Project is probably a net sink for nutrients diverted out of Klamath Lake and Klamath River. Data to support these assertions are presented. Introduction Most of the surface waters in the Klamath Basin are included in the Oregon department of Environmental Quality (DEQ) 303D list as water-quality limited. While the only criterion for listing of many streams is temperature, based on a preliminary standard of 64°F, Klamath Lake and Klamath River are listed for chlorophyll a, dissolved oxygen, un-ionized ammonia, and pH. The DEQ is working toward development of TMDL allocations for Klamath River and
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28. [Image] Resolving the Klamath
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Abstract Everest, Fred H.; Stouder, Deanna J.; Kakoyannis, Christina; Houston, Laurie; Stankey, George; Kline, Jeffery; Alig, Ralph. 2004. A review of scientific information ...
Citation Citation
- Title:
- A review of scientific information on issues related to the use and management of water resources in the Pacific Northwest
- Year:
- 2004
Abstract Everest, Fred H.; Stouder, Deanna J.; Kakoyannis, Christina; Houston, Laurie; Stankey, George; Kline, Jeffery; Alig, Ralph. 2004. A review of scientific information on issues related to the use and management of water resources in the Pacific Northwest. Gen. Tech. Rep. PNW-GTR-595. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 128 p. Fresh water is a valuable and essential commodity in the Pacific Northwest States, specifically Oregon, Washington, and Idaho, and one provided abundantly by forested watersheds in the region. The maintenance and growth of industrial, municipal, agricultural, and recreational activities in the region are dependent on adequate and sustainable supplies of fresh water from surface and ground-water sources. Future development, especially in the semiarid intermountain area, depends on the conservation and expansion of the region's water resource. This synthesis reviews the state of our knowledge and condition of water resources in the Pacific Northwest. Keywords: Water distribution, flow regimes, water demand, conflicts, tools, water use.
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ABSTRACT A water quality study was performed in the mainstem Klamath River from Keno, Oregon to Seiad Valley, California during 1996 through 1998. Four sites within the study area were continuously ...
Citation Citation
- Title:
- Water quality and nutrient loading in the Klamath River between Keno, Oregon and Seiad Valley, California from 1996-1998
- Author:
- Campbell, S. G
- Year:
- 2001, 2007, 2005
ABSTRACT A water quality study was performed in the mainstem Klamath River from Keno, Oregon to Seiad Valley, California during 1996 through 1998. Four sites within the study area were continuously monitored using multiparameter recorders. Water quality sampling was also performed at these four locations in 1996 and 1997. Additional water quality sampling sites were added in 1998 for a total of 8 locations between Keno and Seiad. Temperature ranged from near zero ?C to >25 ?C with cooler temperatures in early spring and fall, and maximum temperatures occurring in July and August of each year. Dissolved oxygen concentration ranged from near zero mg/L to >13 mg/L with highest DO occurring in early spring and fall and lowest DO occurring in mid-summer. Air temperature was generally highly correlated with water temperature with r values ranging from 0.8 to 0.9 during the study period from 1996-1998. Water temperature in the study area exceeded chronic (>16?C) and acute (>22?C) criteria for salmonids during the summer months. Although chronic DO (<7 mg/L) criteria were exceeded throughout most of the study area during the summer, in the free-flowing river below Iron Gate Dam the acute DO (<5.5 mg/L) criteria were not exceeded. Nonpoint source pollution in the form of agricultural return flows, industrial, or sewage effluent entering the stream may have resulted in higher ammonia and total organic nitrogen concentrations at the upstream locations in the Klamath River study area (Keno and J.C. Boyle Powerplant). Nitrification of ammonia and organic nitrogen seemed to result in higher concentrations of nitrate in the downstream Klamath River (Iron Gate Dam). Total phosphorus concentration stayed relatively stable through the reservoirs in the study area, but decreased in the downstream direction between Iron Gate Dam and Seiad. Ortho-phosphorus concentrations increased longitudinally through the reservoirs, then decreased in the downstream direction between Iron Gate Dam and Seiad. An increase in ortho-phosphorus concentration can indicate internal cycling occurring in the reservoirs as well as photosynthesis. On an annual basis total phosphorus loading increased longitudinally from up- to downstream between Keno and Seiad. The increase was statistically significant (p = .03) indicating that the reservoirs in series in the Klamath River study area do not function as a nutrient sink. However, during the summer there was no statistically significant difference in total P loading when Keno, Iron Gate and Seiad locations were compared, therefore, the reservoirs may act as a nutrient sink seasonally. The Klamath River study locations were generally nitrogen limited, although at Keno, a regular change from N limitation to P limitation occurred during the fall of all three years of the study. When the Klamath River annual nutrient loading values are compared to other rivers in the vicinity, the Carson, Truckee, and Long Tom Rivers also appear to be nutrient enriched. The Carson and South Yamhill Rivers seem to be N limited systems and the Wood, Long Tom, Snake and Truckee Rivers seem to be P limited systems. Implementing management strategies for reservoir operations to improve water quality and reduce nutrient concentration or loading in the Klamath River study area to benefit anadromous fisheries may be difficult and expensive. However, improving the thermal regime in spring to benefit YOY salmonids may be possible as is short-term relief in fate summer for over-summering species. Decreases in nutrient concentration or loading accomplished through best management practices in the water shed may allow general protection of water resources in the Klamath Basin for future needs.
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INTRODUCTION AND GENERAL Genex*al Description of the Project Location. The Klamath Project is in the Upper Klamath River Basin, east of the Cascade Range. It is located in Klamath Comity, Oregon, ...
Citation Citation
- Title:
- Annual project history: Klamath Project, Oregon-California, 1958
- Author:
- United States. Bureau of Reclamation
- Year:
- 1958, 2008, 2006
INTRODUCTION AND GENERAL Genex*al Description of the Project Location. The Klamath Project is in the Upper Klamath River Basin, east of the Cascade Range. It is located in Klamath Comity, Oregon, and in Modoc and Siskiyou Counties of California. Project headquarters is located at the principal city of Klamath Falls, Oregon, which has a population of about 3&>^00, including suburbs. Smaller towns on the project in Oregon are Merrill, Malin, and Bonanza. The town of Tulelake, California, was established in 1931 near the center of the Tule Lake Division. Climate ? The mean temperature for the warmest month is 630 F. The coldest month has raez.n temperature of 29? F. Summer nights are cool. The annual rainfall is about 13 inches, of which about 3^ inches fall during the growing season of 90 to 130 days. Topography, soils, and crops. The project area is about U,100 feet elevation above sea level. The surface topography is generally smooth and flat for the large areas of lake bottom, and gently sloping on the higher lands? Peat and muck soils are common in the recent lake bottoms. Soils vary from sandy loam to clay on other parts of the project. The principal crops grown are alfalfa, malting and feed barley, potatoes, clover seed, and irrigated pasture and other forage. Stock raising is an important enterprise. Industry and transportation. Farming and lumbering each provide the major portion of the economy of the Basin. Three major railroad lines, one major highway and many secondary highways, and two airlines serve the project area. Plan and purpose. In 1958 the project provided irrigation service to 21^,500 acres. The water supply is provided by two main water courses, Klamath River and Lost River and their tributaries. Besides storing, diverting, and distributing water for irrigation, project facilities have reclaimed by drainage large areas formerly inundated by Lower Klamath and Tule Lakes. Flood waters of Lost River, which terminates In Tule Lake, are diverted to the Klamath River through the Lost River Diversion Channel. This channel is also used to carry irrigation water in the opposite direction in the summertime. Another principal function of the project is water-level control for the Tule Lake and Lower Klamath Lake National Wildlife Refuges. DTERODUCTIOH AND GBNKRAL (Continued) General Description of the Project (Cont.) Upper Klamath Lake on the Klamath River is the principal storage reservoir, having an active capacity of 52^,800 acre-feet. It is controlled by Link River Dam constructed, maintained, and operated by The California Oregon Power Company under an agreement with the project whereby irrigation requirements and rights are protected. The Main, Lower Klamath, and Tule Lake Divisions are served from this source. Gerber Reservoir on Miller Creel; and Clear Lake Reservoir on Lost River provide flood control for the Tule Lake Division and an irrigation supply for the Langell Valley Division. Their active storage capacities are 9*b3OO acre-feet and 513*300 acre-feet, respectively. Federally-financed project works also include the diversion, distribution, and drainage systems for the Main and Tule Lake Divisions; the diversion darn and main canals for the Langell Valley Division; and drainage outlets for the Lower Klamath and Tule Lake Divisions?
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"The goal of the project is to quantitatively describe the nature and extent of the ground-water flow systems in the basin."
Citation Citation
- Title:
- Upper Klamath Lake Basin nutrient-loading study: assessment of historic flows in the Williamson and Sprague Rivers
- Author:
- Risley, John C.
- Year:
- 1999, 2005, 2004
"The goal of the project is to quantitatively describe the nature and extent of the ground-water flow systems in the basin."
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Imprint from transmittal sheet; Distributed to depository libraries in microfiche; Shipping list no.: 97-0071-M; One ill. on 1 folded leaf in pocket; Includes bibliographical references
Citation Citation
- Title:
- Report of 1994 Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western United States
- Author:
- Workshop on the Correlation of Marine and Terrestrial Records of Climate Changes in the Western U.S. (3rd : 1994 : Watsonville, Calif.)
- Year:
- 1996, 2007, 2005
Imprint from transmittal sheet; Distributed to depository libraries in microfiche; Shipping list no.: 97-0071-M; One ill. on 1 folded leaf in pocket; Includes bibliographical references
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37. [Image] Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon
Abstract The Swan Lake-Yonna Valleys area consists of two intermountain valleys with their subordinate side valleys adjoining slopes, and mountainous boundary ridges, In all the area covered is about 256 ...Citation Citation
- Title:
- Geology and ground-water resources of the Swan Lake-Yonna Valleys area, Klamath County, Oregon
- Author:
- Meyers, Joseph D.
- Year:
- 1952, 2007, 2005
Abstract The Swan Lake-Yonna Valleys area consists of two intermountain valleys with their subordinate side valleys adjoining slopes, and mountainous boundary ridges, In all the area covered is about 256 square miles but the essential agricultural sections are restricted to the floors of Swan Lake and Yonna valleys with their respective subsidiary extensions of Pine Flats and Alkali Lake flats, a valley-floor area totaling about 90 square miles The floors of Swan Lake Valley and Yonna Valley lie at an altitude of about U52OO feet but the mountainous boundary ridges rise generally to 6000 feeto Yonna Valley is largely drained to Lost River by Buck Creek but also in part to Alkali Lakeo Swan Lake Valley and Pine Flats have only internal drainage. The Swan Lake Valley floor is the top of a deep alluvial fill, while Yonna Valley floor is mainly an erosional surface sloping to lines of through drainage Precipitation is about lit inches annually on the valley floors 9 but must be much more, possibly 18 to 24 inches, on the higher parts of the drainage basins. The growing season is short and killing frosts do occur in late spring and early fall. The rock units forming the bedrock structure of the area are consolidated or semiconsolidated rocks of Tertiary age and are largely of volcanic-flow and volcanic-sedimentary originc They consist of three main elements, a lower lava-rock unit, a sedimentary and volcanic-sedimentary unit, and an upper lava-rock unito The unconsolidated deposits are the older alluvium of Quaternary (and in part of late-Tertiary) age and the younger alluvium of Quaternary age0 The bedrock is faulted and deformed particularly so along a northwest-southeast set of fault lines that have given a remarkable linearity to the topography. Unpublished records subject to revision Ground water occurs below a regional water table that slopes south-ward to the level of the Lost Rivero The upper lava rocks and the lower lava rocks contain the principal permeable zones that occur beneath the areao Breccia and other porous zones in those rocks in places yield water to wells at a rate as large as 35OOO gallons per minute with but 1 or 2 feet of drawdowno The economical construction of irrigation wells requires the determination of the best possible location at which those rocks may be tapped at shallow depth below the level of the water tableo The ground water in general relatively low in dissolved mineral matter and is but slightly to moderately hard and would be considered chemically satisfactory for most uaeso Irrigation is the principal use of the ground water in the area north of the Horsefly Irrigation Districto There 3? wells supplied about 6,000 acre-feet of water to about 3800 acres of land in 1950. Water-level records obtained since 19U8 and approximations of the probable annual recharge from precipitation indicate that the present withdrawals are considerably less than the annual increment of the ground-water recharge, Rough estimates indicate that an increase in withdrawals of as much as 100 percent or more can take place before ground-water levels, by a persistent lowering, will begin to indicate that the annual replenishment is being exceeded.
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38. [Image] Klamath River Basin issues and activities
Klamath River Basin Issues and Activities: An Overview Summary The Klamath River Basin, an area on the California-Oregon border, has become a focal point for local and national discussions on water ...Citation Citation
- Title:
- Klamath River Basin issues and activities
- Author:
- Kyna Powers
- Year:
- 2005, 2008, 2006
Klamath River Basin Issues and Activities: An Overview Summary The Klamath River Basin, an area on the California-Oregon border, has become a focal point for local and national discussions on water management and water scarcity. Water and species management issues were brought to the forefront when severe drought in 2001 exacerbated competition for scarce water resources and generated conflict among several interests - farmers, Indian tribes, commercial and sport fishermen, other recreationists, federal wildlife refuge managers, environmental groups, and state, local, and tribal governments. The conflicts over water distribution and allocation are physically and legally complex, reflecting the varied and sometimes competing uses of limited water supplies in the Basin. For management purposes, the Basin is divided at Iron Gate Dam into the Upper and Lower Basins. As is true in many regions in the West, the federal government plays a prominent role in the Klamath Basin's water management. This role stems from three primary activities: (1) the operation and management of the Bureau of Reclamation's Klamath Water Project and Central Valley Project (e.g., Trinity River dams); (2) management of federal lands in the Basin, including five national wildlife refuges, several national forests, and public lands; and (3) implementation of federal laws, such as the Endangered Species Act (ESA), Clean Water Act (CWA), and National Environmental Policy Act (NEPA). Conflict was sparked in April of 2001 when the Bureau of Reclamation, which has supplied water to farms in the Upper Basin for nearly 100 years, announced that "no water [would] be available" for farms normally receiving water from the Upper Klamath Lake to avoid jeopardizing the existence of three fish species listed as endangered or threatened under the ESA. While some water was subsequently made available to some farmers from other sources (e.g., wells and other Bureau sources), many farmers faced serious hardships. During Reclamation's operations in September of 2002, warm water temperatures and atypically low flows in the lower Klamath contributed to the death of at least 33,000 adult salmonids. This die-off damaged fish stocks and the tribes, commercial fishermen, and recreational anglers that catch Klamath fish. There have been many studies, Biological Opinions, and operating plans over recent years, all of which have been controversial. The events of 2001 and 2002 prompted renewed efforts to resolve water conflicts in the Klamath Basin. Congress has responded to the controversy in a number of ways, including holding oversight hearings and appropriating funds for activities in the area. This report provides an overview of recent conflict in the Klamath Basin, with an emphasis on activities in the Upper Basin, and summarizes some of the activities taking place to improve water supply reliability and fish survival. This report will be updated as events warrant.
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"BLM/OR/WA/PL-02/038+1792"--P. [2] of cover; Cover title; Includes bibliographical references (v. 2, p. 219-228) and index
Citation Citation
- Title:
- Draft upper Klamath River management plan environmental impact statement and resource management plan amendments. Volume 2 - Appendices
- Author:
- United States. Bureau of Land Management. Klamath Falls Resource Area Office
- Year:
- 2003, 2004
"BLM/OR/WA/PL-02/038+1792"--P. [2] of cover; Cover title; Includes bibliographical references (v. 2, p. 219-228) and index
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The Oregon Plan for Salmon and Watersheds Biennial Report 2005-2007. This is the sixth report on the Oregon Plan for Salmon and Watersheds. The report provides an update on the accomplishments and continuing ...
Citation Citation
- Title:
- Oregon Plan for Salmon and Watersheds biennial report, 2005-2007
- Author:
- Oregon Watershed Enhancement Board
- Year:
- 2006, 2007
The Oregon Plan for Salmon and Watersheds Biennial Report 2005-2007. This is the sixth report on the Oregon Plan for Salmon and Watersheds. The report provides an update on the accomplishments and continuing efforts of people throughout Oregon to improve and protect clean water and recover and maintain healthy populations offish and wildlife in our watersheds. The Oregon Plan is unique because it engages communities in the restoration and long-term stewardship of their watersheds. This extraordinary effort encourages local partnerships and voluntary actions to improve the conditions of our watersheds. Over the years, these actions have made Oregon a national leader in local cooperative conservation. This report collects project and condition data, voluntary private lands restoration information, and agency program accomplishments under the Oregon Plan. Consistent with the past two reports, this document continues to provide specific data on each of the state's fifteen reporting basins. A new element to this report is the inclusion of stories about the people, partnerships, and on-the-ground projects that are benefiting watersheds and communities across the state. Thanks to the many Oregon Plan partners who contributed to this report. Thomas M. Byler Executive Director Oregon Watershed Enhancement Board
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SUMMARY The U.S. Geological Survey's program for geologic and hydrologic evaluation of physiographic provinces to identify areas potentially suitable for locating repository sites for disposal of high-level ...
Citation Citation
- Title:
- Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste [part 1 introduction and guidelines]
- Author:
- Bedinger, M. S.; Sargent, Kenneth A.; Reed, J. E.
- Year:
- 2008, 2005
SUMMARY The U.S. Geological Survey's program for geologic and hydrologic evaluation of physiographic provinces to identify areas potentially suitable for locating repository sites for disposal of high-level nuclear wastes was announced to the Governors of the eight States in the Basin and Range Province on May 5, 1981. Representatives of Arizona, California, Idaho, New Mexico, Nevada, Oregon, Texas, and Utah, were invited to cooperate with the Federal Government in the evaluation process. Each Governor was requested to nominate an Earth scientist to represent the State in a province working group composed of State and U.S. Geological Survey representatives. This report, Part I of a three-part report, provides the background, introduction and scope of the study. This part also includes a discussion of geologic and hydrologic guidelines that will be used in the evaluation process and illustrates geohydro-logic environments and the effect of individual factors in providing multiple natural barriers to radionuclide migration. Part II is a reconnaissance characterization of the geologic and hydrologic factors to be used in the initial screening of the Basin and Range Province. Part III will be the initial evaluation of the Province and will identify regions that appear suitable for further study. The plan for study of the Province includes a stepwise screening process by which successively smaller land units are considered in increasing detail. Each step involves characterization of the geology and hydrology and selection of subunits for more intensive characterization. Selection of subunits for further study is by evaluation of geologic and hydrologic conditions following a set of guidelines. By representation on the Province Working Group, the States participate in a consultation and review role in: (1) Establishing geologic and hydrologic guidelines, and (2) characterizing and evaluating the Province. The States also participate in compilation of geologic and hydrologic data used in characterizing the Province. The current (1983) needs for a high-level radioactive waste repository include: (1) Disposal in a mined repository; (2) re- trievability of the waste for as much as 50 years; and (3) confidence of isolation of the waste from the accessible environment. Isolation of the waste needs to be assured using geologic and hydrologic conditions that: (1) Minimize risk of inadvertent future intrusions by man; (2) minimize the possibility of disturbance by processes that would expose the waste or increase its mobility; and (3) provide a system of natural barriers to the migration of waste by ground water. The guidelines adopted by the Province Working Group are designed to provide a standard with which these conditions can be compared. The guidelines can be grouped into four principal categories: (1) Potential host media, (2) ground-water conditions, (3) tectonic conditions, and (4) occurrence of natural resources. Ideally the host medium constitutes the first natural barrier to migration of radionculides. The host medium ideally should be a rock type that prevents or retards dissolution and transport of radionuclides. Rocks in both the saturated and unsaturated zones may have desirable characteristics for host media. Rocks?other than the host?in the ground-water flow path from the repository ideally should be major barriers to radionuclide migration. Confining beds of low permeability might be present to retard the rate of flow between more permeable beds. Additionally, sorption of radionuclides by materials such as clays and zeolites in the flow path can further retard the flow of radionuclides by several orders of magnitude. Tectonic conditions in an area should not present a probable cause for exhumation or increased mobility of radioactive waste. Natural resources are a factor for consideration because of the problem of future human intrusion and exposure to radioactivity in the quest for minerals, oil, gas, water, and geothermal resources. The ultimate evaluation of the suitability of a geohydrologic environment for developing a mined repository needs to assess all geologic and hydrologic characteristics and their interaction in providing confidence that a geohydrologic environment will effectively isolate radionuclides from human access. Several hypothetical settings with typical geohydrologic conditions in the Basin and Range Province are used to illustrate the effect of multiple barriers in the isolation of radionuclides.
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43. [Image] Annual Report on the Project to Design and Experimentally Test an Improved Geothermal Drill Bit
Progress is reported in a research and development program to design, build, and test an improved geothermal drill bit. The major tasks of the Phase I effort are entitled: failure mechanisms of existing ...Citation Citation
- Title:
- Annual Report on the Project to Design and Experimentally Test an Improved Geothermal Drill Bit
- Author:
- Barker, L.M.
- Year:
- 1976
Progress is reported in a research and development program to design, build, and test an improved geothermal drill bit. The major tasks of the Phase I effort are entitled: failure mechanisms of existing bits; new steels and new bearing design; and new seals and lubricants. It appears that a significant gain in drill-bit life can be attained by the use of higher-temperature steels which retain more hardness at temperatures above 260/sup 0/C (500/sup 0/F). Such steels are available, and two research bits of high-temperature steels were made and will shortly be tested in a laboratory-simulated full-scale geothermal drilling environment. Two control bits of the same design, but made with conventional drill bit steels, were also obtained for identical laboratory test runs, so that the performance of the research bits can be meaningfully assessed. Base-line properties of the steels, such as hardness and fracture toughness as functions of temperature, are being measured to further assess the value of the high-temperature steels selected for the research bits. A geothermal test vessel was designed and fabricated in which the full-scale drill bits will be tested. The vessel is capable of temperature to 427/sup 0/C (800/sup 0/F) and pressures to 35 MPa (5,000 psi). Seal and lubrication designs were studied, and the state of the art in high-temperature seals and lubricants was assessed. Some candidate seals and lubricants have been obtained for testing, and others are being procured. In addition, a seal test vessel has been designed and will soon be completed which can simulate the geothermal drilling environment in full-scale testing of seal and lubricant designs and materials. (JGB)
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44. [Image] The Klamath Project
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"Prepared for Klamath Basin Ecosystem Foundation, and the Upper Williamson River Catchment Group, in cooperation with the Upper Klamath Basin Working Group, and the Klamath Watershed Council."
Citation Citation
- Title:
- Draft upper Williamson River Watershed assessment
- Author:
- David Evans and Associates, Inc.
- Year:
- 2004, 2005
"Prepared for Klamath Basin Ecosystem Foundation, and the Upper Williamson River Catchment Group, in cooperation with the Upper Klamath Basin Working Group, and the Klamath Watershed Council."
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AN ABSTRACT OF THE THESIS OF STEPHEN DOUGLAS REILING for the MASTER OF SCIENCE (Name) (Degree) in AGRICULTURAL ECONOMICS presented on (Major) (Date) Title: THE ESTIMATION OF REGIONAL ...
Citation Citation
- Title:
- The estimation of regional secondary benefits resulting from an improvement in water quality of Upper Klamath Lake, Oregon: an interindustry approach
- Author:
- Reiling, Stephen Douglas
- Year:
- 1971, 2006, 2005
AN ABSTRACT OF THE THESIS OF STEPHEN DOUGLAS REILING for the MASTER OF SCIENCE (Name) (Degree) in AGRICULTURAL ECONOMICS presented on (Major) (Date) Title: THE ESTIMATION OF REGIONAL SECONDARY BENEFITS RESULTING FROM AN IMPROVEMENT IN WATER QUALITY OF UPPER KLAMATH LAKE, OREGON; AN INTERINDUSTRY APPROACH Abstract approved^ Herbert H. Stoevener The primary objective of this study was to estimate the impact that an increase in recreational expenditures, resulting from water quality improvements of Klamath Lake, would have upon the Klamath County economy. As the sales of the economy expand to serve the needs of the recreationists, real benefits will be forthcoming to the businesses and households of the county in the forms of more business and higher incomes., To estimate the total impact of the increased volume of recreational expenditures that may be made in the economy, the economic relationships of the local economy h
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BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath ...
Citation Citation
- Title:
- Biological assessment of Klamath Project's continuing operations on the endangered Lost River sucker and shortnose sucker
- Author:
- United States. Bureau of Reclamation
- Year:
- 2001, 2005
BIOLOGICAL ASSESSMENT OF KLAMATH PROJECT'S CONTINUING OPERATIONS ON THE ENDANGERED LOST RIVER SUCKER AND SHORTNOSE SUCKER U.S. Bureau of Reclamation Mid-Pacific Region Klamath Basin Area Office Klamath Falls, Oregon February 13,2001 TABLE OF CONTENTS 1.0 INTRODUCTION 2 2.0 DESCRIPTION OF THE ACTION 3 3.0 DESCRIPTION OF HISTORIC OPERATIONS 6 4.0 ENDANGERED SPECIES POTENTIALLY AFFECTED BY THE KLAMATH PROJECT 16 5.0 ENVIRONMENTAL BASELINE 60 6.0 EFFECTS OF KLAMATH PROJECT ON BALD EAGLES 60 7.0 EFFECTS OF KLAMATH PROJECT ENDANGERED SUCKERS 63 8.0 PROPOSED CRITICAL HABITAT FOR ENDANGERED SUCKERS 82 9.0 CUMULATIVE EFFECTS 84 10.0 DETERMINATION OF EFFECTS 89 11.0 LITERATURE CITED 90 12.0 PERSONAL COMMUNICATIONS 100 13.0 APPENDIX 1 - ESA CONSULTATION REVIEW 101
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Recent Paleolimnology of Upper Klamath Lake Eilers et al. 2001 ABSTRACT Sediment cores were collected from Upper Klamath Lake in October, 1998 and analyzed for 210Pb, 14C, 15N, N, P, C, Ti, Al, diatoms, ...
Citation Citation
- Title:
- Recent paleolimnology of Upper Klamath Lake, Oregon
- Author:
- United States. Bureau of Reclamation
- Year:
- 2001, 2005
Recent Paleolimnology of Upper Klamath Lake Eilers et al. 2001 ABSTRACT Sediment cores were collected from Upper Klamath Lake in October, 1998 and analyzed for 210Pb, 14C, 15N, N, P, C, Ti, Al, diatoms, Pediastrum, and cyanobacterial akinetes. These results were used to reconstruct changes in water quality in Upper Klamath Lake over the last 150 years. The results showed that there was substantial mixing of the upper 10 cm of sediment, representing the previous 20 to 30 years. However, below that, 210Pb activity declined monotonically, allowing reasonable dating for the period from about 1850 to 1970. The sediment accumulation rates (SAR) showed a substantial increase in the 20th century. The increase in SAR corresponded with increases in erosional input from the watershed as represented by the increases in sediment concentrations of Ti and Al. The upper 20 cm of sediment (representing the last 150 years) also showed increases in C, N, P, and 15N. The increases in nutrient concentrations may be affected to various degrees by diagenetic reactions within the sediments, although the changes in concentrations also were marked by changes in the N:P ratio and in a qualitative change in the source of N as reflected in increasing S15N. The diatoms showed modest changes, particularly in the upper sediments, with increases in Asterionellaformosa, Stephanodiscus hantzschii, and S. parvus. Pediastrum, a green alga, was well-preserved in the sediments and exhibited a sharp decline in relative abundance in the upper sediments. Total cyanobacteria, as represented by preserved akinetes, exhibited only minor changes in the last 1000 years. However, a taxon which was formerly not present in the lake 150 years ago, Aphanizomenon, has shown major increases in recent decades. Although the mixing in the upper sediments prevents high-resolution temporal analysis of the recent history (e.g. last 30 years) of Upper Klamath Lake, the results demonstrate that major changes in water quality likely have occurred leading to a major modification of the phytoplankton assemblage. The changes in sediment composition are consistent with land use activities during this period that include substantial deforestation, drainage of wetlands, and agricultural activities associated with livestock and irrigated cropland.
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49. [Image] Geopressured Energy Resource Evaluation
The geopressured aquifers that extend along the northern Gulf of Mexico are a large, perhaps the largest, potential source of geothermal energy and natural gas in the US. Because of the high cost of completing ...Citation Citation
- Title:
- Geopressured Energy Resource Evaluation
- Author:
- Samuels, G.
- Year:
- 1979
The geopressured aquifers that extend along the northern Gulf of Mexico are a large, perhaps the largest, potential source of geothermal energy and natural gas in the US. Because of the high cost of completing wells into these formations and their relatively low temperatures (200 to 400 F), the utilization of the geothermal energy will be highly depend on, and of secondary importance to, the value of the methane. The economics of extracting either the geothermal energy or natural gas from these aquifers does not look promising. The combined requirements of high well flow rates (40,000 bbl/day), long life (20 years), and the necessity for close well spacing to minimize the cost of the collection system may be incompatible with the actual characteristics of the reservoirs. These factors place such stringent requirements on the reservoir size, permeability, and compressibility, or specific storage coefficient, that the number of promising production areas may be severely limited
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The Bureau of Reclamation (Reclamation) is the responsible Federal agency for operation of the Klamath Project (Project). Operation of the Project has been the subject of numerous previous consultations ...
Citation Citation
- Title:
- Biological assessment of the Klamath Project's continuing operations on southern Oregon/Northern California esu coho salmon and critical habitat for southern Oregon/northern California esu coho salmon
- Year:
- 2001, 2004
The Bureau of Reclamation (Reclamation) is the responsible Federal agency for operation of the Klamath Project (Project). Operation of the Project has been the subject of numerous previous consultations with the U.S. Fish and Wildlife Service (Service) and one with the National Marine Fisheries Service (NMFS) under Section 7 of the Endangered Species Act (ESA). Severe drought conditions in 1992 and 1994 and resultant associated shortages in project water supplies coupled with the 1997 listing of the southern Oregon/northern California (SONCC) coho salmon, Oncorhynchus kisutch, as threatened in the Klamath River downstream from the Project led to a review of Reclamation 19s operations. This biological assessment (BA) describes the effects on federally-listed species (i.e., coho salmon) and its designated critical habitat from on-going operation of the project based on historic operations, as described in this BA. The biological opinion (BO) addressing this BA and any subsequent BA amendments will be among the information that will inform the development of alternatives of the long-term operations plan and environmental impact statement (EIS). Reclamation is developing a long-term operations plan and EIS for the Project. The preferred alternative for implementation from the long-term operations plan would be the subject of a separate future ESA consultation. This BA describes the needs of anadromous fish with emphasis on SONCC coho salmon. It was developed using the best available scientific and commercial information on anadromous fish in the Klamath River. Coho salmon were listed as threatened on June 6, 1997 (NMFS 1997). The NMFS published a final rule designating critical habitat for SONCC coho salmon in May, 1999 (NMFS 1999a). Designated critical habitat for SONCC coho salmon encompasses accessible reaches of all rivers (including estuarine areas and tributaries) between the Mattole River in California and the Elk River in Oregon. Critical habitat includes all waterways, substrate, and adjacent riparian zones below longstanding, naturally impassable barriers. The areas upstream from Iron Gate Dam (IGD) (river mile 190) were not proposed critical habitat because areas downstream were considered sufficient for the conservation of the species. Reclamation has not evaluated whether the action that is the subject of this BA is consistent with its trust responsibility to Klamath Basin Indian Tribes. There are several important scientific reports and analyses (e.g., Phase II flow study) currently not available to Reclamation concerning threatened coho salmon, their habitat, and water quality as it relates to appropriate river flows that may be necessary to operate the Project consistent with the trust responsibility to Klamath Basin Indian Tribes. When this additional information becomes available, Reclamation intends to consider it during the development of the Project operations plans and include it in subsequent consultations with NMFS, as appropriate.
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The Endangered Species Act and Claims of Property Rights "Takings" Summary The federal Endangered Species Act (ES A) has long been one of the major flash points in the "property rights" debate. This ...
Citation Citation
- Title:
- The Endangered Species Act and claims of property rights "takings"
- Author:
- Meltz, Robert
- Year:
- 2005, 2008
The Endangered Species Act and Claims of Property Rights "Takings" Summary The federal Endangered Species Act (ES A) has long been one of the major flash points in the "property rights" debate. This report first outlines the ESA provisions most relevant to the act's impacts on private property, and then surveys the major ESA-relevant principles of Fifth Amendment takings law. The report then proceeds to its core topic: the court decisions adjudicating whether government measures based on the ESA effect a taking of property under the Fifth Amendment. The cases address four kinds of ESA measures: (1) restrictions on land uses that might adversely affect species listed as endangered or threatened; (2) reductions in water delivery to preserve instream flows needed by listed fish; (3) restrictions on the defensive measures a property owner may take to protect his/her property from listed animals; and (4) restrictions on commercial dealings in members of species acquired prior to listing as endangered or threatened. To date, only one of the 12 ESA-based takings decisions revealed by research has found a taking.
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52. [Image] Geothermal Investigations in Idaho. Part 8. Heat Flow Study of the Snake River Plain Region, Idaho
The Snake River Plain of Idaho has recent lava flows and a large number of thermal springs and wells. A heat flow study was initiated which, together with available geological and geophysical information, ...Citation Citation
- Title:
- Geothermal Investigations in Idaho. Part 8. Heat Flow Study of the Snake River Plain Region, Idaho
- Author:
- Brott, C.A.
- Year:
- 1976
The Snake River Plain of Idaho has recent lava flows and a large number of thermal springs and wells. A heat flow study was initiated which, together with available geological and geophysical information, allows a better definition of the geothermal resource and evaluation of the geothermal potential. Local geothermal anomalies were not the objects of this study and have not been studied in detail. The quality of the heat flow values obtained varies as interpretation was necessary to determine geothermal gradients for many of the holes which had disturbances. A major problem in determining the heat flow values is the lack of knowledge of the in situ porosity of the rocks. The heat flow values obtained for the Eastern Snake River Plain are from shallow wells (< 200 m), hence the heat flow there is low (< 0.5 HFU) because of the water movement in the Snake Plain aquifer. The anomalous regional heat flow pattern around the Snake River Plain, together with other geophysical and geological data, suggest the presence of a major crustal heat source. With the exception of the area of the Snake Plain aquifer, high geothermal gradients were found in all areas of southern Idaho (40 to 100/sup 0/C/km). Temperatures hot enough for space heating can be found most anywhere in the Plain at relatively shallow depths (1 to 2 km). Temperatures hot enough for electrical power generation (200/sup 0/C) can be found beneath southern Idaho almost anywhere at depths of 3 to 4 kilometers. The Plain is fault bounded and hot water circulating along the fault zones from depths can be a very important geothermal resource at shallow depths. The margins of the Plain have the highest heat flow values, are the most faulted, and have possibly the highest geothermal resource potential
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"July 2003."; "GAO-03-514."
Citation -
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TABLE OF CONTENTS PART I INTRODUCTION 18 - 11 History and ethnology 18 Irrigated area table 19 Cultural geography 19 General physiographic features 262e . .3 Physiographic areas and farming 1d CLIMATE ...
Citation Citation
- Title:
- Soils of the Klamath Indian Reservation; interim report, June 11, 1958
- Author:
- United States. Bureau of Indian Affairs
- Year:
- 1958, 2005, 2004
TABLE OF CONTENTS PART I INTRODUCTION 18 - 11 History and ethnology 18 Irrigated area table 19 Cultural geography 19 General physiographic features 262e . .3 Physiographic areas and farming 1d CLIMATE 182 - 18 Climatic table, Sprague River, Oregon 185 Precipitation table , Chiloquin, Oregon 186 Temperature table, Chiloquin, Oregon 187 Climatic table, Fort Klamath, Oregon 188 VEGETATION 189 - 25 GEOLOGY 196 - 51 Hydrography: rivers, lakes, marshes, ground water 196 Relief and geological formations. 262e .32 Diatomite - tuff formation 262e . 1c4 Pliocene sediments of the Modoc Point area 262e.. 37 Faulted tuff formation 1c9 Pumice tuff formation.. 1d0 Pumice mantle and pumice flows ........ 262e.... .........40 Table of chemical analyses of pumice and scoria 1d5 Geology Map 262e . 262e 221 BIBLIOGRAPHY 262e 262e...52 PART II DESCRIPTIONS OF SOILS 223 - 60 Classification and survey 262e 262e.. 262e... 53 Soil profile and nomenclature. .... 262e...53 Chestnut Soils 262e 224 "Western" Brown Forest Soils 225 Regosol Soils . . 262e. 262e......56 Solonetz Soils 262e.....57 Halomorphic Soils 262e 228 Hydromorphic Soils 262e... 229 Soil Association Map 262e 229 KEY TO SOIL SERIES 262e61 - 63 SOIL SERIES AND MAPPING UNIT DESCRIPTIONS 134 ~ 254 APPENDIX 1955 - 297 Soil Series and mapping unit index. 2620. . . . 255 Glossary of terms 263f 262e. . . . 272 Table of soil analyses (Oregon State College)... 1989 Table of irrigation water quality (Oregon State College) 1990 Table of conductivity and reaction. . . . 1991 Table of resistance of saturated paste 262e296
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24 p.; ill.; Title from cover
Citation Citation
- Title:
- Klamath County, Oregon: its resources and advantages, its present and its future; a land of great pines, hardy cattle, wonderful lakes and temperate climate; its productive land needs thousands of people for its proper development
- Author:
- Pierce, Joseph G.
- Year:
- 1900, 2006, 2005
24 p.; ill.; Title from cover
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57. [Image] Klamath Project : historic operation
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1 Acknowledgements 2 3 The completion of this work in large part can be attributed to the efforts of the 4 U.S. Fish and Wildlife Service Arcata Field Office staff and in particular to Mr. 5 Thomas Shaw ...
Citation Citation
- Title:
- Evaluation of Interim Instream Flow Needs in the Klamath River Phase II Final Report
- Author:
- Hardy, Thomas B; Addley. R. Craig
- Year:
- 2001, 2008, 2005
1 Acknowledgements 2 3 The completion of this work in large part can be attributed to the efforts of the 4 U.S. Fish and Wildlife Service Arcata Field Office staff and in particular to Mr. 5 Thomas Shaw for providing much of the supporting site-specific field data, 6 habitat mapping, and fisheries data used in the analyses. The efforts of the 7 various Tribal fisheries personnel were critical in supplying additional fisheries 8 collection data, and intensive site substrate and cover mapping. In particular, the 9 efforts of Tim Hayden, Charlie Chamberlain and Mike Belchik. USGS personnel 10 from the Midcontinent Ecological Science Center also provided valuable 11 assistance and field data used in the cross section based hydraulic and habitat 12 modeling. Mr. Gary Smith and Mike Rode of the California Department of Fish 13 and Game also provided critical information on site-specific habitat suitability 14 criteria and conceptual foundations for the escape cover analysis used in the 15 habitat simulations. Much of this work was also supported by work of Tim 16 Harden (Harden and Associates). The Bureau of Reclamation also provided 17 valuable input during the Phase II study process on Klamath Project operations. 18 A special thanks is also given to Mr. Mike Deas (U.C. Davis) for providing water 19 temperature simulations below Iron Gate Dam. The Technical Team also 20 provided critical input and review of all technical elements of this work as well as 21 providing reviews of the report. Finally, the completion of this work would not 22 have been possible without the tireless efforts of Jennifer Ludlow, Mark 23 Winkelaar, James Shoemaker, Shannon Clemens, Jerilyn Brunson, William 24 Bradford, Sarah Blake, Brandy Blank, Matt Combes, Leon Basdekas, and Aaron 25 Hardy at the Institute for Natural Systems Engineering, Utah State University. 26 27 Executive Summary 28 29 Previous instream flow recommendations developed as part of Phase I (Hardy, 30 1999) recommended interim instream flows in the main stem Klamath River 31 based on analyses of hydrology data. At that time, site-specific data suitable for 32 analysis and evaluation using habitat based modeling were not available. This 33 report details the analytical approach and modeling results from site-specific 34 studies conducted within the main stem Klamath River below Iron Gate Dam 35 downstream to the estuary. Study results are utilized to make revised interim 36 instream flow recommendations necessary to protect the aquatic resources 37 within the main stem Klamath River between Iron Gate and the estuary. This 38 report also makes specific recommendations for future research needs as part of 39 the on-going strategic instream flow studies being undertaken by the U.S. Fish 40 and Wildlife Service and collaborating private, local, state, federal, and tribal 41 entities. 42 43 This report was developed for the Department of the Interior (DOI) who provided 44 access to a technical review team composed of representatives of the U.S. Fish 45 and Wildlife Service, Bureau of Reclamation, Bureau of Indian Affairs, U.S. 46 Geological Survey, and the National Marine Fisheries Service. The technical Draft - Subject to Change 1 review team also included participation by the Yurok, Hoopa Valley, and Karuk 2 Tribes given the Departments trust responsibilities and the California Department 3 of Fish and Game as the state level resource management agency. The 4 technical review team provided invaluable assistance in the review of methods 5 and results used in the analysis, provided comments on draft sections of the 6 report, and provided data and supporting material for use in completion of the 7 Phase II report. In addition, several agencies and private individuals provided 8 written comments on the Preliminary Draft Report, which have been addressed in 9 this report where appropriate. 10 11 This report is organized to follow the general process used to implement the 12 technical studies. It first provides important background information on the 13 historical and current conditions of the anadromous species, highlights factors 14 that have contributed to their decline, provides an overview of the Phase I study 15 process and its principal findings. The report then continues with a description of 16 the Phase II technical study process. Key sections address methods and 17 findings for each technical component such as study design, study site selection, 18 field methods, analytical approaches, summary results, and recommended 19 instream flows. 20 21 The Phase II study relied on state-of-the-art field data collection methodologies 22 and modeling of physical habitat for target species and life stages of anadromous 23 fish. The field methods were directed toward achieving a three-dimensional 24 representation of each study site that incorporated between 0.6 to over one mile 25 of river depending on the specific study site. At each study site, a spatially 26 explicit substrate and vegetation map was developed and then integrated with 27 the three-dimensional channel topography in GIS. Fieldwork also involved 28 collection of hydraulic calibration data and fish observation data. The later 29 information was used in the development of habitat suitability criteria, conceptual 30 habitat model development and implementation, and habitat model validation 31 efforts. 32 33 Hydrology in the main stem Klamath River below Iron Gate Dam was estimated 34 differently for different purposes in Phase II. For example, we used simulated 35 unimpaired inflows (i.e., no depletions) to Upper Klamath Lake routed to Iron 36 Gate Dam with no Klamath Project imposed water demands. This simulated 37 scenario represents the best available estimates of the unimpaired flows below 38 Iron Gate Dam for the purposes of this study. The remaining flow scenarios 39 included the use of Upper Klamath Lake net inflows, historical Klamath Project 40 water demands, and the USFWS Biological Opinion (2000) target Upper Klamath 41 Lake water elevations. These scenarios represent different potential operational 42 flow scenarios as points of reference to the instream flow recommendations 43 developed as part of Phase II. Differences between these simulated flow 44 scenarios required the use of different models and/or modeling assumptions. 45 The assumptions and modeling tools are described in the appropriate technical 46 sections of the report. The estimated hydrology at each study site was used in Draft - Subject to Change 1 both the physical habitat modeling and temperature simulations using the USGS 2 Systems Impact Assessment Model (SIAM) or its components. 3 4 Physical habitat modeling at each study site relied on two-dimensional hydraulic 5 simulations that were coupled to three-dimensional habitat models. The 6 analytical form of the habitat models varied for spawning, fry, and 'juveniles' (i.e., 7 pre-smolts). These modeling results were compared to available 1-dimensional 8 cross section based hydraulic and habitat modeling at study sites that overlapped 9 between existing USFWS/USGS and Phase II studies. 10 11 Habitat suitability criteria for target species and life stages of anadromous fish 12 were developed from site-specific data for Chinook spawning, Chinook fry, and 13 steelhead 1+. These curves were validated both by field observations using the 14 habitat modeling results as well as by comparison to results from an individual 15 based bioenergetics model for drift feeding salmonids developed at USU. A 16 separate procedure was developed to obtain habitat suitability curves for Chinook 17 juvenile (i.e., pre-smolts), steelhead fry, and coho fry based on available 18 literature data. This approach used a systematic process to construct an 19 'envelope' habitat suitability curve that encompassed the available literature 20 curves. The overall process included a validation component that compared the 21 habitat versus discharge relationships between envelope curves to the site- 22 specific curves for Chinook spawning, Chinook fry, and steelhead 1+. The results 23 validated the use of the envelope curves for use as interim criteria pending 24 further research and development of site-specific curves for these species and 25 life stages within the Klamath River. 26 27 Habitat modeling involved the integration of substrate and cover mapping with 28 the three-dimensional topography and hydraulic properties at each study site with 29 the habitat suitability curves. Habitat modeling was undertaken for Chinook 30 spawning, fry, and juveniles, coho fry and juveniles, and steelhead fry and 31 steelhead 1+. Different habitat models were developed for spawning, fry, and 32 juveniles. The study generated a salmonid fry habitat model that incorporated a 33 distance to escape cover that also required sufficient depth within the escape 34 cover in order for it to be utilized at a given flow rate. This model also 35 incorporated quantitative differences in the type of escape cover. 36 37 The habitat modeling results for each species and life stage were validated 38 against the spatial distribution of each species and life stage surveyed at study 39 sites at different flow rates. These results generally demonstrated that the 40 integrated habitat modeling was validated for the study in terms of spawning and 41 fry life stages. Our assessment of the pre-smolt or juvenile life stage results is 42 that they are consistent for the existing habitat model assumptions. However, we 43 discuss what we perceive to be inherent biases in these results (juveniles) based 44 on the existing habitat model structure and make specific recommendations of 45 what additional work would likely improve the results for this particular life stage. 46 Draft - Subject to Change jjj 1 Temperature simulations based on the unimpaired flow regime below Iron Gate 2 Dam were conducted with HEC5Q as part of the SIAM applications. These 3 results supported the findings in Phase I that flows lower than ~ 1000 cfs during 4 the late summer would likely increase the environmental risk to anadromous 5 species due to almost continual exposure to chronic temperature thresholds. We 6 believe that these simulation results show that there is very little flexibility for 7 reservoir operations at Iron Gate Dam to mitigate deleterious flow dependent 8 temperature effects. This finding has previously been reported by the USGS 9 (Bartholow 1995) and Deas (1999). 10 11 The integration of the habitat modeling with the unimpaired hydrology was used 12 to develop habitat reference values for target species and life stages at each 13 study reach on a monthly basis for flow exceedence ranges between 10 and 90 14 percent. The reference habitat value was computed as the percent of maximum 15 habitat associated with the unimpaired flow values for each species and life 16 stage on a monthly basis. This reference habitat value was used as one 'target' 17 condition to guide the selection of monthly flow recommendations at a given 18 exceedence flow level. 19 20 The flow recommendation process also employed a prioritization of species and 21 life stages to be considered within the year and/or within a specific month. The 22 prioritization of life stages was taken from the life history sequence of 23 anadromous species (i.e., spawning, fry, and then juveniles). The initial priority 24 order for species was defined as Chinook, then coho, and finally steelhead. It is 25 stressed that this initial prioritization was used to conceptually simplify the flow 26 recommendation process only, and that all species and life stages were 27 examined as part of the overall analysis. The process then relied on an iterative 28 procedure to select target flows for each month at a given exceedence level. 29 This procedure attempted to pick a target flow that would simultaneously 30 preserve the underlying characteristics of the seasonal unimpaired hydrograph at 31 that exceedence flow, the underlying relationship of the unimpaired hydrograph 32 between all exceedence flow levels, while striving to maximize habitat for the 33 priority species and life stages relative to the unimpaired habitat reference 34 conditions. The corresponding monthly flow rates at each exceedence level 35 were then used to compute the percent of maximum habitat for all other species 36 and life stages in a given month. These values were then compared to their 37 respective unimpaired habitat values to ensure that adequate protection of 38 habitat for non-priority species and life stages remained reasonable. 39 40 The flow recommendations developed in the Iron Gate to Shasta River Reach 41 were 'propagated' downstream to each successive reach by addition of the reach 42 gains as presently defined by the USGS in their MODSIM module of SIAM. It is 43 recognized that these reach gains reflect existing depletions in tributary systems 44 (e.g., Shasta and Scott Rivers) but are the only estimates presently available for 45 use in the simulation models for the system. The flow recommendations for each 46 river reach were then used to compute the percent of maximum habitat on a Draft - Subject to Change 1 monthly basis for each species and life stage. The recommended flow based 2 calculation of percent of maximum habitat for each species and life stage was 3 then compared against the associated unimpaired flow based habitat values. 4 5 Although flow recommendations were developed for the 10 to 90 percent 6 exceedence range (i.e., nine water year types), five water year types were 7 identified representing Critically Dry, Dry, Average, Wet, and Extremely Wet 8 inflow conditions for Upper Klamath Lake. These water year classifications 9 parallel those developed for the Trinity River and were used as operational 10 definitions in the Phase I report. Furthermore, the USBR KPSIM model was 11 modified to use this five-water year type format for simulating operations under 12 different instream flow requirements below Iron Gate Dam. The 90, 70, 50, 30, 13 and 10 percent exceedence flow levels were assigned to each of these water 14 year types, respectively (i.e., critically dry to extremely wet). This assignment 15 was used to demonstrate several key points regarding the use of 16 recommendations at this level of resolution (i.e., five water year types) and how 17 the existing operational models for the Klamath Project simulate flow scenarios. 18 19 These five water year type dependent recommendations were utilized in the U.S. 20 Bureau of Reclamation's Klamath Project Simulation Module (KPSIM) to simulate 21 project operations over the 1961 to 1997 period of record. This analysis 22 confirmed that the project could be operated to achieve these recommendations 23 in all but 19 of the 468 simulated months in this period of record. These results 24 also highlighted that an alternative water year 'classification' strategy for 25 specifying instream flows should be considered in lieu of a five water year type 26 scheme. We provide a specific recommendation of how this could be 27 approached based on the instream flow recommendations developed in Phase II. 28 29 30 Draft - Subject to Change
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The object of the Marysville Geothermal Project is to investigate a region of abnormally high geothermal heat flow near Marysville, MT, about 20 miles northwest of Helena. The research should determine ...
Citation Citation
- Title:
- The Marysville, Montana Geothermal Project (Revised)
- Author:
- McSpadden, W.R.
- Year:
- 1974
The object of the Marysville Geothermal Project is to investigate a region of abnormally high geothermal heat flow near Marysville, MT, about 20 miles northwest of Helena. The research should determine the nature and size of the resource, how the energy might be extracted, the potential monetary value of the energy, and how similar resources elsewhere might be located. The heat source was expected to be a granitic pluton or magmatic intrusion, 10,000 to 40,000 years old, with temperatures in the range of 300 to 500°C. Originally it was thought that the pluton was at relatively shallow depths, but at present its depth and exact location are unknown
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INTRODUCTION AND GENERAL General Description of the Project Location. The Klamath Project is in the Upper Klamath River Basin, east of the Cascade Range. It is located in Klamath County, Oregon, and ...
Citation Citation
- Title:
- Annual project history: Klamath Project, Oregon-California, 1957
- Author:
- United States. Bureau of Reclamation
- Year:
- 1957, 2008, 2006
INTRODUCTION AND GENERAL General Description of the Project Location. The Klamath Project is in the Upper Klamath River Basin, east of the Cascade Range. It is located in Klamath County, Oregon, and in Modoc and Siskiyou Counties of California. Project headquarters is located at the principal city of Klamath Falls, Oregon, which has a population of about 35>700, including suburbs. Smaller towns on the project in Oregon are Merrill, Malin, and Bonanza. The town of Tulelake, California, was established in 1931 near the center of the Tule Lake Division. Climate. The mean temperature for the wannest month is 630 F. The coldest month has mean temperature of 29? F. Summer nights are cool. The annual rainfall is about 13 inches, of which about 3?-inches fall during the growing season of 90 to 130 days. Topography, soils, and crops. The project area is about ^-,100 feet elevation above sea level. The surface topography is generally smooth and flat for the large areas of lake bottom, and gently sloping on the higher lands. Peat and muck soils are common in the recent lake bottoms. Soils vary from sandy loam to clay on other parts of the project. The principal crops grown are alfalfa, malting and feed barley, potatoes, clover seed, and irrigated pasture and other forage. Stock raising is an important enterprise. Industry and transportation. Farming and lumbering each provide the major portion of the economy of the Basin. Three major railroad lines, one major highway and many secondary highways, and two airlines serve the project area. Plan and purpose. The project serves 211,000 acres. The water supply is provided by two main water courses, Klamath River and Lost River and their tributaries. Besides storing, diverting, and distributing water for irrigation, project facilities have reclaimed by drainage large areas formerly inundated by Lower Klamath and Tule Lakes* Flood waters of Lost River, which terminates in Tule Lake, are diverted to the Klamath River through the Lost River Diversion Channel. This channel is also used to carry irrigation water in the opposite direction in the summertime. Another principal function of the project is water-level control for the Tule Lake and Lower Klamath Lake National Wildlife Refuges. Upper Klamath Lake on the Klamath River is the principal storage reservoir, having an active capacity of 52U,800 acre-feet. It is controlled by Link River Dam constructed, maintained, and operated INTRODUCTION AND GENERAL (Continued) General Description of the Project (Cont.) by The California Oregon Power Company under an agreement with the project whereby irrigation requirements and rights are protected. The Main, Lower Klamath, and Tule Lake Divisions are served from this source, Gerber Reservoir on Miller Creek and Clear Lake Reservoir on Lost River provide flood control for the Tule Lake Division and an irrigation supply for the Langell Valley Division. Their active storage capacities are 9*^300 acre-feet and 513*300 acre-feet, respectively. Federally-financed project works also include the diversion, distribution, and drainage systems for the Main and Tule Lake Divisions; the diversion dam and main canals for the Langell Valley Division; and drainage outlets for the Lower Klamath and Tule Lake Divisions.
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Determining Surface Water Availability in Oregon By Richard M. Cooper, PE Abstract The Oregon Water Resources Department (Department or OWRD) limits appropriation from Oregon streams to assure new applicants ...
Citation Citation
- Title:
- Determining surface water availability in Oregon : open file report SW 02-002
- Author:
- Oregon. Water Resources Dept.
- Year:
- 2002, 2005
Determining Surface Water Availability in Oregon By Richard M. Cooper, PE Abstract The Oregon Water Resources Department (Department or OWRD) limits appropriation from Oregon streams to assure new applicants use of surface water a reasonable amount of time and to minimize regulatory conflict. The standards for new appropriation of water are: (1) consumptive use from allocations for out-of-stream uses can total no more than the 80-percent ex-ceedance natural stream flow, and (2) allocations for in-stream flows can be no more than the 50-percent exceedance natural stream flow. OWRD has created and maintains a database of the amount of surface water available for appropriation for most waters in the state. This database is used to evaluate applications for new uses of water. Water availability (WA) is obtained from natural stream flow (QNSF) by subtracting existing storage (ST), out-of-stream consumptive uses (CU) and in-stream demands (IS). WA = QN -ST-CU-IS Ideally, water availability would be calculated for every watershed above a point of diversion or in-stream demand. Practically, the number of watersheds must be limited. The watersheds selected for analysis are called Water Availability Basins (WABs). Stream flow can be highly variable, and it is useful to characterize it in some way, usually by a statistic, e.g., a monthly or annual mean. For water availability, it is important to know how often water is available. The appropriate statistic in this case is exceedance stream flow. This statistic tells us how often to expect a given rate of stream flow to occur. Exceedance stream flows are determined directly from gage records, or for ungaged streams, by estimation through modeling. When determined from gage records, the exceedance flows must be corrected to a common base period, and then, to natural stream flow. When determined through modeling, the exceedance flows are estimated from statistical models that relate watershed characteristics to natural stream flow. The models are derived by multiple linear regression. Storage is water retained in a reservoir. It is debited from water availability when the water is stored. It diminishes availability both upstream and downstream of the point of diversion. Consumptive use is divided into three major categories: irrigation, municipal, and all others e.g., domestic, livestock. These uses are less than 100 percent consumptive. It is assumed the non-consumed part of a diversion is returned to the stream from which it was diverted. Consumptive use from irrigation is from estimates made by the US Geological Survey (Portland). Consumption from other uses is based on the associated water rights. In these cases, consumptive use is obtained by multiplying the maximum diversion rate allowed for the water right by a consumptive use coefficient. Consumptive use diminishes availability both upstream and downstream of the point of diversion. There are two types of in-stream demands: in-stream water rights and scenic waterway flows. In-stream demands diminish availability upstream only. Because they are non-consumptive, they do not diminish stream flow downstream as do consumptive uses. Water availability has been calculated for over 2500 WABs. In general, the calculation of water availability at one WAB cannot be considered in isolation from other WABs in the same stream system. For water to be available at any given upstream point, it must be available at all points of calculation downstream.
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The oxidation-reduction (known as redox) electrode was studied in a pH range corresponding to that found in a CO/sub 2/-silicate buffered system at temperatures ranging from 100 to 250/sup 0/C. Oxidizing ...
Citation Citation
- Title:
- Development of the high-temperature redox electrode. Interim report ending March 1980
- Author:
- Danielson, M.J.
- Year:
- 1980
The oxidation-reduction (known as redox) electrode was studied in a pH range corresponding to that found in a CO/sub 2/-silicate buffered system at temperatures ranging from 100 to 250/sup 0/C. Oxidizing conditions were created by injecting oxygen; the greatest reducing conditions, by using hydrogen. The sulfur system (H/sub 2/S, HS/sup -/, S/sup 2/) was not examined at this time, but future work will include this system since it is an important component of the geothermal brine. Both a platinized platinum (Pt-Pt) and a bare platinum (Pt-foil) electrode respond to the redox environment. The response does not appear to indicate thermodynamic equilibrium with the chemical environment; instead a mixed potential response is indicated. The difference in potential between a strong oxidizing environment (0.4-ppM O/sub 2/) and a strong reducing environment (0.5-atm H/sub 2/) is typically > 1 volt at all temperatures. The magnitude of this response makes the platinum electrode a suitable sensor for continuous monitoring of the geothermal environment for oxygen intrusions. The platinized platinum redox electrode is superior to the bare platinum electrode; PNL-3377
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SIGNIFICANT FINDINGS The distribution of SOD2q values (measured sediment oxygen demand values corrected to 20°C [degrees Celsius]) had a median value of 1.6 g/m2/day (grams per square meter per day) in ...
Citation Citation
- Title:
- Sediment oxygen demand in Upper Klamath and Agency Lakes, Oregon, 1999
- Author:
- Wood, Tamara M.
- Year:
- 2001, 2005, 2004
SIGNIFICANT FINDINGS The distribution of SOD2q values (measured sediment oxygen demand values corrected to 20°C [degrees Celsius]) had a median value of 1.6 g/m2/day (grams per square meter per day) in the spring and 1.7 g/m2/day in the late summer. These values were well within the range of values in the literature for sites with similar sediment characteristics: primarily silty with at least a moderate amount of organic content. Over most of the lake there appears to be relatively little variation in SOD 14the interquartile range in values was 0.4 g/m2/day in the spring and 0.7 g/m2/day in the late summer. A significant exception was apparent in Ball Bay, where SOD in the late summer was greater than 10.2 g/m2/day. In the absence of primary production, an SOD of this magnitude could deplete the water column of oxygen in a few days. This measurement provided evidence that localized areas of very high SOD occur episodically in the bays, perhaps associated with large algal mats being trapped by the lake circulation patterns. A statistical test for a spring to late summer difference in the median values of SOD confirmed that SOD in the late summer (median value 1.7 g/m2/day) was significantly higher than in the spring (median value 1.2 g/m2/day). The difference was primarily due to seasonal changes in temperature; when SOD values were corrected to 20°C, there was no seasonal difference in the median values. There was no correlation between SOD20 and the sediment characteristics measured in this study: percent fines, organic carbon, and residue lost on ignition.
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CONTENTS Statement of?©ag!, Anklin, William 2620 115 Barnett, Hon. Leo, Judge, Gilliam County, Oreg 2620 196 Chapman, James, president, Klamath Cattlemen's Association, Inc., Klamath Falls, Oreg ...
Citation Citation
- Title:
- Effects of the drought on small business and agriculture : hearings before the Select Committee on Small Business, United States Senate, Ninety-fifth Congress, first session ... Klamath Falls, Oreg., August 16, 1977, Burns, Oreg., August 17, 1977
- Author:
- United States. Congress. Senate. Select Committee on Small Business
- Year:
- 1977, 2005, 2004
CONTENTS Statement of?©ag!, Anklin, William 2620 115 Barnett, Hon. Leo, Judge, Gilliam County, Oreg 2620 196 Chapman, James, president, Klamath Cattlemen's Association, Inc., Klamath Falls, Oreg 269 112 Cockram, Fred J., president, Oregon Dairymen's Association 2620 116 Cody, Jim, District Director, Farmers Home Administration, Port land, Oreg 2620 184 Eisgruber, Ludwig M., professor and head of the Department of Agri cultural and Resource Economics, School of Agriculture, Oregon State University 2620 118 Flitcraft, Hon. George C, Mayor, city of Klamath Falls, Klamath Falls, Oreg 2620 1 Fujii, Howard, manager, Public Affairs, Oregon Farm Bureau Fed eration 2620 170 Gift, Lloyd 2620 110 Goertzen, Victor, Assistant District Director, Management Assistance, Boise District Office, U.S. Small Business Administration 2620 189 Graham, Jack, coordinator, Agricultural Drought Office, State of Oregon 2620 174 Hagelstein, Fred, assistant director, Oregon State University Exten sion Service, Corvallis, Oreg 2620 39 Hawkins, Bert, president, Oregon Cattlemen's Association, Ontario, Oreg 2620 5 Hernandez, Richard, Associate Administrator for Operation- U.S. Small Business Administration, accompanied by J. Don Chapman, District Director, Portland District Office, SBA 2620 74 Huff, Bert, regional vice president, First National Bank of Oregon, Portland, Oreg 2620 129 Johnson, Samuel, member of the legislature, Klamath County, Oreg 2620 5 Langley, Dwight, representing Baker County Livestock Association, Baker, Oreg 2620 157 Mayer, William H., Regional Director, Federal Disaster Assistance Administration, Region 10, Seattle, Wash 2620 94 Miller, Tad, president, Oregon Wheat Growers League, Pendleton, Oreg., accompanied by Wes Grilley 2620 160 Nicholson, Mr 2620 110 Otley, Charles, past president, Oregon Cattlemen's Association 2620 196 Ross, Bill, first vice president, Oregon Cattlemen's Association 2620 146 Sehorn, Talbert D., State Executive Director, Agricultural Stabiliza tion and Conservation Service, U.S. Department of Agriculture 2620 103 Sitz, James H., president, Harney County Stockgrowers, Drewsey, Oreg 2620 197 Skinner, Bob, president, Malheur County Livestock Association 2620 151 Smith, Earl, member, State Department of Agriculture, Salem, Oreg 2620 140 Storms, Murl W., State Director, Oregon State Office, Bureau of Land Management, Portland, Oreg 2620 65 Thorne, Raymond P., Board of County Commissioners, County Commissioners Chambers, Klamath County Courthouse Annex, Klamath Falls, Oreg 2620 2 White, Hon. Dale, County Judge for Harney County, Burns, Oreg- 2620 134 Williams, Gary, representing the Oregon Wool Growers Association._ 21 Zinn, Thomas G., Wasco County Extension Agent, Oregon State Uni versity Extension Service 2620 48 (in) IV APPENDIX Statement of Edward Peile, president, Jackson County Stockmen's As- sociation 2620 201 Statement of Mike Hanley, Jordan Valley, Oreg 2620 201 Statement of Gene Officer, president, Grant County Stockgrowers Asso ciation, Canyon City, Oreg 2620 204 HEARING DATES August 16, 1977: Afternoon session 2620 1 August 17,1977: Afternoon session 2620 133
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67. [Image] Lakeview proposed resource management plan and final environmental impact statement [volume 1]
4 v.; maps (some col.); "August 2002"; "January 2003" -- coverCitation Citation
- Title:
- Lakeview proposed resource management plan and final environmental impact statement [volume 1]
- Author:
- U.S. Department of the Interior. Bureau of Land Management; Lakeview Resource Area Office. Lakeview District
- Year:
- 2002, 2006, 2005
4 v.; maps (some col.); "August 2002"; "January 2003" -- cover
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68. [Image] Seeking refuge: making space for migratory waterfowl and wetlands along the Pacific Flyway
Abstract "Seeking Refuge" examines the history of migratory waterfowl management along the Pacific Flyway, the westernmost of four main migration routes in North America. Drawing on approaches from historical ...Citation Citation
- Title:
- Seeking refuge: making space for migratory waterfowl and wetlands along the Pacific Flyway
- Author:
- Wilson, Robert Michael
- Year:
- 2003, 2005, 2004
Abstract "Seeking Refuge" examines the history of migratory waterfowl management along the Pacific Flyway, the westernmost of four main migration routes in North America. Drawing on approaches from historical geography and environmental history, this study shows how wildlife officials developed migratory bird refuges in Oregon and California, where over 60 percent of Pacific Flyway waterfowl winter. During the early-twentieth century, reclamation and river diking eliminated most of the wetlands in the birds' wintering range. Bird enthusiasts such as bird watchers and duck hunters successfully lobbied for the creation of wildlife refuges in a few areas along the flyway. These early refuges failed to protect waterfowl habitat and they were severely degraded by reclamation. In the 1930s and 1940s, the U.S. Fish and Wildlife Service (FWS) and its predecessor, the Bureau of Biological Survey, undertook an ambitious program to resurrect these sanctuaries and to create new ones. Many farmers opposed these refuges out of fear that waterfowl would damage crops. To respond to these concerns and to ensure an adequate food supply for the birds, the FWS raised rice, barley, and other grains. The agency adopted many of the technologies of modern, industrial agriculture including synthetic herbicides and insecticides such as 2, 4-D and DDT. By the 1960s, the refuges had become largely mirrors of the surrounding irrigated farmlands, the main difference being that the FWS raised grain for waterfowl rather than for market. Refuges could not escape the agricultural settings in which they were embedded. As units within the irrigated countryside, Pacific Flyway refuges were often at the mercy of nearby farmers and federal reclamation agencies. Poor water quality and insufficient supplies of water often hampered FWS efforts to manage refuges. In the late-twentieth century, reduced water supply due to diversions to California municipalities and to sustain endangered fish species affected the amount of water reaching refuges. This dissertation has other goals. First, it critiques the anthropocentrism of most historical geography by focusing on how political, cultural, and ecological factors affected wildlife. Second, it contributes to the literature on the state's role in environmental protection by investigating the overlapping, and often contradictory, spaces within which wildlife managers implemented environmental regulations.
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ill., maps; Final report in partial satisfaction of cooperative agreement CA-9000-8-0007, subagreement 7, National Park Service, Pacific Northwest Region; "Autumn 1988."
Citation Citation
- Title:
- Prescribed fire effects in the Panhandle area, Crater Lake National Park
- Author:
- Swezy, Michael; Agee, James K
- Year:
- 1988, 2008
ill., maps; Final report in partial satisfaction of cooperative agreement CA-9000-8-0007, subagreement 7, National Park Service, Pacific Northwest Region; "Autumn 1988."
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iii; 99p.; "Printed for the use of the Committee on Energy and Natural Resources"; Distributed to some depository libraries in microfiche
Citation Citation
- Title:
- Water Symposium: Symposium before the Committee on Energy and Natural Resources, United States Senate, One Hundred Ninth Congress, First Session, on Water Issues, April 5, 2005
- Author:
- Water Symposium (2005: Washington, D.C.)
- Year:
- 2005, 2006
iii; 99p.; "Printed for the use of the Committee on Energy and Natural Resources"; Distributed to some depository libraries in microfiche
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71. [Image] Field Electrochemical Measurements of Corrosion Characteristics of Materials in Hypersaline Geothermal Brine
A flow cell (with appropriate accessories) was developed for use in short-term testing of the corrosion behavior of materials in approximately 100{sup 0}C, hypersaline geothermal brine. The apparatus was ...Citation Citation
- Title:
- Field Electrochemical Measurements of Corrosion Characteristics of Materials in Hypersaline Geothermal Brine
- Author:
- Harrar, J.E.
- Year:
- 1977
A flow cell (with appropriate accessories) was developed for use in short-term testing of the corrosion behavior of materials in approximately 100{sup 0}C, hypersaline geothermal brine. The apparatus was designed to accommodate commercial (Petrolite) corrosion measurement equipment and conducted experiments on-line at the Lawrence Livermore Laboratory Test Station in the Salton Sea Geothermal Field. The apparatus also permitted direct readings of corrosion potentials, solution redox potential (E{sub h}), brine flow rate, pH, and temperature. Estimates of general corrosion rates were obtained by the linear polarization resistance technique and from measurements of complete potentiodynamic polarization curves. The latter also afforded predictions of pitting susceptibilities of active-passive type materials. Twenty-two alloys (with various heat treatments) were tested and readily grouped according to general corrosion resistances in acidified hypersaline (approximately 4 M chloride) brine. Especially promising in regard to corrosion resistance-vs-cost is the series of low Cr--Mo steels. Prescaling of materials in unacidified (pH approximately 5.7) brine prior to exposure to acidified (pH 2 to 4.5) brine was found to be beneficial in reducing corrosion rates at 100{sup 0}C
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72. [Image] Relation between selected water-quality variables and lake level in Upper Klamath and Agency Lakes, Oregon
Relation Between Selected Water-Quality Constituents and Lake Stage in Upper Klamath and Agency Lakes, Oregon By Tamara M. Wood, Gregory J. Fuhrer, and Jennifer L. Morace SUMMARY Upper Klamath Lake is ...Citation Citation
- Title:
- Relation between selected water-quality variables and lake level in Upper Klamath and Agency Lakes, Oregon
- Author:
- Wood, Tamara M.
- Year:
- 1996, 2005, 2004
Relation Between Selected Water-Quality Constituents and Lake Stage in Upper Klamath and Agency Lakes, Oregon By Tamara M. Wood, Gregory J. Fuhrer, and Jennifer L. Morace SUMMARY Upper Klamath Lake is a large (140 square-mile), shallow (mean depth about 8 ft) lake in south-central Oregon that the historical record indicates has been eutrophic since its discovery by non-Native Americans. In recent decades, however, the lake has had annual occurrences of near-monoculture blooms of the blue-green alga Aphanizomenon flos-aquae. In 1988 two sucker species endemic to the lake, the Lost River sucker (Deltistes luxatus) and the shortnose sucker (Chasmistes brevirostris), were listed as endangered by the U.S. Fish and Wildlife Service, and it has been proposed that the poor water quality conditions associated with extremely long and productive blooms are contributing to the decline of those species. It has also been proposed that the low lake levels made possible by the construction of a dam at the outlet from the lake in 1921 have contributed to worsening water quality through a variety of possible mechanisms (Jacob Kann, Klamath Tribes, written com-mun., 1995). One such mechanism would be an increase in internal phosphorus loading from resuspended sediments (Jacoby and others, 1982), resulting from an increase in bottom shear stresses at lower lake levels (Laenen and LeTourneau, 1996), leading in turn to more intense algal blooms. Another possible mechanism is an earlier triggering of algal blooms. When early spring lake levels are low, greater light intensity at the sediment surface might speed recruitment of algal cells from the sediments. Sediment recruitment has been shown to be an important contributor to water column biomass increases in A. flos aquae (Barbiero and Kann, 1994) and Gloeotrichia echinulata (Barbiero, 1993). An earlier bloom could result in poor water quality conditions occurring earlier in the year, when young-of-the-year fish may be more susceptible to those conditions. Lake level can also influence water quality directly. An increased frequency of sediment resuspension at lower lake levels could increase chemical and biological oxygen demand, resulting in decreased dissolved oxygen concentrations. Sediment oxygen demand also may be enhanced at lower lake levels because it is concentrated over a smaller volume of water. Some compensation for increased oxygen demand at lower lake levels might be provided by increased reaeration, if the water column mixes from top to bottom more frequently. Based on the analysis of data that they have been collecting for several years, the Klamath Tribes recently recommended that the Bureau of Reclamation (Reclamation) modify the operating plan for the dam to make the minimum lake levels for the June-August period more closely resemble pre-dam conditions (Jacob Kann, written commun., 1995). The U.S. Geological Survey (USGS) was asked to analyze the available data for the lake and to assess whether the evidence exists to conclude that year-to-year differences in certain lake water-quality variables are related to year-to-year differences in lake level. The results of the analysis will be used as scientific input in the process of developing an operating plan for the Link River Dam. Datasets Two water-quality datasets were analyzed. The first was a series of hourly records of pH, dissolved oxygen, and water temperature, each of approximately a week's duration. The records were collected at 3 sites over 3 years, 1992 through 1994, with enough consistency to define the seasonal patterns. This dataset provided information about the diel extremes in dissolved oxygen and pH and the seasonal pattern in the diel cycle, but measurements were limited to a depth of 1 m(3.28 ft). The second dataset was a set of depth profiles of pH and dissolved oxygen and concurrent depth-integrated samples for nutrients and chlo-rophyll-a. The profiles were collected at approximately biweekly intervals at nine sites (seven in Upper Klamath and two in Agency Lake) over the 5 years 1990 through 1994. These depth profiles provided information on the depth-dependence of dissolved oxygen and pH, and allowed more extensive year-to-year comparisons than did the hourly records. Because measurements were made at each site only once during the sampling day, however, they did not capture the daily extremes in water quality. Lake level is measured daily by the USGS at three sites around the lake: Rocky Point, Rattlesnake Point, and near the city of Klamath Falls. These daily measurements are then used to compute a spatially weighted average of the lake level that is reported in the USGS annual Water-Data Report for Oregon. The average lake levels were used in this report. Two climatic datasets were used in this report; both were collected at the Klamath Falls airport. Air temperature was recorded as a daily maximum and daily minimum value. Cloud cover was quantized on a daily basis into one of seven levels. Because the focus of this study was primarily to examine possible relations between water quality and lake level, the lake level data provide an important context for the discussions that follow.
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This report is a review of scientific research done by various organizations involved in the Klamath Reclamation Project to assess the "status and management of coho salmon in the Klamath River and . . ...
Citation Citation
- Title:
- IMST review of the USFWS and NMFS 2001 biological opinions on management of the Klamath Reclamation Project and related reports: a report of the Independent Multidisciplinary Science Team, Oregon Plan for Salmon and Watersheds
- Author:
- Independent Multidisciplinary Science Team (Oregon)
- Year:
- 2003, 2004
This report is a review of scientific research done by various organizations involved in the Klamath Reclamation Project to assess the "status and management of coho salmon in the Klamath River and . . . management of Upper Klamath Lake and its watershed"; "April 16, 2003"; Includes bibliographical references (p. 104-112)
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74. [Image] The necessity for irrigation
An article espousing the efficiency and benefits of irrigation in agriculture. Includes photos of "Waiting for water: scene on the Truckee-Carson Project" and "Irrigation in southern California"Citation Citation
- Title:
- The necessity for irrigation
- Author:
- Pardee, George C.
- Year:
- 1906, 2005, 2004
An article espousing the efficiency and benefits of irrigation in agriculture. Includes photos of "Waiting for water: scene on the Truckee-Carson Project" and "Irrigation in southern California"
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75. [Image] Klamath Falls Resource Area resource management plan and environmental impact statement : final : Volume 2
Proposed resource management plan/final environmental impact statement for the Klamath Falls Resource AreaCitation Citation
- Title:
- Klamath Falls Resource Area resource management plan and environmental impact statement : final : Volume 2
- Author:
- United States. Bureau of Land Management. Klamath Falls Resource Area Office
- Year:
- 1994, 2005, 2004
Proposed resource management plan/final environmental impact statement for the Klamath Falls Resource Area
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76. [Image] The Oregon conservation strategy
v, 419 p.; col.ill.; col.maps; "February 2006"; Foreword by Marla Rae, Chair, Oregon Fish and Wildlife CommissionCitation -
The purpose of this summary report is to provide an overview of the findings developed for the Lower Snake River Juvenile Salmon Migration Feasibility Study. For more detailed information, the reader should ...
Citation Citation
- Title:
- Improving salmon passage: draft, the Lower Snake River juvenile salmon migration feasibility report/environmental impact statement
- Year:
- 1999, 2004
The purpose of this summary report is to provide an overview of the findings developed for the Lower Snake River Juvenile Salmon Migration Feasibility Study. For more detailed information, the reader should refer to the Draft Feasibility Report/Environmental Impact Statement and attached appendices. The genesis of this study is the National Marine Fisheries Service's 1995 Biological Opinion for the Reinitiation of Consultation on 1994-1998 Operation of the Federal Columbia River Power System and Juvenile Transportation Program in 1995 and Future Years (95 Biological Opinion). While the focus of this study is the relationship between the four dams on the lower Snake River and their effects on juvenile fish traveling toward the ocean, the implications of the study are broader. The Draft Feasibility Report/Environmental Impact Statement includes the best available information on the biological effectiveness, engineering, economic effects, and other environmental effects associated with the four specific alternatives. It does not, however, include a recommendation or identify a preferred alternative. This will give the public and other agencies an opportunity to review and understand this information and provide input before a preferred alternative is selected. At the same time, this will allow the region to consider the Habitat, Hatcheries, Harvest, and Hydropower Working Paper on salmon recovery by the Federal Caucus. Information from this process will be fully examined to determine how it may influence decisions on actions for the lower Snake River.
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78. [Image] Biological opinion Klamath Project operations
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Puga and Chumathang Geothermal fields are situated near the collided junction of the Indian and Asian Crystal plates and thermal activity in these fields is attributed to the widespread igneous activity ...
Citation Citation
- Title:
- Geothermal Exploration of the Puga and Chumathang Geothermal Fields, Ladakh, India
- Author:
- Shanker, R.
Puga and Chumathang Geothermal fields are situated near the collided junction of the Indian and Asian Crystal plates and thermal activity in these fields is attributed to the widespread igneous activity of Upper Cretaceous to late Tertiary age. A deep suture zone, recognised in between these two fields and the associated faults provide channels for the upward migration of the thermal fluids. High concentrations of Cl, F, Si02, B, Na, Li, Rb, Cs in thermal fluids signify contribution of magmatic bodies towards heat, and fluid supply. These fields are characterized by high heat flow conditions (13 HFU), abnormal shallow geothermal gradients (0.7 - 2.5 c/m) , high base temperature (220 - 270 C) as obtained by alkalia and Ne-K-Ca geothermometry and low resistivity values (2-20 ohm.m.). Low resistivity zones occupy on an area of three and one sq.km. and extend down to maximum depths of 300 m. and 130 m. at Puga and Chumathang respectively. Shallow drilling (28-130 m.) has established the existence of wet steam reservoirs under moderate pressure (2-4.5 kg/cm^2). Hot fluid (95-135 C) discharges from eight flowing wells ranged from 7.5 to 30 t/h. These thermal fluids are stored in the partly consolidated fluvioglacial deposits of Quarternary to Recent age. The occurrence of a limestone layer in the country rock at Puga brightens the prospects of getting good reservoir at depth. In both these fields two aquifers have been recognised, each having sizeable potential for retaining ground water. The ground water recharge is mainly through snow melt from glaciers in the case of Puga field and principally from Indus river in the case of Chumathangfield
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"May 2000"; From cover: Prepared for U.S. Department of Agriculture/Natural Resources Conservation Service, 2316 South 6th Street, Suite C, Klamath Falls, Oregon 97601. In Partnership with The Nature Conservancy, ...
Citation Citation
- Title:
- Williamson River delta restoration project : environmental assessment
- Year:
- 2000, 2005
"May 2000"; From cover: Prepared for U.S. Department of Agriculture/Natural Resources Conservation Service, 2316 South 6th Street, Suite C, Klamath Falls, Oregon 97601. In Partnership with The Nature Conservancy, 821 SE 14th Avenue, Portland, Oregon 97214 and US Fish and Wildlife Service, US Bureau of Reclamation, Klamath Tribes, PacifiCorp, Cell Tech International; Includes bibliographic references (p. 60-66)
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81. [Image] Gerber-Willow Valley Watershed Analysis
x, 386 p., ill., maps (some col.); Cover title; "July 2003"Citation Citation
- Title:
- Gerber-Willow Valley Watershed Analysis
- Author:
- U.S. Department of the Interior. Bureau of Land Management; Klamath Falls Resource Area Office; U.S. Department of Agriculture. Forest Service; Fremont-Winema National Forests; Modoc National Forest
- Year:
- 2003, 2006, 2005
x, 386 p., ill., maps (some col.); Cover title; "July 2003"
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The Klamath Project at 100: Conserving our Resources, Preserving our Heritage 1905- 2005: The First Century of Water for the Klamath Project Grain Truck, Lower Klamath Lake, 2004 Prepared by Dan Keppen, ...
Citation Citation
- Title:
- The Klamath Project at 100 : conserving our resources, preserving our heritage
- Author:
- Keppen, Dan
- Year:
- 2004, 2005
The Klamath Project at 100: Conserving our Resources, Preserving our Heritage 1905- 2005: The First Century of Water for the Klamath Project Grain Truck, Lower Klamath Lake, 2004 Prepared by Dan Keppen, Executive Director Klamath Water Users Association December 2004 1 1 1 1 1 ) 1 1 ) 1 1 1 I 1 I I I 003E00042195 .... rrj R13E ^ ^ T ^ I l* IILLER DIVERSION DAM MILLER CREEK AND LOST RIVER CHANNEL L. ^ ^ IMPROVEMENTS — FEATURES: Hydrography Canal Drain Dike ) ( Tunnel )—( Flume ) - - ( Siphon Pipeline Drop 9 Pumping Plant Q Irrigation District Pumping Plant H Private Utility Powerplant ik Project Headquarters Project Land Lea3 « Area MAJOR WATER DISTRICTS: Ady Dist. Improv. Co. Enterprise I. D. Horsefly I. D. Klamath Drain. Dist. Klamath I. D. Langell Valley I. D. Malin ID. Midland Dist. Improv. Co. P Canal Mutual Water Co. Pine Grove I. D. Pioneer Dist. Improv. Co. Plevna Dist. Improv. Co. Poe Valley Improv. Dist. Shasta View I. D. Sunnyside I. D. Tulelake I. D. Van Brimmer Ditch Co. Westside Improv. Dist. KLAMATH PROJECT Oregon - California N 0 12 3 4 5 Miles Background of Klamath Water Users Association The original Klamath Water Users Association was organized on March 4, 1905 under Oregon statute and capitalized in the amount of $ 2,000,000. That Association was created by local farmers, livestock producers, businessmen, bankers, attorneys, and community leaders interested in seeing the Klamath Reclamation Project constructed with the least amount of cost and for the lasting benefit of the entire Klamath community. Working in cooperation with Reclamation the stockholders of the Association contracted with the U. S. Secretary of the Interior to assume the responsibility of payment to the United States the cost of the Klamath Project irrigation works on November 3, 1905. The Association was active in bringing in lands to be served by the Project and addressing water right matters of those lands. By the 1950' s much of the construction costs of the project had been reimbursed to the United States, and irrigation districts assumed the contractual obligations for maintaining and operating the Project. The current Klamath Water Users Association ( KWUA) has its origins in the Klamath Water Users Protective Association, bylaws adopted June 22, 1953, organized to address water right and electrical power issues for Klamath Basin irrigators. The Protective Association reformed itself March 16,1993 with amended bylaws, and incorporated in 1994 as the modern Klamath Water Users Association. The KWUA represents private rural and suburban irrigation districts and ditch companies within the Klamath Project, along with private irrigation interests outside the Project in both Oregon and California in the Upper Klamath Basin. The KWUA is governed by an eleven-person board of directors elected from supporting irrigation districts, private irrigation interests, and the business community. The KWUA now represents over 5,000 water users on 1,400 family farms. Klamath Association KWUA's mission statement: To preserve, protect and defend the water and power rights of the landowners of the Klamath Basin while promoting wise management of ecosystem resources. r Table of Contents Page Executive Summary 4 Introduction 5 Overview 7 Pioneers 9 The Reclamation Act 10 The Klamath Basin Calls in the United States Government 10 Construction Begins 11 Homesteaders 13 The Klamath River Compact 15 The Klamath Project's Finishing Touches 18 New Demands 19 r Sucker Listings 20 Coho Salmon Listing 21 Problems on the East Side 22 2001 Curtailment 24 The Farmers Fight Back 26 Enter President Bush 27 Vindication: The National Research Council Steps In 28 The Assault on the Klamath Project Intensifies 29 Vindication, Part II 32 " We hate to say we told you so, but...." 33 The Klamath Project Regulatory Regime: 3 Years After the Curtailment. 34 Proactive Efforts of Upper Basin Landowners 36 Sucker Recovery Planning 36 On- the- Ground Actions 36 Environmental Water Bank 38 EQIP Funding in Klamath Basin 39 Recognition at Last 39 50 Years After the Compact - Back to the Watershed- Wide Approach 40 BOR Study on Pre- Project Flow Conditions on Upper Klamath River 40 Conclusion - The Future 41 Notes 44 Photo Credits 47 " " Executive Summary r The Klamath Project in 2005 marks its 100- year anniversary. This report summarizes the original formation of the Project, describes the enthusiastic response of the local community to the federal water project, and steps through the development of the Project in ensuing decades. The story of the pioneers, early settlers, and homesteaders who helped settle the area - veterans of both world wars - provides a sense of the character possessed by local farmers and ranchers, who had to rely on similar traits to keep their community alive when irrigation supplies were curtailed in 2001. And it explains a very important dynamic of the region, especially in recent years, where local water users are attempting to proactively address water supply challenges while at the same time trying to stave off a furious round of attacks launched by environmental activists. The immediate future remains uncertain for Klamath Project irrigators, but their marked propensity for adapting to change will keep local farmers and ranchers in business for another 100 years. In order to deal with the uncertain water situation, and facing higher power costs in 2006, the 21st century Klamath Project irrigator is adapting, by developing new market niches for products, creating innovative approaches to energy use, conserving and marketing water, and developing habitat for fish and wildlife. The same abilities shown by pioneers and veteran homesteaders beginning over a century ago to carve out new communities from the wilderness will now be employed to conserve resources and preserve their remarkable and uniquely American heritage. r A load of produce from the Klamath Fair, October 1907. • - r r The Klamath Project at 100: Conserving our Resources, Preserving our Heritage " We desire to impress upon your mind the fact that 99% of the people in the Klamath Basin are a unit, and are clamoring for the assistance which might be rendered by the Government under the Reclamation Act. " 1905 Petition from Basin residents to the Secretary of the Interior " The vision of the Klamath Basin as a place for human habitation must include agriculture, and an agricultural sector of sufficient size to be economically viable. This place ought to have an urban center and a scattering of pleasant small towns - and in between green fields with dancing water from irrigation works." Klamath Falls Herald & News Editorial June 20, 2004 " Agriculture plays a vital role in this state } s economy. An economic issue is one thing, for the farmers who need the resource, need the water, to be able to make a living. There fs another piece to this that ys much larger for all Oregon, and that is a cultural issue. The people here are very, very important to the future of this state. " Oregon Governor Ted Kulongoski, At the A Canal Fish Screen, Klamath Falls, Oregon. April 17, 2003 Introduction The year 2005 marks the one hundred- year birthday of one of the oldest federal water projects in the western United States - the Klamath Irrigation Project. As was painfully made evident in 2001, when Klamath Project supplies were curtailed for the first time in 95 years, the local community and its economy are interwoven with the health of this irrigation project. One hundred years after overwhelming national policy supported its construction, the Klamath Project continues to play a critical role in the local community. " The Klamath Project started out as a good thing, and it remains a good thing", said Tulelake farmer Rob Crawford. " When the Project was created, Klamath Basin people were meeting a national call by doing what they were supposed to do - settle the West. Today, our efforts focus on preserving our heritage, while conserving our resources." r r - r r rr At the beginning of the last century, when the local community learned that the Klamath Project would be developed, an " incredible celebration" ensued, said Paul Simmons, an attorney for the Klamath Water Users Association. " The people of the Klamath Basin basically posed a proposal to the federal government," said Simmons. " They told the government,' if you will be the plumber and the banker, we can do something good for the country.'" The federal government did just that by constructing the irrigation project. Local growers repaid the construction costs in the ensuing decades. Today, thousands of people - family farmers and ranchers, their employees, and agriculture- related businesses - make their living directly from farming and ranching in the Klamath Project. In turn, their activities support the communities of Malin, Merrill, Midland, Bonanza, Tulelake, Newell, and Klamath Falls. And, equally important, their efforts yield high- quality safe food for the country and the world. The last century has been one of massive transformation, vitality, shining hope, and deep despair for the farmers and ranchers served by the Klamath Project. The core reason for the creation of the Klamath Project - to develop water supplies and storage for irrigation uses - has been diminished as new competing demands, intended to satisfy Endangered Species Act ( ESA) and tribal trust conditions, have come on line. As a result, after perceived ESA and tribal trust obligations are met, Klamath Project irrigators and national wildlife refuges essentially get the remaining water. Because very little carryover storage is provided by Klamath Project reservoirs, the farmers now find themselves becoming increasingly reliant on incoming flows to the reservoirs, rather than the stored water that was originally developed to provide them with a reliable summertime irrigation supply. In essence, because of new laws and policies developed in the recent past, the original purpose of the Klamath Project has been somewhat lost in the shuffle. This became glaringly obvious in 2001, when for the first time in 95 years, water supplies to the Klamath Project from Upper Klamath Lake were curtailed before the irrigation season had even begun, to meet conditions set by federal fishery agencies to purportedly prevent harm to three fish species. Three and one- half years after Klamath Irrigation Project ( Project) water deliveries were terminated by the federal government, local water users are attempting to proactively address water supply challenges while at the same time trying to stave off a furious round of attacks launched by environmental activists. Project irrigators - who farm on lands straddling the California- Oregon state line - remain apprehensive about the future certainty of water n supplies. However, the strong traits shown by the original Klamath Project settlers - self-independence, creativity, a sense of community - are still apparent, one hundred years later. Without these characteristics, the tragic events of 2001 might have become nothing more than n passing headlines in the local newspaper. Instead, a galvanized community grabbed national media and political attention by forcing the rest of the country to see that things had gone too far. r r Now, Klamath Project irrigators are preparing for the next 100 years. In order to deal with the uncertain water situation, and facing higher power costs in 2006, the 21st century Klamath Project irrigator is adapting, by developing new market niches for his products, creating innovative approaches to energy use, conserving and marketing water, developing habitat for fish and wildlife, and improving the symbiotic relationship he has with neighboring national wildlife refuges. The same abilities shown by pioneers and veteran homesteaders to carve out new communities from the wilderness will now be employed to conserve resources and preserve their remarkable and uniquely American heritage. Overview The irrigable lands of the Klamath Project ( Project) are in south- central Oregon ( 62 percent) and north- central California ( 38 percent). Two main sources supply water for the Project: Upper Klamath Lake and the Klamath River on the Klamath system; and Clear Lake Reservoir, Gerber Reservoir, and Lost River on the Lost River system, are in a closed basin. The total drainage area for the Klamath Project, including the Lost River and the Klamath River watershed above Keno, Oregon is approximately 5,700 square miles. Currently, approximately 225,000 acres, many previously submerged, have been transformed into productive farmland. The crops grown within the Klamath Project area consist of grain, hay, pasture, silage, mint, potatoes, onions, other vegetables, alfalfa, strawberry rootstock, and horseradish. This list of crops represents the majority of planted acreage within the Klamath Project over the last 40 to 50 years. The cropping pattern has varied from year to year, but the overall planted acreage has remained consistent. The Bureau of Reclamation operates Clear Lake Dam, Gerber Dam, and the Lost River Diversion Dam. The Link River Dam is operated by the Pacific Power and Light Company in accordance with Project needs, or more recently also as directed by federal agencies. The Tulelake Irrigation District operates the Anderson- Rose Dam, and the Langell Valley Irrigation District operates the Malone and Miller Diversion Dams. The various irrigation districts operate the canals and pumping plants. The original Klamath Project plan included construction of facilities to divert and distribute water for irrigation of basin lands, including reclamation of Tule and Lower Klamath Lakes, and control of floods in the area. The development of the stored water provided by the Klamath Project allowed for the controlled, beneficial use of water in the Upper Basin. Currently, late summer and fall flows in the Lower Klamath River are augmented with stored water that would not be there, but for the Project. Under pre- Project conditions, natural controls existed below both Upper Klamath Lake and Lake Ewauna which stabilized lake levels except during critical droughts. Those controls were natural reefs of hard earth material in the channel and other channel constrictions. Under these pre- Project conditions, the Klamath River flowed into the Lower Klamath Lake area. A 1906 map titled " Topographic and Drainage Map, Upper and Lower Klamath Project" shows the invert of the Klamath Strait approximately the same level as the Klamath River channel bottom near Keno. In addition, the Lost River terminated at Tule Lake. These flows flooded approximately 183,000 acres within Lower Klamath and Tule Lake. In general, under pre- Project conditions, Klamath River flows downstream of Keno likely occurred after a certain water level was reached in the Klamath River and Lower Klamath Lake. An engineer speaking in the early days of the Project observed that adequate Klamath Project water supplies were not a worry. Rather - something that would be inconceivable today - dealing with too much water was more of a concern at the time: " It contains an irrigation problem, an evaporation problem, a run- off problem, any one of which is difficult in itself but all of which together form a most perplexing whole," said the engineer. " In nearly all reclamation projects water has to be conserved. In this project there is more than enough and the question of disposing of it becomes an important part." 1906 Map of Pre- Project Area r • r r r Pioneers Irrigation development began in areas now served by the Klamath Project in the latter half of the nineteenth century. Various landowners and entrepreneurs utilized water of the Klamath River and its tributaries, and undertook a wide range of visionary activities. Prime farmland, exposed around the edges of old historic Tule Lake as early as 1846 stimulated early settlers' interest in irrigation. Similarly, early settlers beginning in the early 1860s relied on " naturally irrigated" greases and forage in the Lower Klamath area for pasture and hay. The first irrigation ditch was dug by George Nurse and Joseph Conger in the bottom of Linkville Canyon in 1868. In 1878, this ditch was expanded and incorporated into the Linkville Water Ditch Company. Early pioneers Steele and Ankeny pursued a canal to deliver water to land between Klamath Falls and Merrill. Ultimately, the canal system was replaced by the A Canal and its distribution system which, operated by Klamath Irrigation District, continues to serve Project land to this day. t Adams Cut, July 18,1906. Diversion for irrigation of additional agricultural lands in the area now comprising the Klamath Project was initiated in 1882 with construction of an irrigation ditch by the Van Brimmer brothers to the land from White Lake, which was fed by the Klamath River. Private interests further developed this project by constructing the Adams Canal in 1886, which was supplied also from White Lake. Frank Adams, with assistance from the Van Brimmer r rr rr r Brothers, cut a canal through tule roots using hay- knives and a derrick, in order to improve diversion from White Lake. This canal ultimately extended to a length of 22 miles. By 1903, approximately 13,000 acres were irrigated by private interests, with the canal system in progress to deliver much more. After the 1905 authorization of the Klamath Project ( see below), many water rights were acquired to facilitate, and for the benefit of, the Klamath Project enterprise, and other agreements were made with other water right- holders. The Project utilized, extended, expanded and/ or improved previously existing systems, and included construction of other facilities. The Reclamation Act In 1902 Congress enacted the Reclamation Act, which encouraged the settlement of lands in the western states and the development of agricultural economies to feed the nation. The 1902 Act provided for federal financing of irrigation works, with the construction costs to be repaid over time by project water users. In addition, public lands were made available for homesteaders who accepted the responsibility to undertake improvements and pay the water charges. Both the Oregon and California legislatures also enacted laws making state- owned land available for use in the Klamath Project. The Klamath Basin Calls in the United States Government In 1903, the Reclamation Service conducted investigations that led in 1904 to the first withdrawal of land by the Secretary of the Interior for developing a federal irrigation project. J. B. Lippincott, a supervising engineer from Los Angeles - who also played a key role in the City of Los Angeles' securement of Owens Valley water supplies - personally toured the Klamath Basin in June of 1904. l Although private irrigation projects were moving forward by the turn of the century, and some large- scale projects were being planned, most local citizens saw great value in a federally authorized and supported project. In 1905, local residents sent numerous petitions to Washington, D. C. requesting government irrigation assistance. By this time, a private corporation had given notion of its plans to develop water for what would ultimately become virtually the entire Klamath Project. Ironically, after Owens Valley agricultural water rights were secured by the City of Los Angeles, many of the displaced farmers moved to the Klamath Basin for the " reliable" water supplies of the Klamath Project. On their way north, they passed the first Reclamation Project in the West - the Newlands Project, near Reno, Nevada. 10 r r r r r r r " We desire to impress upon your mind the fact that 99% of the people in the Klamath Basin are a unit, and are clamoring for the assistance which might be rendered by the Government under the Reclamation Act," stated one petitioner. In November 1904, F. H. Newell, Chief Engineer of the federal Reclamation Service, told a large audience of enthusiastic farmers in Klamath Falls that, in his judgment, they had " a great irrigation project". Early in 1905, California and Oregon had ceded certain rights in the Upper and Lower Klamath Lakes and Tule Lake to the United States. On May 1, 1904, a board of engineers made a report that served as the basis for authorization of the Project. Congress authorized the use of lands and water in accordance with the State Acts of February 1905. The Secretary of the Interior authorized development of the Project on May 15, 1905, under provisions of the Reclamation Act of 1902. Construction Begins The Interior Secretary's 1905 authorization provided for project works to drain and reclaim lake bed lands of the Lower Klamath and Tule Lakes, to store waters of the Klamath and Lost Rivers, to divert irrigation supplies, and to control flooding of the reclaimed lands. The states of Oregon and California ceded then- submerged land to the federal government for the specific purpose of having the land drained and reclaimed for irrigation use by homesteaders. The Oregon Legislature also authorized the raising and lowering of Upper Klamath Lake in connection with the Project, and allowed the use of the bed of Upper Klamath Lake for storage of water for irrigation. Construction began on the Project in 1906 with the building of the main " A" Canal. Water was first made available May 22, 1907, to the lands now known as the Main Division. 1907 Completion of the A Canal Headgates 11 r r r r r This initial construction was followed by the completion of Clear Lake Dam in 1910, the Lost River Diversion Dam and many of the distribution structures in 1912, and the Lower Lost River Diversion Dam in 1921. ( In 1970, a public dedication at the Lower Lost River Diversion Dam officially changed the name of the structure to Anderson- Rose Dam.) Constructing Clear Lake Dam, September 1909. Large stone in self- dumping car. A contract executed February 24, 1917, between the California- Oregon Power Company ( now the Pacific Power and Light Company) and the United States authorized the company to construct Link River Dam for the benefit of the Project and for the company's use, and also extended to the water users of the Klamath Project certain preferential power rates. The dam was completed in 1921. The contract was amended and further extended for a 50- year period on April 16, 1956. The Malone Diversion Dam on the Lost River was built in 1923 to divert water to Langell Valley. The Gerber Dam on Miller Creek was completed in 1925, and the Miller Diversion Dam was built in 1924 to divert water released from Gerber Dam. In the Great Depression, continued settlement and leasing and distribution construction resulted in a significant increase, between 1930 and 1939 of the acres receiving water directly from Project facilities. The project work undertaken during this period included the enlargement of the Lost River Diversion Channel. In 1940, construction was begun on Pumping Plant D and the Tule Lake Tunnel. By 1942, these facilities, as well as the P- Canal were completed. In 1943, the Ady pumping plant was placed in operation, and in the next two years, the Straits Drain and pumps were constructed and installed and began operation. 12 r r Homesteaders The story of the homesteaders is a source of great pride in the Klamath Project. As Tule Lake receded according to plan, the lake bottom became suitable for cultivation. The land that ultimately became homesteads was under jurisdiction of the U. S. Bureau of Reclamation ( Reclamation). Homesteading and developing more productive agricultural land was the goal of the reclamation project that " reclaimed" the beds of Tule Lake and Lower Klamath Lake to expose more arable land. After Tule Lake was dewatered, a large area of public land became available for agriculture. The government would lease this land to settlers, and in fact leased as much as 50,000 acres in Tule Lake in the 1920s. Over time, most of this land was homesteaded. In 1917,180 people applied for the 37 homestead parcels the Reclamation made available on the drained wetlands and lake beds. Between 1922 and 1937 there were five more homestead offerings and hundreds of homesteaders settled in on the fertile soil of the drained lake bed. Then, World War II curtailed the homesteading process. » rri.. . r i* Ul. r- Xio. 1 wi sat Mi M MM ttw DCCA rru. ilon _ ji « _ jra .... r. r tk. M r « i t » a-. . « *^ J •* 4. MM r* T RTMtNT Or THE X ,. . tie*. . ..< L. » ii tatwJ l u i » T « 11 r ( » T « rnr » ) xfc. ir « « . •" « » ^> « • inS| « Ut !•• « . • TTDHOII. ,.> , ^% laMitk r » u. « . orumtm. _ JBKS!*! « r._: iit_ » « « » i.. bwrlac n i M la t&. MttaJOMI ( 1* nat.. J « a>. aa4 tk* a. t* JKLaUMftULJatiLJlJrt.. . . . . W l t a . is a- S.- ..- M « ri « ia*. t u . ar tka ar. ra* al « » ot af i t kav* a » « . > n » M < aatrr. • M M MMtMl. MMM t . aa n » tn4 » r ua « « . o. rol - • M it. » • « i WMM .. 1927 Homesteader Affidavit In three drawings held in 1946, 1948 and 1949, a total of 216 World War II veterans were awarded homesteads on farmland in the Tule Lake Basin, as a thank you from a grateful nation. The number of applicants was far greater than the number of available homesteads. Veterans and the community gathered to watch the names drawn from a pickle jar. Farm homesteads and crop- producing land were the goals of reclamation, and the Tule Lake Basin became a showcase for reclamation work. 13 " When I arrived to see my homestead there was nothing there, just an expanse of opportunity," recalls Carman. " No roads, no houses, no trees, just bare ground. I then pitched my tent in the corner of my homestead." My wife Eleanor was expecting our second child, but could not join me until later. A tent was not acceptable living quarters for a young woman, a small child and another baby on the way." The settlers formed organizations, elected a school board, and went about creating a society. " When I began my new life as a Tulelake homesteader there were approximately 300 homesteaders, most of them with families," said Carman. " We united and began to build schools, churches and a hospital in Klamath Falls. We started a community. We were living the American dream and our dream was achieved by hard work and dedication, and I must say we could never have done this without our wives." Homesteaders: Robinsons in 2001 Remember Days Gone By r - The Klamath River Compact The Klamath River Compact ( Compact) is a law of both Oregon and California, consented to by and Act of Congress. In the following decade, a variety of concerns and issues led to the passage of the Compact in 1957. These included: • Differing positions regarding the extent of development that could occur under Klamath Project water rights; 15 • • The related issue of priority of Klamath Project and overall Upper Klamath Basin irrigation development as against other uses, especially generation of hydro- electric power on the mainstem Klamath River; and • Concerns over potential future out- of- basin water exports. The development of the Compact was closely tied to an application for a water right filed by the California Oregon Power Company ( Copco) in 1951. This application anticipated using water at a proposed hydroelectric project on the Klamath River known as " Big Bend No. 2." In turn, this dispute folded in past dealings, agreements and opinions related to the operation of Link River Dam on Upper Klamath Lake. The agreements made between Copco and the Bureau of Reclamation at the time of construction of Link River Dam around 1920 had been controversial. Upper Klamath Basin irrigation interests had three primary concerns: 1. Power development, as an incident of the Project's reclamation purpose, should be undertaken only by the United States; 2. That the agreements threatened Klamath Project water supplies; and 3. The agreements were inconsistent with state legislation authorizing use of Upper Klamath Lake by the United States for storage or reclamation purposes. In 1951, Copco filed an application with the Oregon Hydroelectric Commission ( OHC) for a water right for the proposed Big Bend No. 2 hydroelectric facility. The OHC at that time had authority and jurisdiction over issuance of water rights for hydropower facilities. Copco at the time of filing took the position that water was available for appropriation and Copco was entitled to a right, senior in priority, to any future Upper Klamath Basin irrigation that was not then actually developed. J. C. Boyle Dam on the Klamath River. — 16 r r • A. To facilitate and promote the orderly, integrated and comprehensive development, use, conservation and control thereof for various purposes, including, among others: the use of water for domestic purposes; the development of lands by irrigation and other means; the protection and enhancement offish, wildlife, and recreational resources; the use of water for industrial purposes and hydroelectric power production; and the use and control of water for navigation and flood prevention. B. To further intergovernmental cooperation and comity with respect to these resources and programs for their use and development and to remove causes of present and future controversies by providing ( l) for equitable distribution and use of water among the two states and the Federal Government, ( 2) for preferential rights to the use of water after the effective date of this compact for the anticipated ultimate requirements for domestic and irrigation purposes in the Upper Klamath River Basin in Oregon and California, and ( 3) for prescribed relationships between beneficial uses of water as a practicable means of accomplishing such distribution and Copco's application to the OHC, and its parallel application to the Federal Power Commission ( FPC) for a license under the Federal Power Act, were contested and opposed by the Department of the Interior and various agricultural and irrigation interests. The OHC did not act on Copco's application until 1956. The States of California and Oregon appointed commissioners to negotiate an interstate Compact. At the same time, Reclamation and local water users were negotiating a new agreement with Copco for operation of Link River Dam. It appeared that such an agreement might be concluded prior to enactment by the States of a Compact. The draft Copco contract was brought before the Compact negotiating commissioners, who sought to ensure consistency with the Compact being developed. During the course of several meetings of the Compact commissioners, terms were developed which resulted in conditions in the FPC license, the water right certificate, and a new contract for Copco's operating of Link River Dam. After preparation of various drafts, negotiation of the Compact was concluded and the legislatures of Oregon, California, as well as the United States Congress, acted in 1957. The major purposes of this compact are, with respect to the water resources of the Klamath River Basin: The Compact recognized water rights for then- existing and future needs in the Klamath Project service area. It also established a system of priority for new water rights under which Upper Basin irrigation ( up to a specified number of acres) had superior rights over water for power generation, fish or wildlife, or recreation. 17 r r r r r In short, the Klamath Compact provided guidelines to lead the competing interests of the Klamath River watershed towards a more harmonious future. For the next 40 years, the intent of the Compact was essentially fulfilled, until the early 1990s, when new pressures to address endangered fish and tribal trust demands resulted in the reemergence of fractionalized conflict into the Upper Basin. Although it had been seen as a resolution for future disputes, the Compact has been interpreted not to override the Endangered Species Act or tribal trust water rights. The Klamath Project's Finishing Touches r Through the 1950s, Reclamation envisioned continued development of the Project that would have doubled its current size by including Butte Valley, California and other areas. The plans were not implemented and the Project acreage has not significantly increased since the end of the 1940s. In the following decades, the delivery system has been improved, bottlenecks eliminated, and relatively small areas have both been brought under irrigation and converted to commercial or residential development. By 1960, due in part to improvements made on Tule Lake dikes, the M Canal, the Lost River Diversion Channel, and installation of new canals in the southern portion of the Tulelake Irrigation District ( TID) service area and the Miller Hill Pumping Plant, the Project provided irrigation service to nearly 216,000 acres. Tulelake, California In the 1960' s, improvements and expansion of certain facilities led to the formation of Klamath Basin Improvement District. The Stukel and Poe Valley Pumping Plants were constructed and the Miller Hill Pumping Plant enlarged. The D, F and G- Canals were also 18 r enlarged. These facilities provided more reliable service to certain lands and also added land to the area that could receive water from Project works. In the 1970' s, Shasta View Irrigation District and Reclamation entered a $ 3.2 million contract for installation of a pressure irrigation system to replace the previous gravity- fed system. The 1972 Project history reported, ".. . the Project provided irrigation and drainage service to 223,661 acres," while the total harvested acreage "... was 193,160, down 2,329 acres from 1971." Also in the 1970' s, the Straits Drain was enlarged. Because of the Klamath Project's design and the interrelated nature of water use within it, including the use of return flows by farmers and the refuge, Project efficiency is very high. A recent assessment of Klamath Project water use efficiency2 implies that a sophisticated seasonal pattern of water use has evolved in the Klamath Project. One must understand that the Klamath Project has developed into a highly effective, highly interconnected form of water management. According to the 1998 Davids study ( see footnote), effective efficiency for the overall Project is 93 percent, making the Klamath Project one of the most efficient in the country3. New Demands For eighty years, Klamath Project irrigation supplies proved sufficient to meet the needs of the area's burgeoning farming and ranching communities. Although there were years where Mother Nature and Klamath Project storage capacity proved insufficient to meet full irrigation demands, the local community managed to stretch thin supplies and make things work. That all changed in the early 1990s, when steadily more restrictive government agency decisions made to meet Endangered Species Act ( ESA) goals began to steadily chip away at the stored water supply originally developed for irrigation. Two sucker species were listed ( 1988) as endangered and coho salmon were listed ( 1997) as threatened under the ESA. Since then, biological opinions rendered by the U. S. Fish and Wildlife Service ( for the suckers) and NOAA Fisheries ( for the coho), have increasingly emphasized the reallocation of Project water as the sole means of avoiding jeopardizing these fish. Klamath Project " operations plans" based on these biological opinions also factor in tribal trust obligations, although the nature and extent of such obligations is undefined. 2 " Klamath Project Historical Water Use Analysis", Davids Engineering for U. S. Bureau of Reclamation, October 1998. 3 For example, Tulelake Irrigation District irrigates 62,000 acres of farmland. In the 1990s, the district diverted an average of 131,000 acre- feet of water. Each year, an average of 80,000 acre- feet was pumped out of the district. Consumptive use within the district is considerably less than the amount of water diverted. The reason is the difference from the return flow from other districts and the reuse of water within the Project. 19 r Sucker Listings In the past twelve years, political and regulatory demands have affected activities at the Klamath Project. In 1988, the short nose sucker and the Lost River sucker, two species that live in Upper Klamath Lake, were designated as endangered under the ESA. Biological opinions issued by the U. S. Fish and Wildlife Service ( USFWS) in 1992 and 1994 concerning operation of the Klamath Project identified actions to avoid jeopardy to suckers. When the suckers were listed, there had been no mention whatsoever of reservoir elevations as a factor affecting sucker populations. These operation elevations were adopted by Reclamation. The reservoir elevations pertaining to Upper Klamath Lake generally allowed the Project to operate for its intended purposes. However, the United States District Court of Oregon found that the reservoir elevations pertaining to Clear Lake and Gerber Reservoirs to be arbitrary and capricious, and they were invalidated in a succession of decisions4. The most compelling and prominent reason why the federal government justified listing the two sucker species as " endangered" in 1988 was an apparent abrupt downturn in both populations during the mid- 1980s. To support the decision to list the suckers, the USFWS believed the only significant remaining populations were in Upper Klamath Lake. We now know that the assumptions by the USFWS were in error and the assumed sucker population crisis never materialized. In fact, shortly after listing of the species, the populations demonstrated dramatic increases5. r Just prior to the listing of the suckers in 1988, a sport snag fishery was allowed. Before 1969, the fishery was largely unregulated with no harvest limit; in 1969 a generous bag limit of 10 fish per angler was imposed. During the early to mid- 1980s, despite the belief that the numbers offish were in a state of rapid decline, the State of Oregon still allowed the sport snag fishery. Ultimately, because of increased focus on the status of the sucker populations, Oregon eliminated the fishery in 1987. Some fisheries experts believe that if the USFWS would have properly assessed the known impacts on the suckers caused by the snag fishery and the benefits from ceasing the fishery, it very likely could have affected the ultimate listing decision. " Simply stated, the largely unregulated snag fishery slaughtered the sucker populations," said Dave Vogel, with Natural Resource Scientists, Inc. " Since the fishery was eliminated in 1987, the two sucker populations dramatically rebounded. The threat was removed and the populations increased ten- fold." 4 Bennett v Spear, 520 U. S. 154 ( 1997); 5 F. Jupp. 2d 887 ( D. Or. 1998); Bennett v. Badgely, No. 93- 6075- HO ( April 13, 1999, June 11, 1999). 5 Vogel, David, 2004. Testimony Before the Committee on Resources ( Subcommittee on Water and Power), United States House of Representatives. Oversight Field Hearing on The Endangered Species Act 30 Years Later: The Klamath Project. 20 At the time of the listings in 1988, the Klamath Project was not identified as having known adverse affects on the sucker populations, yet four years after the listing, using limited or no empirical data, the USFWS turned to the Klamath Project as their singular focus. Paradoxically, since the early 1990s, despite new beneficial empirical evidence on the improving status of the species and lack of relationship with Klamath Project operations, the USFWS became ever more centered on Project operations and increased restrictions on irrigators instead of paying attention to more obvious, fundamental problems for the species. This circumstance caused tremendous expense in dollars and time by diverting resources away from other known factors affecting the species. Coho Salmon Listing r A similar circumstance occurred with NOAA Fisheries during and after the coho salmon listing in the lower basin in the late 1990s. It cited the reasons to list coho salmon, excluding Klamath Project operations as a significant factor affecting the species. There are many other documented factors that have affected salmon runs in the Klamath River6. The USFWS in the 1980s described the most important eight factors as " most frequently referred to with regard to recent population declines" of anadromous fish in the Klamath River. Those factors are: " • Over fishing • Logging • Trinity River transbasin diversion Irrigation diversions in lower Klamath tributaries • 1964 flood • 1976- 1977 drought • Sea lion predation • Brown trout predation. However, shortly following the listing, and with no supporting data, NOAA Fisheries chose to center its attention on the Klamath Project as the principal factor affecting coho salmon. In its biological opinions, NOAA Fisheries opined that much higher than historic flow levels, released from the stored water of the Klamath Project, would be needed to protect coho salmon downstream of Iron Gate Dam. Iron Gate Dam is located forty miles away and coho are generally found further downstream and in tributaries. 7 In essence, both agencies adopted a single- minded approach of focusing on Klamath Project operations to artificially create high reservoir levels and high reservoir releases. This puzzling, similar sequence of events has yet to be explained by agency officials. 6 KWUA biologists compiled a comprehensive listing of those factors in March 1997. 7 Vogel, David, 2004. Testimony Before the Committee on Resources ( Subcommittee on Water and Power), United States House of Representatives. Oversight Field Hearing on The Endangered Species Act 30 Years Later: The Klamath Project. 21 r " ~ Commercial harvests of salmon intensified with the development of canning technology. By the early 20th century, habitat destruction combined with commercial harvests had resulted in serious salmon depletion on the Klamath River. Cobb ( 1930) estimated that the peak of the Klamath River salmon runs occurred in 1912, Snyder ( 1931) observed " in 1912 three [ canneries] operated on or near the estuary and the river was heavily fished, no limit being placed on the activities of anyone". Problems on the East Side Irrigation districts on the east side of the Klamath Project felt the first impacts from increased regulatory focus on lake levels in the early 1990s. Langell Valley Irrigation District ( LVID) and Horsefly Irrigation District ( HID) receive water from Clear Lake and Gerber reservoirs. Historically, stored water was released from these two reservoirs beginning about April 15 and ending about October 15 each year. These reservoirs are not large, but they provide the essential water supply to an otherwise arid area. In an average year, Clear Lake releases about 36,000 acre- feet of irrigation water, and Gerber releases about 40,000 acre- feet. Clear Lake Reservoir contains populations of both endangered sucker species, and Gerber reservoir hosts one of the species. ESA-" threatened" bald eagles are also known to inhabit the Klamath Project area. In 1991, at the request of the USFWS, Reclamation initiated ESA consultation to assess the impact of the long- term operation of the Klamath Project on the suckers and the bald eagle. In the next year, three biological opinions were rendered by USFWS that imposed minimum levels in Clear Lake to purportedly protect the sucker populations. As a result of the minimum lake levels imposed by the draft biological opinions, and the water lost to evaporation before the USFWS allowed any water releases, the Districts were not able to make their normal irrigation releases during the 1992 water year. Neither district received its first seasonal water delivery until May 15, 1992, a full four weeks later than normal. By 22 r " that date, 12,000 acre- feet of the water that had been stored in Clear Lake in March 1992 had evaporated, an amount that represents about 60% of LVID's total yearly withdrawal from Clear Lake Reservoir. As a result of the minimum lake levels and the evaporation losses, only 2,148 acres of the 16,800 irrigable acres within the LVID received any Klamath Project water at all. The lack of water reduced both acreage farmed and per- acre yields that year. As a result of reduced yields, farm properties lost up to 70% of their assessed values in 1992. The lack of water also hurt the region's cattle ranching operations, because some ranchers could not produce pasture for their cattle. Water users who could afford the extra expense purchased feed to sustain their herds. Others had to cut back substantially on their herds or sell their cattle. Wildlife also suffered as a result of the decision to impose minimum surface levels in the reservoirs. Because the Lost River obtains most of its water from releases from Clear Lake Dam and return flows from agricultural operations, the water levels in the Lost River and its tributaries were exceedingly low in 1992. As a direct result, wildlife relying on Lost River water, including deer, sandhill cranes, hawks, turtles, frogs, ducks, and more, were all noticeably scarce that year. On July 22, 1992, USFWS finally issued its final biological opinion on the long- term operations of the Klamath Project. While the 1992 opinion conceded that " little" was known about Gerber Reservoir's shortnose sucker population, the opinion reported " good numbers" of these fish and noted that the Gerber sucker population appeared to be successfully reproducing, despite the lowered lake levels of the early 1990s. Despite this undisputed evidence, the 1992 biological opinion concluded that continuing to operate the Project, including Clear Lake and Gerber reservoirs, in its historic manner was likely to jeopardize the continued existence of both sucker fish species. Reclamation accepted the USFWS recommendations for continued adherence to minimum lake levels, prompting the Districts and two of the individual farmers to sue the federal agencies. Even after the federal district court entered judgment invalidating the jeopardy conclusions, USFWS defied this judgment, and the districts were forced to bring several additional motions to enforce the Court's rulings. At each stage of the legal proceedings, the districts prevailed, based largely on the fact that USFWS had no scientific evidence to justify its actions. When the United States Supreme Court considered the Districts' case against the USFWS, the Court described the purpose of the ESA's science requirement as follows: The obvious purpose of the requirement that each agency " use the best available scientific and commercial data available" is to ensure that the ESA not be implemented haphazardly, on the basis of speculation or surmise. While this no doubt serves to advance the ESA's overall goal -., of species preservation, we think it readily apparent that another objective ( if not indeed the 23 primary one) is to avoid needless economic dislocation produced by agency officials zealously but unintelligently pursuing their environmental objectives. Now, ten years later, HID and LVID enjoy positive relationships with USFWS and Reclamation. However, the problems they suffered in the early 1990s were a harbinger of things to come for other Klamath Project irrigators shortly after the turn of the new century. 2001 Curtailment The net result of increasing restrictions on other Klamath Project water users was fully realized on April 6, 2001, when Reclamation announced its water allocation for the Project after U. S. Fish and Wildlife Service and NOAA Fisheries officials finalized the biological opinions ( BOs) for project operations in a critically dry year. Based on those regulatory actions, Reclamation announced that - for the first time in Project's 95- year history - no water would be available from Upper Klamath Lake to supply Project irrigators. No water for most farmers April 6, 2001 Local Headlines The resulting impacts to the local community were immediate and far- reaching. Even with a later release of a small percentage of needed water over a 30- day period in July and August, thousands of acres of valuable farmland were left without water. In addition to harming those property owners, managers, and workers, also imparted an economic " ripple" effect through the broader community. The wildlife benefits provided by those farms - particularly the food provided for area waterfowl - were also lost with the water. 24 Kliewer Family in Dry Fields South of Klamath Falls - 2001 The local farming community is still reeling from the April 6, 2001 decision, and severe business losses echoed the hardship endured by farmers and farm employees. As farmers and laborers attempted to deal with the loss of jobs, a year's income, and in some cases the land itself, referrals for mental health counseling increased dramatically. The Tulelake school district lost around 50 students after farm families sold their land and moved on. Students were under stress, understandably confused as to why three species of fish were more important than their lifelong homes. Tragically, one Hispanic family had started out as field workers, and after a lifetime of piecework under the sun had saved enough to buy their own farm. They lost everything as a direct result of the irrigation cutofi . Veteran homesteaders, who fifty years ago were promised reliable water, felt betrayed by the same government, who chose to provide water to fish instead of farmers in 2001. " I want the government to honor the contract that promised me and my heirs water rights forever," said Jess Prosser, a World War II veteran and Tulelake homesteader, in 2001, after water supplies were cut. " This land is our life. Farmers and fish have survived previous drought years when the farmers voluntarily cut back on water consumption. The Klamath Project was designed to withstand drought conditions, and right now there is more than ample water for agriculture and fish. The government took 100% of the water for fish, disregarding farmers, ranchers, families and numerous other species of wildlife in the Klamath Basin. This is a man- made disaster. This will be the end of a way of life and an entire community." 1 " Calamity in Klamath", Blake Hurst. The American Enterprise magazine. October / November 2002, pp 28- 29. 25 Cemeteries Went Dry in 2001 The Farmers Fight Back The local community did not take the decision lying down. Employing the ingenuity and perseverance that allowed them to successfully create brand new communities over the past century, local farmers, ranchers, elected officials and business leaders organized a " bucket brigade" to dramatize their plight, drawing nearly 20,000 sympathizers to the streets of Klamath Falls. A web site and cell phone calling tree were set up, and farmers, who only a year before were working their fields, suddenly became knowledgeable about the media. Civil disobedience, in the form of peaceful protests at the A Canal headgates, drew television crews from throughout the Pacific Northwest. The 2001 Klamath Basin crisis became the topic of front- page coverage and sympathetic editorials in publications like Time magazine, the Los Angeles Times, the Wall Street Journal, and the New York Times. Time Magazine Captures Rob Crawford & Family, Summer 2001. In part because of the tremendous media and political attention generated by the local community, a congressional field hearing was held in the summer of 2001 at the Klamath County fairgrounds, which drew the largest audience to ever attend such a hearing in the nation's history. Much of the focus was on the decision- making and processes that led to the fishery agencies' recommendation to curtail irrigation supplies. 26 In 2001, a desperate community essentially was looked in the eye and told, " sorry, we know it may hurt, but ' the science' is compelling and requires you to go without water." This was wrong, literally, and as a matter of policy. For whatever reason, the agencies had become too close to, and too much a part of, the side- taking that had come to dominate issues surrounding the Klamath Project. For this reason alone, outside review was needed. Nearly 20,000 marchers support the Klamath Bucket Brigade, May 2001. Prayer / protest at the A Canal headgates, 2001. Elected officials - from county commissioners and supervisors, to state representatives and senators, to U. S. Senators and Representatives, continued the fight, and ultimately, later in 2001, the U. S. Secretary of the Interior, Gale Norton, directed the National Academy of Sciences to conduct an independent peer- review of the agency decision to curtail irrigation supplies. Also, in early 2002, President Bush himself took a personal interest in the plight of the Klamath Project irrigator. Enter President Bush In January 2002, just months after the federal government curtailed Klamath Project irrigation deliveries for the first time in 97 years, Sen. Gordon Smith and Rep. Greg Walden met the president in southern California, boarded Air Force One, and took a slight detour over the Basin on their way to a Portland high school where the Mr. Bush was to deliver a speech. On the flight north, the president was briefed on the 2001 Klamath water crisis. When he entered the gymnasium at Park Rose High School, he opened his speech up with a pledge to help both the farmers and the fish of the Klamath Basin. 27 Compassion: George W. Bush Meets and Greets Klamath Basin Residents in Redmond, Oregon, 2003. In the ensuing two years, President Bush has followed through with his pledge by establishing a Klamath Basin cabinet- level working group, promoting sound and independent peer-reviewed science, and making funding of Klamath River water and environmental projects a priority. Enacted and requested Bush Administration funding in the Klamath River watershed for fiscal years 2003- 2005 exceeds $ 260 million dollars, according to a federal government summary. This includes $ 105 million proposed by the administration for Klamath Basin federal funding in the Fiscal Year 2005 budget. Vindication: The National Research Council Steps In The Klamath Water Users Association and others in the community in 2001 strongly advocated for an independent peer review of the 2001 fishery agency biological opinions, the underlying science, and the related overall scientific process. In early 2002, an interim report from the National Research Council ( NRC) Committee on Endangered and Threatened Fishes in the Klamath Basin was released. This represented a critical step towards ensuring proper assessment and maintenance of healthy fish populations. The panel successfully completed an objective, unbiased initial review of the information used by the U. S. Fish and Wildlife Service ( USFWS) and NOAA Fisheries to formulate the agencies' two 2001 Biological Opinions ( BOs). The interim NRC report concluded that there was insufficient scientific evidence used by USFWS and NOAA Fisheries in 2001 to support changing the recent historical water operations of the Klamath Project. Specifically, the NRC interim report concluded that higher or lower than recent historical lake levels or Klamath 28 rr r rrr r r r River flows were not scientifically justified based on the available information used by the USFWS and NOAA Fisheries. Despite varying interpretations of the data used by the USFWS and NOAA Fisheries in the BOs, it is especially noteworthy that the NRC panel achieved consensus on the Interim Report's conclusions for not just one, but both BOs. The report's conclusions were adequately supported by the available evidence and analyses used by USFWS and NOAA Fisheries. It was particularly evident that the NRC Committee report was fair and impartial, essential attributes that were sorely lacking in Klamath basin issues to date. The Assault on the Klamath Project Intensifies The release of the NRC Committee's interim report in early 2002 unleashed a barrage of criticism from environmental activists and their allies in academia and government agencies. Two Oregon State University professors, supporters of the high lake level requirements that contributed to the 2001 water curtailment, submitted a formal " rebuttal" of the interim report to a fisheries journal. The " rebuttal" ( so labeled when transmitted by its authors) and other media developments caused the Klamath Project community to fear that the NRC work would be diluted. The local community simply did not have the resources or the networks of contacts to continually counter the anti- Klamath Project messages that were being sent to the public and policymakers, primarily by outside environmental activist organizations. The NRC Committee's interim report triggered what grew to be an extraordinary, and obviously coordinated, attack on the Klamath Project by these interests. Media outlets seemingly relish a good western fight, and many uncritically reprinted a good deal of information that was not fair to Klamath Basin irrigators. The scrutiny on the Klamath Project and the Bush Administration's reliance on the NRC interim report intensified further that fall, when 33,000 salmon died on the lower Klamath River. Immediately after the unfortunate die- off, vocal critics of Project operations and Bush Administration environmental policy used the event to renew attacks on irrigated agriculture in the Klamath Basin. Even though the fish die- off occurred 200 miles downstream from the Project, at a location below the confluence of the main stem Klamath River and the Trinity River, traditional advocates for higher river flows quickly assigned blame to Klamath Project farmers and ranchers. Some of these same interests and others in the environmental community even attempted to directly link the fish die- off to alleged political maneuvering orchestrated by senior policy officials in the Bush Administration. As a result, presidential hopeful Senator John Kerry called on the U. S. Interior Department's Inspector General to look into whether " political pressure from the White House is intimidating staff and influencing policy" in Klamath River management decisions. Interior Department Inspector General Earl Devaney's report - released in March 2004- found " no evidence of political influence affecting the decisions pertaining to the water in the Klamath Project." 29 r r r r r r Eugene Register- Guard Why the salmon died: Pattern points to Bush administration policies A Register- Guard Editorial A 2002 Editorial Headline Between 2002- 2004, the fish die- off was effectively spun by Klamath Project critics to drive a dizzying array of attacks aimed at the Bush Administration and federal agencies responsible for Klamath Project management. Well- coordinated media coverage surrounding several acts of litigation and proposed federal legislation in the two years since the fish die- off have effectively imprinted the environmentalists' message in the minds of many: • " Fish need water"; • " Klamath Project farmers were denied water in 2001 and no fish died in the Klamath River"; • " Klamath Project farmers received full supplies in 2002, and 33,000 salmon died in the river"; • " The Bush Administration sacrificed fish for the benefit of farmers." The claims discussed above are just a few of the more prominent arguments that Klamath Project critics have employed to justify a series of actions undertaken in the wake of the public release of the interim NRC Committee report, including the following: • Federal legislation that would finalize a controversial and flawed draft Klamath River flow report. • Unsuccessful federal legislation that would restrict the ability of local lease land farmers to grow row crops. • Litigation ( PCFFA v. USBR) that, if successful, would have likely shut down Klamath Project operations in 2003. • Public protests staged by tribal members and environmentalists in Klamath Falls in 2002 and in Sacramento in 2003. 30 Listing of the Klamath River as the third most endangered waterway in the country by American Rivers, a Washington, D. C. - based activist group. An unsuccessful lawsuit filed by environmental groups against NOAA Fisheries to hasten the potential ESA listing of the green sturgeon. The release of an Oregon Natural Resources Council ( ONRC) report, which contends that voluntary buyouts of willing sellers within the Project " remain the most politically responsible, socially just, and economically viable method" to address power and ecological challenges. A subsequent letter sent by ONRC to Project landowners, tempting them with the promise of a buyout that would provide them with 2 '/ z times the fair market value of their land. Numerous editorials, journal articles and magazine stories that clearly accept the arguments made by Project critics. However, others did not jump so quickly on to the " blame game bandwagon." During late summer and early fall of 2002, Dave Vogel, a fisheries biologist with 28 years of experience, conducted a field investigation to assess water temperatures in the main stem Klamath River. - Vogel noted that main stem water temperatures in the Klamath River were measured hourly just prior to and during the fall- run Chinook salmon migration season. He found that water temperatures in the upper Klarnath River downstream of Iron Gate Dam during September 2002 were unsuitable for adult salmon, a finding that was similar to that of previous studies. As expected, a normal seasonal cooling trend at the end of September and early October provided the moderating influence lowering Klamath River temperatures to tolerable levels for salmon. Vogel also found that large numbers of salmon entered the lower Klamath River earlier than usual and were exposed to two dramatic and uncharacteristic cooling and warming conditions causing disease outbreak from warm water and crowded conditions. The combination of these factors was chronically and cumulatively stressful to fish and is probably the most plausible reason for the fish die- off. " In my opinion, the best available scientific data and information indicate that the continued operation and maintenance of historical flows at Iron Gate Dam will not jeopardize coho salmon," said Vogel in March 2003. " Furthermore, in my opinion the operations of Iron Gate Dam during the summer and fall of 2002 did not cause and could not have prevented the fish die- off in the lower Klarnath River." Unfortunately, scant media coverage was afforded to Vogel's findings. Outside of the Upper Basin, the press made no mention of the fact that, despite the die- off, the numbers of fish returning to Iron Gate hatchery on the Klamath River were the third highest in 40 years. The media also largely ignored a similar finding made in October 2003 by the National Research Council Committee on Endangered and Threatened Fish in the Klamath Basin. In its final report, the Committee failed to find a linkage between the operation of the Klamath Project and the fish die- off, and questioned whether changes federal project operations at the time would have prevented it. Clearly, the hard working landowners of the Upper Klamath Basin have been on the receiving end of a cruel and long- distance war being waged by environmental activists who assert that the federal water project - representing only 2 percent of the total land base of the Klamath River watershed, and consuming only 3- 4 percent of the average annual flows to the Pacific Ocean - is somehow responsible for all of the environmental woes of the river system. These advocates are intent on portraying the Klamath Basin as a poster child to help fuel outside efforts that are focused on litigating, legislating and publicly condemning the local community for doing what it has done for 98 of the last 99 years - irrigating farm and ranch land. r r r r These interests know that federal water projects are an easy target of litigation, since federal environmental and clean water laws govern project operations. The lawsuits are often aimed at federal entities - such as the U. S. Bureau of Reclamation and fishery agencies - which, on the surface, give the appearance that the environmental plaintiffs are simply interested in correcting errors made by some non- descript governmental agency. The true intended target of these actions, however, ultimately becomes the landowners and water users who fall under the management jurisdiction of the federal agencies. It is the farmers and ranchers that pay the price of litigation through altered management practices, increased uncertainty, and escalating legal expenses to defend their interests. For the most part, the potentially damaging effects these actions could cause family farmers and ranchers have been deflected. However, local water users are concerned that permanent Klamath River policy will be influenced by misinformation in the future. Vindication, Part II After an 18- month barrage of anti- Klamath Project attacks in the media and courtrooms, the long- awaited final report from the National Research Council ( NRC) Committee on Endangered and Threatened Fishes in the Klamath Basin was released in October 2003. The final NRC report is important to local farmers and ranchers for several key reasons: 1. The report clearly indicated that recovery of endangered suckers and threatened coho salmon in the Klamath Basin cannot be achieved by actions that are exclusively or primarily focused on operation of the Klamath Project. 2. The committee also reconfirmed its findings from the earlier interim report that found no evidence of a causal connection between Upper Klamath Lake water levels and sucker health, or that higher flows on the Klamath River mainstem help coho salmon. 3. The NRC committee did not accept arguments that the operation of the Klamath Project caused the 2002 fish die- off or that changes in the operation of the Project at p the time would have prevented it. 32 r ~ r r Despite the final conclusions, some environmentalists and many in the media continue to maintain the sensational but unsupported position that the Klamath Project was responsible for the 2002 fish mortality that occurred over 200 miles from the Klamath Project. The final NRC report was consistent with what Upper Basin interests have been saying for years: the Klamath Project cannot solely bear the burden for species recovery in this basin. A watershed- wide approach to species recovery - one that addresses all the stressors to fish - is essential to improving the environment and saving the local economy. Local water users shared the NRC report's vision that increased knowledge, improved management, and cohesive community action would promote recovery of the fishes. At the same time, they remained extremely concerned that the " business as usual" approach - regulation of the Klamath Project - would remain the dominant aspect of ESA biological opinions and advocacy of Project opponents. For reasons now clearly evident, the irrigators' original recommendation for an outside technical review of the ESA activities in the Klamath basin by an objective group such as the r National Academy of Sciences back in 1993 ( KWUA 1993) was an important first step. The benefits of an ESA peer review are obvious after reading the NRC's final report. " We are beginning to see signs of progress with ESA activities in the basin," said Dave Vogel, nearly one year after the release of the final NRC Committee report. " However, alarmingly, there are some individuals within the agencies that are in a state of denial over the findings and conclusions of the NRC's report. Despite the NRC's final report, the USFWS and NOAA Fisheries still have too much focus on the Klamath Project and not enough emphasis on a watershed- wide approach." Other experts agree. " We found that the prevailing scientific sentiment in the basin-' More water is better for fish'- was the wrong approach," NRC Committee member Jeffrey Mount told California Farmer magazine in December 2003, two months after the final NRC report was released. " We hate to say we told you so, but...." It is very important to note that many of the most pertinent findings, conclusions, and r recommendations of the NRC Klamath Committee were not new to the USFWS or NOAA Fisheries. Dave Vogel elaborated on this in testimony he provided to the House Resources Committee at a field hearing held in Klamath Falls in June 2004. " The NRC final report advocates a watershed approach, peer review, greater stakeholder involvement, oversight of agency actions, focus on factors other than the Klamath Project 33 r operations, reduction of resource conflicts, and incorporation of the principles of adaptive management toward species recovery," said Vogel. " Over the past decade, local water users and their allies forwarded much of the same and similar technical findings and recommendations to those two agencies, but were mainly ignored. Additionally, the NRC's major conclusion that there is insufficient scientific justification for high reservoir levels and high instream flows was always prominent in water users' technical comments on the agencies' biological opinions during the past decade." r " The NRC Klamath Committee's final report was an outstanding effort and the product must serve as a catalyst to advance balanced natural resource management in the basin," Vogel said. " If federal agencies meaningfully incorporate many of the NRC's principal findings, conclusions, and recommendations, we fully expect positive results to the species recovery and reduced resource conflicts. We should use the momentum of the NRC's final report to guide recovery efforts and watershed improvements. However, if the agencies do not take this pro- active approach, we could again return to the disaster that transpired in 2001." • Dr. Mount agrees. r " For too long, Klamath managers have relied on fixing their problems by turning only one knob- the knob of raising and lowering water levels in Upper Klamath Lake and the river," said Mount, a University of California professor. " They need to take new approaches that support multiple populations offish and healthy ecosystems throughout the watershed," he said. The Klamath Project Regulatory Regime: 3 Years After the Curtailment The U. S. Bureau of Reclamation's final 10- year Biological Assessment for Klamath Project 2002- 2012 operations properly incorporated the findings of the 2002 interim National Research Council's ( NRC) interim report, and generally captured the essence of the " watershed- wide" philosophy endorsed in the final 2003 NRC report. Unfortunately, the fishery agency biological opinions ( BOs) do not. Despite the so- called ecosystem approach to species recovery advocated by the USFWS and NMFS, their actions in the Klamath basin over the past decade amply demonstrates that the exact opposite took place. They focused on: 1) a single- species approach; and 2) Klamath Project operations. The USFWS opinion continues to perpetuate the questionable assumption that lake level management is the principle mechanism affecting sucker survival in Upper Klamath Lake ( UKL). The NOAA Fisheries jeopardy decision similarly continues to place high emphasis on downstream flows. The stored water developed for Klamath Project farmers continues to be reallocated to meet the artificial demands set by agency biologists. 34 r The combined - and apparently, unanticipated - impacts placed on the Upper Basin community from the application of the two opinions are unacceptable. On June 25th, 2003, local irrigators were told by Reclamation officials that UKL diversions to the Project would be shut down for a minimum of 5 days - in the middle of the growing season. By day's end, reason prevailed: the agencies backed off their initial request9 and instead, Reclamation notified farmers to continue their efforts to reduce diversions from the lake. This was driven by one apparent agency mission: to avoid dropping UKL one inch below a lake level requirement established by the USFWS. Rancher Gary Wright learns that the Klamath Project would be shut down in the middle of the irrigation season, June 25, 2003. Common sense prevailed, and later in the day, Reclamation rescinded its earlier decision. In addition to the continued uncertainty irrigators face, the opinions are generating new, unanticipated impacts to the community. In the past 40 to 50 years, while the cropping pattern in the Klamath Project has varied from year to year, the overall planted acreage has remained consistent. On the other hand, the 2002- 2012 biological opinion created by NOAA Fisheries for coho salmon established the river flow schedule and an " environmental water bank" - which ratchets up to 100,000 acre- feet in 2005, regardless of actual hydrologic conditions - that is the primary source of new demand for water in the Klamath River watershed. The result: stored water that has flowed to farms, ranches and the refuges for nearly 100 years is now sent downstream at such high levels, that groundwater pumped from the Lost River basin is being used to supplement the resulting " coho salmon demand" in the Klamath River. 9 Improved coordination between USFWS managers and their Reclamation counterparts in Klamath Falls and Sacramento was one important reason for the positive corrective action that was taken. 35 It is not the farmers who have imposed new water demands that, in essence, have made groundwater the default supplemental supply to the Klamath Project. It is the opinions of agency fishery biologists who have fundamentally altered how this century- old water project operates, and who have apparently failed to anticipate the resulting impacts to the community. While Reclamation in 2002 sharply disagreed with the findings of both fishery agency biological opinions, it is not yet clear how consultation will be reinitiated to create a new operations plan. Proactive Efforts of Upper Basin Landowners Since the early 1990s, and particularly in the new millennium, local water users - both within the Klamath Project and those who farm in upstream areas north of Upper Klamath Lake - have taken proactive steps to protect and enhance water supplies, enhance the environment, r and stabilize the agricultural economy. Farmers and ranchers in the Klamath Project have consistently supported restoration actions to improve habitat for the basin's fish and wildlife species. Sucker Recovery Planning KWUA in 1993 published the Initial Ecosystem Restoration Plan - the first ecosystem- based, scientifically valid planning document on Klamath Basin restoration. The plan placed particular emphasis on real, on- the- ground projects to recover endangered species. It was widely recognized as a meaningful assessment of necessary restoration activities. KWUA in 2001 reiterated its previous call with the release of a report entitled Protecting the Beneficial Uses of Upper Klamath Lake: A Plan to Accelerate Recovery of the Lost River and Shortnose Suckers. The 2001 report provided timelines and budgets for dozens of projects that could provide real benefits. Regrettably, until the past three years, there has been failure to effectively implement most of the on- the- ground activities proposed by KWUA. On- the- Ground Actions Local agricultural and business leaders have dedicated thousands of volunteer hours and have spent millions of dollars in the past ten years to participate in processes associated with environmental restoration, Klamath Basin water rights adjudication, dispute resolution, drought- proofing, and water supply enhancement. Most impressive, however, is the multitude of actions undertaken on- the- ground: • Local efforts to assist National Wildlife Refuges ( e. g. " Walking Wetlands") • Ecosystem Enhancement and Sucker Recovery Efforts in the Upper Basin • Fish Passage Improvement Projects • Wildlife Enhancement and Wetland Restoration Efforts • Local Efforts to Improve Water Quality 36 • Power Resource Development • Efforts to Improve Klamath Project Water Supply Reliability and Water Use Efficiency Many of these efforts were driven by an initial desire to implement meaningful restoration actions intended to provide some sort of mitigation " credit" that could be applied towards reducing the burden carried by Klamath Project irrigators to " protect" threatened and endangered fish species. For many years, that credit was not recognized. For example, Federal agencies or non- profit conservation groups have acquired over 25,000 acres of farmland in the Upper Klamath Basin for habitat purposes. Each time the agencies sought additional land, they promised that each acquisition would provide environmental benefits, reducing pressure on the Klamath Project's family farmers and ranchers. Those promises have not materialized, and Project irrigation water still remains the sole regulatory tool used to address federal ESA objectives for endangered suckers and threatened coho salmon in the Klamath River watershed. • TEAMWORK A broad range of partners include U. S. Fish and Wildlife, Bureau of Reclamation. CalOre Wetlands. Tulelake Growers Association, Audubon Society. Tulelake Irrigation District, California Waterfowl Association. University of California. Ducks Unlimited. Klamath Water Users Association. USDA NRCS. Leaseland Advisory Council, and numerous volunteer organizations. A page from the " Refuge" section of the tule- Iake. com website. Environmental Water Bank KWUA in early March 2003 announced it would support, and assist the Department of Interior in the implementation of, a Klamath Project Pilot Environmental Water Bank in 2003 to provide over 50,000 acre- feet of additional water for environmental purposes. Reclamation's 10- year Biological Assessment ( BA) developed in February 2002 proposed an environmental water bank through which willing buyers and sellers will provide additional water supplies for fish and wildlife purposes and to enhance tribal trust resources. The 2002- 2012 biological opinion created by NOAA Fisheries for coho salmon firmly established the river flow schedule and the water bank - which ratchets up to 100,000 acre- feet in 2005, regardless of actual hydrologic conditions - that is the primary source of new demand for water in the Klamath River watershed. 37 The coho biological opinion's rigid water bank schedule, which steps up the magnitude of the bank for the first four years, regardless of actual hydrology, is difficult to justify. This type of water bank does not reflect the intent of either the proposal put forth by KWUA in 2002 ( see below), or the original USBR biological assessment, which proposed implementation of a water bank in drier years, not every year. Water users committed to pursue developing a water bank with Reclamation in January 2002. At that time, KWUA was asked by Reclamation to develop a Project- wide water bank to assist with meeting environmental water demands in drier years. KWUA's Water Bank and Supply Enhancement Committee held over 30 meetings in 2002- 03 to develop the 65- page report/ proposal for a long- term water bank, which differs substantially from the pilot water bank proposed by Reclamation this past year. Certainty of water supplies is a key principle imbedded in KWUA's long- term water bank proposal. Local water users insist that, in exchange for voluntary participation in a Project water bank - which would be used to " fund" environmental water needs - 100% of the irrigation demand for remaining Project acreage will be satisfied, season- long. Water users further believe that the water bank cannot be viewed as a stand- alone element. While Reclamation's 2003 and 2004 pilot programs did not closely resemble KWUA's vision for a long- term bank, water users are hopeful that Reclamation and Interior will look to the irrigators' document to complete its 10- year water bank proposal. EQIP Funding in Klamath Basin The federal government in 2003 released $ 7 million in conservation funding to the Klamath Basin. This sum represents a portion of the $ 50 million in funding earmarked for the Basin in the 2002 Farm Bill under the Environmental Quality Incentives Program ( EQIP). KWUA was instrumental in securing these provisions during Farm Bill negotiations. In 2004, Interior Secretary Norton included another $ 12 million for this program in the president's 2005 budget request. The funds provided cost- share payments to farmers and ranchers to employ water conservation measures. Over 800 Klamath Basin landowners have applied to participate in this program, despite the requirement that they pay 25% of the costs. This shows remarkable commitment by local irrigators to do the right thing, despite the fact that many of these landowners are still recovering from the financial impacts of the 2001 water curtailment. Recognition at Last In the past year, local irrigators have finally begun to get the recognition - if not the actual regulatory relief- they deserve for their proactive efforts. To wit: • KWUA was awarded the 2003 " Leadership in Conservation" award by the Oregon Department of Agriculture; • KWUA in 2004 was honored on the steps of the Oregon state capitol for " exemplifying the spirit" of the Oregon Plan for Salmon and Watersheds; 38 Tulelake Irrigation District in January 2004 received the F. Gordon Johnston award for its innovative canal lining project completed near Newell; and U. S. Secretary of Agriculture Ann Veneman and NRCS chief Bruce Knight in 2004 recognized local rancher Mike Byrne for his leadership in conservation. NRCS Chief Bruce Knight ( left) with 2004 Excellence in Conservation Award winner Mike Byrne. It is clear that local irrigators have not been idle in the past ten years. Their efforts to improve their environment are all the more impressive when one considers that the uncertainty and difficulty associated with keeping their farming operations profitable have not diminished. Oregon Governor Ted Kulongoski, Congressman Greg Walden and KWUA Executive Director Dan Keppen at the new A Canal Headgates, April 2003. 39 50 Years After the Compact - Back to the Watershed- Wide Approach Klamath Project water users in October 2004 enthusiastically greeted the announcement that the states of California and Oregon and the Bush Administration had signed the historic " Klamath River Watershed Coordination Agreement". The agreement - signed by California Governor Arnold Schwarzenegger, Oregon Governor Ted Kulongoski, and four of President Bush's cabinet level secretaries - underscored the commitment of these parties to solve the fisheries challenges of the Klamath River on a watershed - wide basis. The state- federal Klamath agreement reflects the philosophy embedded in both the Klamath River Basin Compact and the 2003 NRC Klamath report, which confirmed that Klamath Basin issues must be dealt with in an integrated and comprehensive way for a lasting solution of the challenges facing the basin. The NRC committee report makes clear that merely closing the spigot on the Klamath Project will not solve the problems facing Klamath Basin fisheries, and that strategy obviously was disastrous for farming and ranching communities. The coordination agreement recognizes that message and promotes a unified effort that many water users believe is much needed. An important part of this agreement is that it supports the Conservation Implementation Program ( CIP), a work in progress proposed by federal agencies to coordinate management actions in the Klamath River watershed. The CIP would meld a scientific advisory body, local communities, and resource agencies to identify, coordinate and resolve the Basin's critical water quality, water quantity and fish and wildlife restoration challenges. KWUA is working with other producer groups and local government to develop guidelines that make the CIP workable and acceptable to Klamath Basin communities. USBR Study on Pre- Project Flow Conditions on Upper Klamath River Reclamation in late 2004 finalized a draft study intended to provide a glimpse at how the Klamath River might have looked before the Klamath Project was built. The report shows that- especially in drier years - historic flows in the Klamath River near Keno, Oregon dwindled to a mere trickle. The report provides compelling evidence that supports claims made by local residents for decades - the stored water provided by the Klamath Project may actually provide more flows downriver than what would have flowed before the Project was built. This is primarily due to the developed storage and the fact that farmlands that were once under water now use less water than what was historically lost to consumptive and evaporative use of the former marshes. 40 Ufric; lfftid Kur , Jhm% tr Excerpt from Draft BOR Flow Study 41 Conclusion - The Future To solve the problems of the Klamath River watershed, we need a coordinated management program that spans two states in a watershed that is characterized by a strong federal presence. Competition among stakeholder groups - including four tribes, agricultural water users, and countless environmental groups - is fierce. In order to be successful, we need to better understand the real state of the watershed by developing the facts and best possible information to make the best possible decisions. Collaborations need to replace ideological advocacies; watershed wide approaches need to replace regionalism; and honest exchanges of information need to displace environmental sensationalism. A June 20, 2004 editorial published by the Klamath Falls Herald & News provides an apt glimpse of what the future might bring to the Klamath irrigation community and how the Klamath Water Users Association will address that future: Recently, the Klamath Water Users Association got an award for not using water, which is not a contradiction in terms at all. It's a matter of doing what has to be done to keep farming and ranching alive in the Klamath Basin. The award was from the state of Oregon and recognized the water users' efforts in behalf of the Oregon Plan for Salmon and Watersheds. It was presented to the group in a ceremony on the steps of the Capitol with leaders such as Gov. Ted Kulongoski and the Democratic and Republican leaders of the Legislature participating. The award recognizes a welter of actions in the Basin, some using federal and state dollars and some not, many aimed at making agricultural operations more efficient water users. Some have given agriculture interests heartache, such as the conversion of farmlands to wetlands - the water users cite 24,000 acres in the past decade, equal to more than a tenth of the Klamath Reclamation Project. Nevertheless, it's clear that farmers and ranchers have recognized their predicament given the pressure of the Endangered Species Act and competition for water from Indian tribes upstream and down. Agriculture is in the midst of a struggle that could take decades yet to play out, and its defenders are determined that they will survive. This is a longer- term version of the creativity they showed in 2001, when, faced with imminent ruin, they responded with skill and imagination in a political protest that brought national attention and saved Basin agriculture to fight another day. The vision of the Klamath Basin as a place for human habitation must include agriculture, and an agricultural sector of sufficient size to be economically viable. This place ought to have an urban center and a scattering of pleasant small towns - and in between green fields with dancing water from irrigation works. ~ 42 Whatever alternate vision exists involves blowing away towns such as Merrill Malin and Tulelake and shriveling the city ofKlamath Falls. It involves throwing lots of people off the land, and itfs not acceptable. This is not the first such award, and won't be the last. It is a signal of a widening recognition in Oregon and the nation that farmers and ranchers will do good things here to make sure that they can continue in their necessary and honorable work. The Klamath Water Users Association, with the talents and support of the community, will continue to address the resource needs of its constituency in a proactive and creative manner. The KWUA has shown itself to be steadfast and able in protecting water users while being receptive to innovative and reasonable solutions. Our irrigating communities, through the continued efforts of the KWUA, will always be persistent and adaptable representatives of our American heritage. The " future".. . bring it on, we can handle it. r Father and daughter ride to the headgates, summer 2001. 43 Notes Information sources used in the preceding report sections are further described below. Overview The source for much of this information comes from the Klamath Water Users Association 2003 Water Bank report. Pioneers The Department of the Interior, United States Reclamation Service 1913 report entitled " History of the Klamath Project. Oregon- California. From May 1, 1903 to December 13, 1912", written by I. S. Voorhees, contains detailed accounting of early irrigation works in the Upper Klamath Basin. Paul Simmons of Somach Simmons and Dunn also made significant contributions based on research he and his staff conducted on behalf of Klamath Project water users in the State of Oregon Klamath River adjudication process. The Klamath Basin Calls in the United States Government *— The Voorhees document, noted above, details this issue. Construction Begins The source for much of this information comes from the Klamath Water Users Association 2003 Water Bank report, the Voorhees report, and the affidavit and testimony of Rebecca Meta Bunse, who in 2004 prepared a detailed historic summary of Klamath Project development on behalf of Klamath Project irrigators for the Klamath River adjudication process. ( Reference No. 003E00040050, before the Office of Administrative Hearings, State of Oregon, for the Water Resources Department). Paul Simmons of Somach Simmons and Dunn also made significant contributions based on research he and his staff conducted on behalf of Klamath Project water users in the State of Oregon Klamath River adjudication process. The Bureau of Reclamation Klamath Basin Area Office also provided factual data on the Klamath Project. Homesteaders The Journal of the Modoc County Historical Society, No. 18- 1996, focuses exclusively on twentieth century development of the Tule Lake area. Betty Lou Byrne- Shirely's " The Reclamation of Tule Lake" and the February 1947 Reclamation Era article " Gold Mine in the Sky", both included in the Modoc County historical journal, served as sources for the homesteader information. Quotes made by Dave Carman, a World War II veteran Tule Lake homesteader, were pulled from his testimony submitted at a House Resources Committee field hearing in Klamath Falls in June 2004. The Klamath River Compact The source for much of this information regarding development of the Compact comes from the affidavit and testimony of Stephen R. Wee, who in 2004 prepared a detailed historic summary of Klamath Project water rights and related issues on behalf of Klamath Project irrigators for the Klamath River adjudication process. ( Reference No. 003E00040049, before the Office of Administrative 44 - r Hearings, State of Oregon, for the Water Resources Department). The conclusion of this section contains the actual purposes of the Compact, as identified in Article I of that document. The Klamath Project's Finishing Touches The source for much of this information comes from the Klamath Water Users Association 2003 Water Bank report, the Voorhees report, and the affidavit and testimony of Rebecca Meta Bunse, who in 2004 prepared a detailed historic summary of Klamath Project development on behalf of Klamath Project irrigators for the Klamath River adjudication process. ( Reference No. 003E00040050, before the Office of Administrative Hearings, State of Oregon, for the Water Resources Department). Paul Simmons of Somach Simmons and Dunn also made significant contributions based on research he and his staff conducted on behalf of Klamath Project water users in the State of Oregon Klamath River adjudication process. New Demands Legal documents prepared by the Klamath Water Users Association attorney - Paul Simmons, of Somach, Simmons & Dunn - provide much of the background information regarding the steadily increasing regulations faced by Project irrigators, starting in the 1990s. Specifically, the plaintiffs' memorandum of points and authorities in support of motion for preliminary injunction ( Kandra et al v. United States of America) was relied upon. Also, David Vogel's testimony before the U. S. House of Representatives Committee on Resources oversight field hearing in June 2004 provides an excellent treatise on the real reasons for the decline of suckers in the Upper Klamath Basin. The Klamath Water Users Association previously developed the section that assesses stressors to coho salmon during the 1990s. Problems on the East Side This section derives from an excellent letter ( dated July 28, 2004) prepared by Best Best & Krieger on behalf of Horsefly Irrigation District and Langell Valley Irrigation District. The letter was submitted to the U. S. House of Representatives Resources Committee in connection with a congressional field hearing held in Klamath Falls in July 2004. 2001 Curtailment Of the numerous media accounts of the 2001 water cutoff, I believe Blake Hurst's piece " Calamity in Klamath", which originally was published in The American Enterprise magazine in late 2002, is the best. I have borrowed liberally from Mr. Hurst, particularly his assessment of the impacts to the community of Tulelake, California. Jess Prosser's comments were originally printed in Range Magazine in 2001. The Farmers Fight Back The comments regarding the " desperate community" were pulled from an outstanding paper presented by Paul Simmons at the American Bar Association Environmental Section Fall 2004 Meeting. 45 Enter President Bush I was in the audience when President Bush made his speech in Portland. After the president's speech, I met Congressman Greg Walden for the first time; he conveyed to me some of the details of the president's flight over the Klamath Basin earlier in the day. Vindication: The National Research Council Steps In This section was derived from press statements developed by KWUA in early 2002. The Assault on the Klamath Project Intensifies Most of this section derives from personal experience, and the latter part was pulled directly from an opinion piece I was asked to write for a Boise, Idaho newspaper at the request of Idaho water users who were also being attacked by some of the same activists engaged in Klamath issues. Vindication, Part II / " We hate to say we told you so, but...." Much of this information originates in Dave Vogel's written testimony that he submitted to the House Resources Committee in June 2004. After more than a decade of professional and sometimes, personal criticism by agency and tribal biologists, the final NRC Report perhaps vindicated Dave Vogel more than anyone else. The Klamath Project Regulatory Regime: 3 Years After the Curtailment This section was written based on personal experience of the author. Proactive Efforts of Upper Basin Landowners We refer you to www. kwua. org and a 45- page document entitled Summary of Recent and Proposed Environmental Restoration and Water Conservation Efforts Undertaken by Klamath Water Users and Basin Landowners for further information on this topic. 50 Years After the Compact - Back to the Watershed- Wide Approach This perspective comes from KWUA assessments and press releases. USBR Study on Pre- Project Flow Conditions on Upper Klamath River The USBR study is incredibly important, because, for the first time, it provides a numerical modeling assessment of the conditions that likely existed on the Upper Klamath River before Europeans settled the area. Prior to this effort, assertions that flow conditions in the river were likely lower than the present could only be backed up by anecdotal ( albeit accurate) reports and incomplete flow studies. Conclusion - The Future The June 20, 2004 Herald & News editorial on recent water user efforts provided a fitting ending to this report, which is further enhanced by language developed by Steve Kandra, 2004- 05 KWUA President. 46 Lower Klamath Lake National Wildlife Refuge, California Photo Credits 1. Cover photo - courtesy of Jacqui Krizo. 2. Map of Klamath Project - courtesy of Bureau of Reclamation. 3. " A load of produce from the Klamath Fair, October 1907" - courtesy of Tulelake- Butte Valley _ Fair, Museum of Local History ( TBVF Museum). 4. " 1906 Map of Pre- Project Area" - courtesy of Oregon Water Resources Department. 5. " Adams Cut, July 18, 1906" - courtesy of Tulelake - Butte Valley Fair, Museum of Local History. 6. " 1907 Completion of the A Canal Headgates" - courtesy of U. S. Bureau of Reclamation. 7. " Constructing Clear Lake Dam, September, 1909" - courtesy of TBVF Museum. 8. " 1927 Homesteader Affidavit" - courtesy of Somach, Simmons and Dunn 9. " Farm Lottery Article, Life Magazine" - courtesy of Bureau of Reclamation. 10. " The Sign Says it AH" - courtesy of U. S. Bureau of Reclamation. 11. " Homesteaders: Robinsons in 2001 Remember Days Gone By" - courtesy of Anders Tomlinson 12. J. C. Boyle Dam on the Klamath River - courtesy of PacifiCorp. 13. " Tulelake, California" - courtesy of Rob Crawford r l4. " Del Norte Salmon Cannery" - courtesy of Anders Tomlinson 15. " April 6, 2004 Headlines" - courtesy of Anders Tomlinson 16. " Kliewer Family in Dry Fields South of Klamath Falls" - courtesy of Anders Tomlinson 17. " Cemeteries went Dry in 2001" - courtesy of Rob Crawford 18. " Time Magazine Captures Rob Crawford & Family" - courtesy of Rob Crawford 19. Klamath Bucket Brigade - courtesy of Klamath Relief Fund. 20. Prayer / Protest at Headgates - courtesy of Klamath Relief Fund. 21. President Bush Photo courtesy of Rob Crawford _ 22. Tulelake Rancher Gary Wright, June 2003 - courtesy of Pat Ratliff 23. Walking Wetlands photo - courtesy of Anders Tomlinson. 24. Bruce Knight and Mike Byrne - courtesy of U. S. Department of Agriculture 25. Gov. Kulongoski, Rep. Walden, and Dan Keppen at the A Canal, 2003 - Courtesy of Pat Ratliff 26. Undepleted Natural Flow of the Upper Klamath River - U. S. Bureau of Reclamation. 27. " Father and Daughter Ride to the Headgates" - courtesy of Rob Crawford 28. " Lower Klamath Lake National Wildlife Refuge, California" - courtesy of Scott Harding Photography r — 47
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83. [Image] Utilization of geothermal energy for methane production for J. A. Albertson Land and Cattle Company
To utilize the geothermal energy in the area of its 30,000-head cattle feedlot, J.A. Albertson Land and Cattle Co. is considering the development of an integrated geothermal/bioconversion system that would ...Citation Citation
- Title:
- Utilization of geothermal energy for methane production for J. A. Albertson Land and Cattle Company
- Author:
- Bissell, R.R.
- Year:
- 1980
To utilize the geothermal energy in the area of its 30,000-head cattle feedlot, J.A. Albertson Land and Cattle Co. is considering the development of an integrated geothermal/bioconversion system that would use the cattle manure as a feedstock for an anaerobic-digestion plant to produce methane plus a digester-residue cattle-feed supplement. The feedlot lies within a high-temperature gradient and heat-flow area associated with the Western Snake River basin in Malheur Co., Oregon. The three digesters designed for the process will operate mesophilically (at 98/sup 0/F) with a 20-day retention time. To make up the digesters' heat losses, the geothermal water source will need to be about 135/sup 0/F and have a flow rate of 120-240 gpm, depending on the size ultimately selected for the facility. If the digester residue replaces alfalfa hay in the cattle's current rations, its value will amount to $1.15 million/yr. Burning the methane in engine/generator sets would produce 985-1970 kW of electric power that could be either sold or used as a day-to-day substitute for the geothermal heat. An economic analysis of the system is presented; DOE/ET/27230-T2
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ASP, a low-power, in-field Automated Seismic Processor of microearthquake network data has been designed, fabricated, and deployed for initial operation in four different field areas to monitor seismicity ...
Citation Citation
- Title:
- ASP: An Automated Seismic Processor for Microearthquake Networks
- Author:
- McEvilly, T. V.
- Year:
- 1981
ASP, a low-power, in-field Automated Seismic Processor of microearthquake network data has been designed, fabricated, and deployed for initial operation in four different field areas to monitor seismicity associated with two geothermal areas (The Geysers, California, and Cerro Prieto, Mexico), a nuclear explosion with its related collapse and aftershock sequence, and late (> 1 year) activity in a major aftershock series (Livermore, California). A second ASP system, with a high-speed front-end, is used in acoustic emission (1-20 kHz) analysis for fracture monitoring. Each of the 15 channels of ASP (configured for up to 128 channels) automatically detects, measures times and amplitudes, and computes and fits FFr's for both the P and S waves on data sampled at 100 samples/sec. These data from each channel are then processed with a central microprocessor for hypocenter location, running b-values, source parameters, event count, and P-wave polarities. The system is capable of processing a 15-station detection in approximately 40 seconds, excluding print-out. The initial trials have demonstrated that infield real-time analysis of data maximizes the efficiency of microearthquake surveys allowing flexibility in experimental procedures, with a minimum of the traditional labor-intensive postprocessing. Current efforts are directed towards improving efficiency of computation and data output and in expanding software capabilities
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Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, ...
Citation Citation
- Title:
- Water quality conditions in Upper Klamath and Agency Lakes, Oregon, 2005
- Author:
- Hoilman, Gene R
- Year:
- 2008
Agency Lakes. Oregon. 2005 M.Wood By Gene R. Hoilman, Mary K. Lindenberg, and Tamara Abstract During June-October 2005, water quality data were collected from Upper Klamath and Agency Lakes In Oregon, and meteorological data were collected around and within Upper Klamath Lake. Data recorded at two continuous water quality monitors In Agency Lake showed similar temperature patterns throughout the field season, but data recorded at the northern site showed more day-to-day variability for dissolved oxygen concentration and saturation after late June and more day-to-day variability for pH and specific conductance values after mid-July. Data recorded from the northern and southern parts of Agency Lake showed more comparable day-to-day variability in dissolved oxygen concentrations and pH from September through the end of the monitoring period. For Upper Klamath Lake, seasonal (late July through early August) lows of dissolved oxygen concentrations and saturation were coincident with a seasonal low of pH values and seasonal highs of ammonia and orthophosphate concentrations, specific conductance values, and water temperatures. Patterns in these parameters, excluding water temperature, were associated with bloom dynamics of the cyanobacterium (blue-green alga) Aphanizomenonflos-aquae in Upper Klamath Lake. In Upper Klamath Lake, water temperature in excess of 28 degrees Celsius (a high stress threshold for Upper Klamath Lake suckers) was recorded only once at one site during the field season. Large areas of Upper Klamath Lake had periods of dissolved oxygen concentration of less than 4 milligrams per liter and pH value greater than 9.7, but these conditions were not persistent throughout days at most sites. Dissolved oxygen concentrations in Upper Klamath Lake on time scales of days and months appeared to be influenced, in part, by bathymetry and prevailing current flow patterns. Diel patterns of water column stratification were evident, even at the deepest sites. This diel pattern of stratification was attributable to diel wind speed patterns and the shallow nature of most of Upper Klamath Lake. Timing of the daily extreme values of dissolved oxygen concentration, pH, and water temperature was less distinct with increased water column depth. Chlorophyll a concentrations varied spatially and temporally throughout Upper Klamath Lake. Location greatly affected algal concentrations, in turn affecting nutrient and dissolved oxygen concentrations—some of the highest chlorophyll a concentrations were associated with the lowest dissolved oxygen concentrations and the highest un-ionized ammonia concentrations. The occurrence of the low dissolved oxygen and high un-ionized ammonia concentrations coincided with a decline in algae resulting from cell death, as rn.easu.red by concentrations of chlorophyll a. Dissolved oxygen production, rates in. experim.en.ts were as high as 1.47 milligrams of oxygen per liter per hour, and consumption rates were as much as -0.73 milligrams of oxygen per liter per hour. Dissolved oxygen, consumption rates measured in. this study were comparable to those measured in a 2002 Upper Klamath Lake study, and a higher rate of dissolved oxygen consumption was recorded in. dark bottles positioned higher in the water column. Data, though, inconclusive, indicated that a decreasing trend of dissolved oxygen productivity through July could have contributed to the decreasing dissolved oxygen concentrations and percent saturation recorded in Upper Klamath Lake during this time. Phytoplankton self-shading was evident from, a general inverse relation between depth of photic zone and chlorophyll a concentrations. This shading caused net dissolved oxygen consumption during daylight hours in lower parts of the water column that would otherwise have been in the photic zone. Meteorological data collected in and around Upper Klamath Lake showed that winds were likely to come from a broad range of westerly directions in the northern one-third of the lake, but tended to come from a narrow range of northwesterly directions over the main body of the lake farther south.
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One chapter of a seven chapter annual report from 1999 examining ecological issues regarding the shortnose and Lost River sucker populations in Upper Klamath Lake and Williamson River.
Citation Citation
- Title:
- Effects of water quality on growth of juvenile shortnose suckers, Chasmistes brevirostris (Catostomidae: Cypriniformes), from Upper Klamath Lake, Oregon
- Author:
- Oregon Cooperative Wildlife Research Unit
- Year:
- 2000, 2005
One chapter of a seven chapter annual report from 1999 examining ecological issues regarding the shortnose and Lost River sucker populations in Upper Klamath Lake and Williamson River.
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"Serial no. 107-39."
Citation Citation
- Title:
- Water management and endangered species issues in the Klamath Basin : oversight field hearing before the Committee on Resources, U.S. House of Representatives, One Hundred Seventh Congress, first session, June 16, 2001 in Klamath Falls, Oregon
- Author:
- United States. Congress. House. Committee on Resources
- Year:
- 2002, 2005, 2004
"Serial no. 107-39."
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89. [Image] Forestry program for Oregon
This document sets forth the Board of Forestry's strategic vision for Oregon's forests for the next eight yearsCitation -
CONTENTS. Page Introduction 2620 5 Climatic conditions 2620 6 Units of measurement 2620 7 Losses by seepage and evaporation 2620 7 Duty of water 26208-10 Evaporation 2620 12 Soil and water analyses ...
Citation Citation
- Title:
- Irrigation in Klamath County : cooperative irrigation investigation with the Office of Experiment Stations, United States Department of Agriculture
- Author:
- Kent, F.L. (Fred LeRoy)
- Year:
- 1905, 2005
CONTENTS. Page Introduction 2620 5 Climatic conditions 2620 6 Units of measurement 2620 7 Losses by seepage and evaporation 2620 7 Duty of water 26208-10 Evaporation 2620 12 Soil and water analyses 262014-15 Data relative to alfalfa growing 2620 15 Summary 2620 16 ILLUSTRATIONS. I. Wing dam at intake of Ankeny canal 269 4 II. Checked field of M. E. Robinson 2620 10 III. Headgate, Ankeny canal 2620 11
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Quigley, Thomas M.; Arbelbide, Sylvia J., tech. eds. 1997. An assessment of ecosystem components in the interior Columbia basin and portions of the Klamath and Great Basins: volume 1. Gen. Tech. Rep. PNW-GTR-405. ...
Citation Citation
- Title:
- An assessment of ecosystem components in the interior Columbia Basin and portions of the Klamath and Great Basins [volume 1]
- Author:
- Quigley, Thomas Milton; Arbelbide, S. J. (Sylvia J.)
- Year:
- 1997, 2008, 2005
Quigley, Thomas M.; Arbelbide, Sylvia J., tech. eds. 1997. An assessment of ecosystem components in the interior Columbia basin and portions of the Klamath and Great Basins: volume 1. Gen. Tech. Rep. PNW-GTR-405. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 4 vol. (Quigley, Thomas M., tech. ed.; The Interior Columbia Basin Ecosystem Management Project: Scientific Assessment). The Assessment of Ecosystem Components in the Interior Columbia Basin and Portions of the Klamath and Great Basins provides detailed information about current conditions and trends for the biophysical and social systems within the Basin. This information can be used by land managers to develop broad land management goals and priorities and provides the context for decisions specific to smaller geographic areas. The Assessment area covers about 8 percent of the U.S. land area, 24 percent of the Nation's National Forest System lands, 10 percent of the Nation's BLM-administered lands, and contains about 1.2 percent of the Nation's population. This results in a population density that is less than one-sixth of the U.S. average. The area has experienced recent, rapid population growth and generally has a robust, diverse economy. As compared to historic conditions, the terrestrial, aquatic, forest, and rangeland systems have undergone dramatic changes. Forested landscapes are more susceptible to fire, insect, and disease than under historic conditions. Rangelands are highly susceptible to noxious weed invasion. The disturbance regimes that operate on forest and rangeland have changed substantially, with lethal fires dominating many areas where non-lethal fires were the norm historically. Terrestrial habitats that have experienced the greatest decline include the native grassland, native shrubland, and old forest structures. There are areas within the Assessment area that have higher diversity than others. Aquatic systems are now more fragmented and isolated than historically and the introduction of non-native fish species has complicated current status of native fishes. Core habitat and population centers do remain as building blocks for restoration. Social and economic conditions within the Assessment area vary considerably, depending to a great extent on population, diversity of employment opportunities, and changing demographics. Those counties with the higher population densities and greater diversity of employment opportunities are generally more resilient to economic downturns. This Assessment provides a rich information base, including over 170 mapped themes with associated models and databases, from which future decisions can benefit. Keywords: Columbia basin, biophysical systems, social systems, ecosystem.
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ill., maps; Typescript (photocopy); Thesis (Ph. D.)--Oregon State University, 1978; Includes bibliographical references
Citation Citation
- Title:
- An investigation into the comparative utility of color infrared aerial photography and LANDSAT data for detailed surface cover type mapping within Crater Lake National Park, Oregon
- Author:
- Walsh, Stephen Joseph,
- Year:
- 1977, 2009
ill., maps; Typescript (photocopy); Thesis (Ph. D.)--Oregon State University, 1978; Includes bibliographical references
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95. [Image] A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California
A GEOLOGIC AND HYDROLOGIC RECONNAISSANCE OF LAVA BEDS NATIONAL MONUMENT AND VICINITY, CALIFORNIA By William R. Hotchkiss ABSTRACT Lava Beds National Monument is on the Modoc Plateau in Modoc and ...Citation Citation
- Title:
- A geologic and hydrologic reconnaissance of Lava Beds National Monument and vicinity, California
- Author:
- Hotchkiss, W. R
- Year:
- 1968, 2008, 2005
A GEOLOGIC AND HYDROLOGIC RECONNAISSANCE OF LAVA BEDS NATIONAL MONUMENT AND VICINITY, CALIFORNIA By William R. Hotchkiss ABSTRACT Lava Beds National Monument is on the Modoc Plateau in Modoc and Siskiyou Counties. The principal geologic units in the vicinity are volcanic rocks,, which in places are highly permeable, and poorly permeable lake sedimentary deposits, all probably post-Oligocene in age. Yields and specific capacities of wells in the unconfined water body within volcanic rocks and lake deposits range widely, but in general are low in the lake deposits and higher in the volcanic rocks. A confined water body, occurring in volcanic rocks underlying the lake deposits yields large quantities of water to three wells in the study area. Dissolved-solids content of ground water generally increases in proportion to the thickness of lake deposits penetrated and to proximity of the lake deposits. Water from wells drilled in the volcanic rocks several miles from the lake deposits, and from wells penetrating the confined water body in volcanic rocks underlying the lake deposits contains small to moderate quantities of dissolved solids. Ground-water supplies can be developed almost anywhere in the study area by drilling wells to depths below the water table. In addition, there is a reasonable possibility of developing wells in a confined water body underlying the water-table system-
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"February 1994." ; "Much of this document was taken directly from, or based on, the Bureau of Land Management's earlier studies of the Klamath River: the Final eligibility and suitability report for the ...
Citation Citation
- Title:
- Klamath wild and scenic river eligibility report and environmental assessment : Klamath River, Oregon : draft
- Author:
- United States. National Park Service. Pacific Northwest Region
- Year:
- 1994, 2004
"February 1994." ; "Much of this document was taken directly from, or based on, the Bureau of Land Management's earlier studies of the Klamath River: the Final eligibility and suitability report for the Upper Klamath wild and scenic river study and the Draft Klamath Falls area resource management plan and environmental impact statement. This assessment also borrowed heavily from the Final environmental impact statement for the Salt Caves hydroelectric project prepared by the Federal Energy Regulatory Commission."-p.i ; "State of Oregon application, Section 2(a)(ii) National Wild and Scenic Rivers Act."
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Humans have altered the Klamath River Canyon in many ways. This study focuses on the years from 1955 to 2003. One substantial alteration is the conversion of terraces into irrigated pastures for agriculture ...
Citation Citation
- Title:
- Land use and vegetation community changes at Beswick Ranch, Klamath River Canyon, California from 1955 to 2003 : focus on relationship between the irrigation and the vegetation and the land use cover
- Author:
- Bilka, Monika N.
- Year:
- 2002, 2005
Humans have altered the Klamath River Canyon in many ways. This study focuses on the years from 1955 to 2003. One substantial alteration is the conversion of terraces into irrigated pastures for agriculture and cattle ranching. This research project explains the relationships between the irrigation network and the vegetation and land use cover patterns that existed in the past and that exist today at Beswick Ranch. Data sources such as aerial photographs, maps, and other historical information are used to create Geographic Information System (GIS) maps and models of the area. Due to time constraints, the final maps and models are not complete at this time. However, the completed models were synthesized with observational data to come to preliminary conclusions. While the ditches of Shovel Creek Pasture have undergone little to no change at all since 1955, ranchers have added ditches to Faye Pasture. Ranch workers have also increased the amount of agricultural land use cover and decreased in tree cover of Faye Pasture. Conversely, ranchers increased the tree cover and non-agricultural land cover, and they have decreased the agricultural cover. The GIS coverages of Shovel Pasture remain in the preliminary stage, and further analyses of the calculated areas of land use cover and ditch lengths are needed to complete this study. In partnership with PacifiCorp and the BLM, this project aims to provide information about the impacts of the current and historical irrigation systems used on the pastures and riparian zones within this reach of the Klamath River Canyon from 1955 to 2003. Even at this stage, the preliminary coverages provide insight into the relationships between irrigation, vegetation communities, and land use cover that have occurred during the study period.
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By Lorraine E. Flint, Alan L. Flint, Debra S. Curry, Stewart A. Rounds, and Micelis C. Doyle Abstract The U.S. Geological Survey (USGS) collected water? quality data during 2002 and 2003 In ...
Citation Citation
- Title:
- Water-quality data from 2002 to 2003 and analysis of data gaps for development of total maximum daily loads in the Lower Klamath River basin, California
- Author:
- Flint, Lorraine E.; Flint, Alan L.; Curry, Debra S.; Rounds, Stewart A.; Doyle, Micelis C.
- Year:
- 2004, 2006, 2005
By Lorraine E. Flint, Alan L. Flint, Debra S. Curry, Stewart A. Rounds, and Micelis C. Doyle Abstract The U.S. Geological Survey (USGS) collected water? quality data during 2002 and 2003 In the Lower Klamath River Basin, in northern California, to support studies of river conditions as they pertain to the viability of Chinook and Coho salmon and endangered suckers. To address the data needs of the North Coast Regional Water Quality Control Board for the development of Total Maximum Daily Loads (TMDLs), water temperature, dissolved oxygen, specific conductance, and pH were continuously monitored at sites on the Klamath, Trinity, Shasta, and Lost Rivers. Water-quality samples were collected and analyzed for selected nutrients, organic carbon, chlorophyll-a, pheophytin-a, and trace elements. Sediment oxygen demand was measured on the Shasta River. Results of analysis of the data collected were used to identify locations in the Lower Klamath River Basin and periods of time during 200
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Abstract Quigley, Thomas M.; Haynes, Richard W.; Graham, Russell T., tech. eds. 1996. Integrated scientific assessment for ecosystem management in the interior Columbia basin and portions of the Klamath ...
Citation Citation
- Title:
- Integrated scientific assessment for ecosystem management in the interior Columbia Basin and portions of the Klamath and Great Basins
- Year:
- 1996, 2005, 2000
Abstract Quigley, Thomas M.; Haynes, Richard W.; Graham, Russell T., tech. eds. 1996. Integrated scientific assessment for ecosystem management in the interior Columbia basin and portions of the Klamath and Great Basins. Gen. Tech. Rep. PNW-GTR-382. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station. 303 p. (Quigley, Thomas M., tech. ed. The Interior Columbia Basin Ecosystem Management Project: Scientific Assessment.) The Integrated Scientific Assessment for Ecosystem Management for the Interior Columbia Basin links landscape, aquatic, terrestrial, social, and economic characterizations to describe biophysical and social systems. Integration was achieved through a framework built around six goals for ecosystem management and three different views of the future. These goals are: maintain evolutionary and ecological processes; manage for multiple ecological domains and evolutionary timeframes; maintain viable populations of native and desired non-native species; encourage social and economic resiliency; manage for places with definable values; and, manage to maintain a variety of ecosystem goods, services, and conditions that society wants. Ratings of relative ecological integrity and socioeconomic resiliency were used to make broad statements about ecosystem conditions in the Basin. Currently in the Basin high integrity and resiliency are found on 16 and 20 percent of the area, respectively. Low integrity and resiliency are found on 60 and 68 percent of the area. Different approaches to management can alter the risks to the assets of people living in the Basin and to the ecosystem itself. Continuation of current management leads to increasing risks while management approaches focusing on reserves or restoration result in trends that mostly stabilize or reduce risks. Even where ecological integrity is projected to improve with the application of active management, population increases and the pressures of expanding demands on resources may cause increasing trends in risk. Keywords: Ecosystem assessment, management and goals; ecological integrity; socio-economic resiliency; risk management
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100. [Image] Narrative history report of the Klamath Project land opening under Public Notice No. 47, 1948
Public Notice No. 47 of August 27, 1948, was prepared in conformity with recommendations for a standardized procedure made at the Salt Lake conference in March 1948; it opened to public entry 86 farm units ...Citation Citation
- Title:
- Narrative history report of the Klamath Project land opening under Public Notice No. 47, 1948
- Author:
- United State. Bureau of Reclamation
- Year:
- 1948, 2004
Public Notice No. 47 of August 27, 1948, was prepared in conformity with recommendations for a standardized procedure made at the Salt Lake conference in March 1948; it opened to public entry 86 farm units embracing 8,283 acres of irrigable land. Of nearly 24,000 application blanks sent out, 5,072 were returned during the simultaneous filing period. A five-man examining board placed 4,911 in the first priority group, 69 in the second priority group and rejected 91. The Regional Director reversed the action of the examining board in two instances making a total of 4,913 participating in the drawing. Applications were received from 39 states, the District of Columbia and the Territory of Alaska. California supplied 50% of all applications considered in the first priority group; Oregon supplied 27%; Utah supplied 6%; and the rest of the states supplied the remaining 17% The examining board interviewed 94 persons of 104 who were notified to appear for personal interviews after the drawing. Of those appearing for interviews, five refused to accept units in area "A" and three were rejectees whose appeals were later denied by the Regional Director. Of the ten who failed to appear for interview, five relinquished their award in writing; four were relegated to the end of their priority list, and one was the victim of an airplane accident. As the result of the drawing and subsequent interviews, 1.4% of the applicants from California 2.5% of the applicants from Oregon and 1.3% of the remaining applicants from other states were awarded farm units. Ten of the 39 states, from which applications were received, were represented in the settlement of the 86 farm units. Of the 23 who selected units in area "A", only two availed themselves of options to lease additional land in the Tulelake sump area* Apparently, because of high rental fees, the majority of the area "A" settlers could not afford to lease lands supplemental to their homestead. Therefore, since the development of area "A" lands will be a costly procedure, it is possible that in the future there may be cases of relin-quishment of units due to the homesteaders' inability to meet expenses. First unit was awarded on March 9, 1949; the last unit was awarded on June 20, 1949.