Oregon Explorer CrossSearch Search Results

1. [Image] Temperatures of Springs in the vicinity of Crater Lake, Oregon in Relation to Air and Ground Temperatures


	ill.; Includes bibliographical references (leaves 6-8)
	Citation Citation Citation Abstract Copy Title: Temperatures of Springs in the vicinity of Crater Lake, Oregon in Relation to Air and Ground Temperatures Author: Nathenson, Manuel Year: 1990, 2008 ill.; Includes bibliographical references (leaves 6-8) Title: Temperatures of Springs in the vicinity of Crater Lake, Oregon in Relation to Air and Ground Temperatures Author: Nathenson, Manuel Year: 1990, 2008 ill.; Includes bibliographical references (leaves 6-8)

2. [Image] Steady-State and Transient Wellbore Temperatures during Drilling


	An extensive literature search was made to locate technical publications and computer programs relating to wellbore temperatures during drilling operations. The search confirmed the need for knowledge ...
	Citation Citation Citation Abstract Copy Title: Steady-State and Transient Wellbore Temperatures during Drilling Author: McDonald, W.J. Year: 1976 An extensive literature search was made to locate technical publications and computer programs relating to wellbore temperatures during drilling operations. The search confirmed the need for knowledge of transient and steady state circulating temperatures in the design of geothermal bits. Two approaches were used in calculating borehole temperatures. The steady state solution of Holmes and Swift was programmed and 2100 cases calculated for various borehole configurations. For transient temperature studies, calculations were made for ten borehole configurations. These calculations help emphasize the need for better high temperature bit performance and improved engineering procedures in drilling. The conclusions and recommendations are based on latest available technology for calculating wellbore temperatures Title: Steady-State and Transient Wellbore Temperatures during Drilling Author: McDonald, W.J. Year: 1976 An extensive literature search was made to locate technical publications and computer programs relating to wellbore temperatures during drilling operations. The search confirmed the need for knowledge of transient and steady state circulating temperatures in the design of geothermal bits. Two approaches were used in calculating borehole temperatures. The steady state solution of Holmes and Swift was programmed and 2100 cases calculated for various borehole configurations. For transient temperature studies, calculations were made for ten borehole configurations. These calculations help emphasize the need for better high temperature bit performance and improved engineering procedures in drilling. The conclusions and recommendations are based on latest available technology for calculating wellbore temperatures

3. [Image] Guidance for evaluating and recommending temperature regimes to protect fish


	Abstract. Procedures are presented for evaluating temperature regimes for fish. Although examples pertain to spring chinook salmon (Oncorhynchus tshawytscha), the principles apply to other species. Basic ...
	Citation Citation Citation Abstract Copy Title: Guidance for evaluating and recommending temperature regimes to protect fish Author: Armour, Carl L. Year: 1991, 2005 Abstract. Procedures are presented for evaluating temperature regimes for fish. Although examples pertain to spring chinook salmon (Oncorhynchus tshawytscha), the principles apply to other species. Basic temperature tolerance relationships for fish are explained and three options are described for comparing alternative temperature regimes. The options are to base comparisons on experimental temperature tolerance results, suitability of a simulated temperature regime for key life stages, or population statistics and predicted responses to simulated temperatures. Key words: Chinook salmon, water temperature, alternative temperature regimes. Title: Guidance for evaluating and recommending temperature regimes to protect fish Author: Armour, Carl L. Year: 1991, 2005 Abstract. Procedures are presented for evaluating temperature regimes for fish. Although examples pertain to spring chinook salmon (Oncorhynchus tshawytscha), the principles apply to other species. Basic temperature tolerance relationships for fish are explained and three options are described for comparing alternative temperature regimes. The options are to base comparisons on experimental temperature tolerance results, suitability of a simulated temperature regime for key life stages, or population statistics and predicted responses to simulated temperatures. Key words: Chinook salmon, water temperature, alternative temperature regimes.

4. [Image] Influences of human activity on stream temperatures and existence of cold-water fish in streams with elevated temperature: report of a workshop: Independent Multidisciplinary Science Team, Corvallis, OR, October 5-6, 2000


	Executive Summary The Independent Multidisciplinary Science Team (IMST) convened a panel of experts on stream temperature and fish ecology on October 5-6, 2000 for a scientific workshop on human influences ...
	Citation Citation Citation Abstract Copy Title: Influences of human activity on stream temperatures and existence of cold-water fish in streams with elevated temperature: report of a workshop: Independent Multidisciplinary Science Team, Corvallis, OR, October 5-6, 2000 Author: Independent Multidisciplinary Science Team (Oregon) Year: 2000, 2008, 2005 Executive Summary The Independent Multidisciplinary Science Team (IMST) convened a panel of experts on stream temperature and fish ecology on October 5-6, 2000 for a scientific workshop on human influences on stream temperature and responses by salmonids. The workshop was designed to review and discuss scientifically credible data and publications about 1) factors related to human activity that influence stream temperature and 2) behavioral, physical, and ecological mechanisms of cold water fish species for existing in streams with elevated temperatures. The goal of the workshop was to review empirical evidence and to identify points of agreement, disagreement, and knowledge gaps within the scientific community concerning the factors that influence stream temperature and fish responses to elevated temperatures. This information will assist the IMST in preparing a broader temperature report on Oregon's stream temperature water quality standards and their implementation. This report is prepared by the IMST. It was reviewed by workshop participants and revised by the IMST accordingly. The report includes abstracts of plenary presentations on factors that influence stream temperatures and fish responses, and the results of group discussions. The workshop participants focused on three main questions and were asked to list statements of agreement and disagreement, and to identify gaps in the scientific knowledge related to each question: ? How and where does riparian vegetation influence stream temperature? ? Do other changes in streams cause increases in stream temperature? ? How can apparently healthy fish populations exist in streams with temperatures higher than laboratory and field studies would indicate as healthy? The workshop participants provided answers to the questions in the form of bullets. The answers below represent the IMST's summation of the workshop findings and were reviewed by the participants. Several gaps in the scientific basis for specific questions or relationships were identified. The participants found no areas of disagreement for which technical information was available. They noted that any disagreements were not related to scientific interpretation, but were based on concerns or opinions about application, regulation, and management. How and where does riparian vegetation influence stream temperature? The influence of riparian vegetation on stream temperature is cumulative and complex, varying by site, over time, and across regions. Riparian vegetation can directly affect stream temperature by intercepting solar radiation and reducing stream heating. The influence of riparian shade in controlling temperature declines as streams widen in downstream reaches, but the role of riparian vegetation in providing water quality and fish habitat benefits continues to be important. Besides providing shade, riparian vegetation can also indirectly affect stream temperature by influencing microclimate, affecting channel morphology, affecting stream flow, influencing wind speed, affecting humidity, affecting soil temperature, using water, influencing air temperature, enhancing infiltration, and influencing thermal radiation. It is critical to know the site potential to understand what vegetation a site can support. There is not a good scientific understanding of how much vegetation shading is required to affect stream temperature. 1 This lack of understanding may be due to the spatial and temporal variability in landscape components, and the resulting variability in both the direct and indirect influences of vegetation on stream temperature. Therefore, it is difficult to generalize about the effects of vegetation on stream temperature. Do other changes in streams cause increases in stream temperature? The answer to this question is yes, other physical changes in the stream system can modify stream temperatures. Stream temperature is a product of complex interactions between geomorphology, soil, hydrology, vegetation, and climate within a watershed. Changes in these factors will result in changes in stream temperature. Human activities influence stream temperature by affecting one or more of four major components: riparian vegetation, channel morphology, hydrology, and surface/subsurface interactions. Stream systems vary substantially across the landscape, and site-specific information is critical to understanding stream temperature responses to human activities. How can apparently healthy fish populations exist in streams with temperatures higher than laboratory and field studies would indicate as healthy? Workshop participants identified several mechanisms that might explain the ability of fish populations to exist at higher than expected temperatures. The first mechanism was that the fish may have physiological adaptations to survive exposures to high temperatures. A second possibility was that stream habitats may contain cooler microhabitats that fish can occupy as refuge from higher temperatures. A third consideration is that ecological interactions may be different under differing thermal conditions resulting, for example, in changes in disease virulence or cumulative effects of stressors. Finally, since substantial differences exist between laboratory and field studies, it is difficult to apply results of laboratory studies to fish responses in the field. It is important to note that these proposed mechanisms are speculative and, as the list of gaps indicates, substantial experimental work is required to establish their influences on fish in different stream systems. Workshop Summaiy Workshop participants recognized gaps in the available science. Additional knowledge about human influences on stream temperatures and, consequently, influences on cold-water fish populations, will improve our ability to prevent further degradation of stream habitat and will enhance efforts geared towards the recovery of depressed fish populations. Even with these gaps, there was enough agreement on factors that influence stream temperature to indicate information is available to start developing and implementing management practices that are designed to reduce stream warming. It was suggested that managers should consider riparian vegetation, channel morphology, and hydrology, and should account for site differences. Title: Influences of human activity on stream temperatures and existence of cold-water fish in streams with elevated temperature: report of a workshop: Independent Multidisciplinary Science Team, Corvallis, OR, October 5-6, 2000 Author: Independent Multidisciplinary Science Team (Oregon) Year: 2000, 2008, 2005 Executive Summary The Independent Multidisciplinary Science Team (IMST) convened a panel of experts on stream temperature and fish ecology on October 5-6, 2000 for a scientific workshop on human influences on stream temperature and responses by salmonids. The workshop was designed to review and discuss scientifically credible data and publications about 1) factors related to human activity that influence stream temperature and 2) behavioral, physical, and ecological mechanisms of cold water fish species for existing in streams with elevated temperatures. The goal of the workshop was to review empirical evidence and to identify points of agreement, disagreement, and knowledge gaps within the scientific community concerning the factors that influence stream temperature and fish responses to elevated temperatures. This information will assist the IMST in preparing a broader temperature report on Oregon's stream temperature water quality standards and their implementation. This report is prepared by the IMST. It was reviewed by workshop participants and revised by the IMST accordingly. The report includes abstracts of plenary presentations on factors that influence stream temperatures and fish responses, and the results of group discussions. The workshop participants focused on three main questions and were asked to list statements of agreement and disagreement, and to identify gaps in the scientific knowledge related to each question: ? How and where does riparian vegetation influence stream temperature? ? Do other changes in streams cause increases in stream temperature? ? How can apparently healthy fish populations exist in streams with temperatures higher than laboratory and field studies would indicate as healthy? The workshop participants provided answers to the questions in the form of bullets. The answers below represent the IMST's summation of the workshop findings and were reviewed by the participants. Several gaps in the scientific basis for specific questions or relationships were identified. The participants found no areas of disagreement for which technical information was available. They noted that any disagreements were not related to scientific interpretation, but were based on concerns or opinions about application, regulation, and management. How and where does riparian vegetation influence stream temperature? The influence of riparian vegetation on stream temperature is cumulative and complex, varying by site, over time, and across regions. Riparian vegetation can directly affect stream temperature by intercepting solar radiation and reducing stream heating. The influence of riparian shade in controlling temperature declines as streams widen in downstream reaches, but the role of riparian vegetation in providing water quality and fish habitat benefits continues to be important. Besides providing shade, riparian vegetation can also indirectly affect stream temperature by influencing microclimate, affecting channel morphology, affecting stream flow, influencing wind speed, affecting humidity, affecting soil temperature, using water, influencing air temperature, enhancing infiltration, and influencing thermal radiation. It is critical to know the site potential to understand what vegetation a site can support. There is not a good scientific understanding of how much vegetation shading is required to affect stream temperature. 1 This lack of understanding may be due to the spatial and temporal variability in landscape components, and the resulting variability in both the direct and indirect influences of vegetation on stream temperature. Therefore, it is difficult to generalize about the effects of vegetation on stream temperature. Do other changes in streams cause increases in stream temperature? The answer to this question is yes, other physical changes in the stream system can modify stream temperatures. Stream temperature is a product of complex interactions between geomorphology, soil, hydrology, vegetation, and climate within a watershed. Changes in these factors will result in changes in stream temperature. Human activities influence stream temperature by affecting one or more of four major components: riparian vegetation, channel morphology, hydrology, and surface/subsurface interactions. Stream systems vary substantially across the landscape, and site-specific information is critical to understanding stream temperature responses to human activities. How can apparently healthy fish populations exist in streams with temperatures higher than laboratory and field studies would indicate as healthy? Workshop participants identified several mechanisms that might explain the ability of fish populations to exist at higher than expected temperatures. The first mechanism was that the fish may have physiological adaptations to survive exposures to high temperatures. A second possibility was that stream habitats may contain cooler microhabitats that fish can occupy as refuge from higher temperatures. A third consideration is that ecological interactions may be different under differing thermal conditions resulting, for example, in changes in disease virulence or cumulative effects of stressors. Finally, since substantial differences exist between laboratory and field studies, it is difficult to apply results of laboratory studies to fish responses in the field. It is important to note that these proposed mechanisms are speculative and, as the list of gaps indicates, substantial experimental work is required to establish their influences on fish in different stream systems. Workshop Summaiy Workshop participants recognized gaps in the available science. Additional knowledge about human influences on stream temperatures and, consequently, influences on cold-water fish populations, will improve our ability to prevent further degradation of stream habitat and will enhance efforts geared towards the recovery of depressed fish populations. Even with these gaps, there was enough agreement on factors that influence stream temperature to indicate information is available to start developing and implementing management practices that are designed to reduce stream warming. It was suggested that managers should consider riparian vegetation, channel morphology, and hydrology, and should account for site differences.

5. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maryland-District of Columbia


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maryland-District of Columbia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maryland-District of Columbia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

6. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Virginia-District of Columbia


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Virginia-District of Columbia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Virginia-District of Columbia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

7. [Image] Potential Uses for a High-Temperature Borehole Gravimeter


	It is possible to design a canister to cool a borehole gravimeter for use in geothermal and high-temperature (up to 350/sup 0/C) gas wells. Repeat surveys with such a gravimeter could (1) help estimate ...
	Citation Citation Citation Abstract Copy Title: Potential Uses for a High-Temperature Borehole Gravimeter Author: Hearst, J.R. Year: 1978 It is possible to design a canister to cool a borehole gravimeter for use in geothermal and high-temperature (up to 350/sup 0/C) gas wells. Repeat surveys with such a gravimeter could (1) help estimate the extent of reservoir plugging in geothermal injection well after one year of operation and (2) detect compaction of a geothermal aquifer if the change in thickness of the aquifer exceeds 1 m. The instrument could be used together with conventional logging tools to evaluate radial dependence of density around a well, or to estimate gas-filled porosity around wells drilled with mud. A high-temperature borehole gravimeter could also be used to evaluate structure and stratigraphy around geothermal and high-temperature gas wells Title: Potential Uses for a High-Temperature Borehole Gravimeter Author: Hearst, J.R. Year: 1978 It is possible to design a canister to cool a borehole gravimeter for use in geothermal and high-temperature (up to 350/sup 0/C) gas wells. Repeat surveys with such a gravimeter could (1) help estimate the extent of reservoir plugging in geothermal injection well after one year of operation and (2) detect compaction of a geothermal aquifer if the change in thickness of the aquifer exceeds 1 m. The instrument could be used together with conventional logging tools to evaluate radial dependence of density around a well, or to estimate gas-filled porosity around wells drilled with mud. A high-temperature borehole gravimeter could also be used to evaluate structure and stratigraphy around geothermal and high-temperature gas wells

8. [Image] Fluid-Temperature Logs for Selected Wells in Eastern Washington


	This Open-File Report consists of fluid temperature logs compiled during studies of the geohydrology and low temperature geothermal resources of eastern Washington. The fluid temperature logs are divided ...
	Citation Citation Citation Abstract Copy Title: Fluid-Temperature Logs for Selected Wells in Eastern Washington Author: Stoffel, K. L. Year: 1983 This Open-File Report consists of fluid temperature logs compiled during studies of the geohydrology and low temperature geothermal resources of eastern Washington. The fluid temperature logs are divided into two groups. Part A consists of wells which are concentrated in the Moses Lake-Ritzville-Connell area. Full geophysical log suites for many of these wells are presented in Stoffel and Widness (1983) and discussed in Widness (1983, 1984). Part B consists of wells outside of the Moses Lake-Ritzville-Connell study area Title: Fluid-Temperature Logs for Selected Wells in Eastern Washington Author: Stoffel, K. L. Year: 1983 This Open-File Report consists of fluid temperature logs compiled during studies of the geohydrology and low temperature geothermal resources of eastern Washington. The fluid temperature logs are divided into two groups. Part A consists of wells which are concentrated in the Moses Lake-Ritzville-Connell area. Full geophysical log suites for many of these wells are presented in Stoffel and Widness (1983) and discussed in Widness (1983, 1984). Part B consists of wells outside of the Moses Lake-Ritzville-Connell study area

9. [Image] Low Temperature Geothermal Resource Management


	Low temperature geothermal fluid is defined in OAR Chapter 690, Division 65 as any ground water used for its thermal characteristics that is encountered in a well with a bottom hole temperature less than ...
	Citation Citation Citation Abstract Copy Title: Low Temperature Geothermal Resource Management Author: Forcella, L. S. Year: 1984 Low temperature geothermal fluid is defined in OAR Chapter 690, Division 65 as any ground water used for its thermal characteristics that is encountered in a well with a bottom hole temperature less than 250°F (I 21°C). As such, low temperature geothermal resources are considered part of Oregon's ground water resources and are managed by the Oregon Water Resources Department (WRD). Use of ground water for its thermal properties is considered a beneficial use. With current interest in renewable resources and improved technology in heat extraction, the thermal value of ground water at all temperatures has increased dramatically adding to the complexity of ground water management Title: Low Temperature Geothermal Resource Management Author: Forcella, L. S. Year: 1984 Low temperature geothermal fluid is defined in OAR Chapter 690, Division 65 as any ground water used for its thermal characteristics that is encountered in a well with a bottom hole temperature less than 250°F (I 21°C). As such, low temperature geothermal resources are considered part of Oregon's ground water resources and are managed by the Oregon Water Resources Department (WRD). Use of ground water for its thermal properties is considered a beneficial use. With current interest in renewable resources and improved technology in heat extraction, the thermal value of ground water at all temperatures has increased dramatically adding to the complexity of ground water management

10. [Image] C. D. Hopkins, et al. , No. 2. Geothermal Well-Of-Opportunity, Wayne County, Georgia. Operational Report


	An oil and gas exploration well, located near Jesup in Wayne County, Georgia (lat. 31/sup 0/32' N, long. 81/sup 0/43' W), was deepened and used for geothermal temperature-gradient measurements. The well ...
	Citation Citation Citation Abstract Copy Title: C. D. Hopkins, et al. , No. 2. Geothermal Well-Of-Opportunity, Wayne County, Georgia. Operational Report Author: Lohse, A. Year: 1978 An oil and gas exploration well, located near Jesup in Wayne County, Georgia (lat. 31/sup 0/32' N, long. 81/sup 0/43' W), was deepened and used for geothermal temperature-gradient measurements. The well was drilled from 4,009 to 4,341 feet, then diamond cored to 4,371 feet, 28 feet of core being obtained for analysis. After logging by the U.S.G.S. District Groundwater Office in Atlanta, the well was terminated with 3/sup 1///sub 2/'' tubing to 4,386 feet. The bottom-hole temperature was determined to be 60/sup 0/C (140/sup 0/F) at 1,331 meters (4,365 feet). Over the interval 47 to 1,331 meters (154 to 4,365 feet) the least-squares temperature gradient was 29.3 +- 0.14 /sup 0/C/km (1.61 +- 0.25 /sup 0/F/100 ft) Title: C. D. Hopkins, et al. , No. 2. Geothermal Well-Of-Opportunity, Wayne County, Georgia. Operational Report Author: Lohse, A. Year: 1978 An oil and gas exploration well, located near Jesup in Wayne County, Georgia (lat. 31/sup 0/32' N, long. 81/sup 0/43' W), was deepened and used for geothermal temperature-gradient measurements. The well was drilled from 4,009 to 4,341 feet, then diamond cored to 4,371 feet, 28 feet of core being obtained for analysis. After logging by the U.S.G.S. District Groundwater Office in Atlanta, the well was terminated with 3/sup 1///sub 2/'' tubing to 4,386 feet. The bottom-hole temperature was determined to be 60/sup 0/C (140/sup 0/F) at 1,331 meters (4,365 feet). Over the interval 47 to 1,331 meters (154 to 4,365 feet) the least-squares temperature gradient was 29.3 +- 0.14 /sup 0/C/km (1.61 +- 0.25 /sup 0/F/100 ft)

11. [Image] Optimization of Residential Size Heat Pumps for Use With Geothermal Energy


	This paper considers the optimum design of unitary water-to-air heat pump units for use in distributed systems. The idea considers a heat pump unit with standard off-the-shelf components but optimized ...
	Citation Citation Citation Abstract Copy Title: Optimization of Residential Size Heat Pumps for Use With Geothermal Energy Author: Reistad, G. M. This paper considers the optimum design of unitary water-to-air heat pump units for use in distributed systems. The idea considers a heat pump unit with standard off-the-shelf components but optimized for heating when using a geothermal resource of a particular temperature and cost, as the low temperature energy source Title: Optimization of Residential Size Heat Pumps for Use With Geothermal Energy Author: Reistad, G. M. This paper considers the optimum design of unitary water-to-air heat pump units for use in distributed systems. The idea considers a heat pump unit with standard off-the-shelf components but optimized for heating when using a geothermal resource of a particular temperature and cost, as the low temperature energy source

12. [Image] Production of Ethanol for Automotive Fuel Employing Geothermal Energy


	This short report provides information on the process of producing ethanol for automotive fuel by employing geothermal energy. It also covers the feasibility of this kind of project
	Citation Citation Citation Abstract Copy Title: Production of Ethanol for Automotive Fuel Employing Geothermal Energy Author: Yu, J. This short report provides information on the process of producing ethanol for automotive fuel by employing geothermal energy. It also covers the feasibility of this kind of project Title: Production of Ethanol for Automotive Fuel Employing Geothermal Energy Author: Yu, J. This short report provides information on the process of producing ethanol for automotive fuel by employing geothermal energy. It also covers the feasibility of this kind of project

13. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arkansas


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arkansas Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arkansas Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

14. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alabama


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alabama Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alabama Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

15. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Connecticut


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Connecticut Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Connecticut Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

16. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Delaware


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Delaware Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Delaware Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

17. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Georgia


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Georgia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Georgia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

18. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Florida


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Florida Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Florida Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

19. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Illinois


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Illinois Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Illinois Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

20. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Indiana


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Indiana Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Indiana Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

21. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Iowa


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Iowa Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Iowa Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

22. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kansas


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kansas Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kansas Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

23. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kentucky


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kentucky Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kentucky Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

24. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Louisiana


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Louisiana Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Louisiana Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

25. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maine


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maine Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maine Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

26. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Massachusetts


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Massachusetts Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Massachusetts Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

27. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Michigan


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Michigan Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Michigan Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

28. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Minnesota


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Minnesota Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Minnesota Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

29. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Mississippi


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Mississippi Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Mississippi Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

30. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Missouri


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Missouri Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Missouri Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

31. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nebraska


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nebraska Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nebraska Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

32. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Hampshire


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Hampshire Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Hampshire Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

33. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Jersey


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Jersey Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Jersey Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

34. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New York


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New York Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New York Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

35. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Carolina


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Carolina Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Carolina Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

36. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Ohio


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Ohio Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Ohio Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

37. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oklahoma


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oklahoma Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oklahoma Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

38. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Pennsylvania


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Pennsylvania Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Pennsylvania Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

39. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Rhode Island


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Rhode Island Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Rhode Island Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

40. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Carolina


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Carolina Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Carolina Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

41. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Tennessee


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Tennessee Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Tennessee Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

42. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Texas


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Texas Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Texas Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

43. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Vermont


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Vermont Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Vermont Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

44. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 West Virginia


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 West Virginia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 West Virginia Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

45. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wisconsin


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wisconsin Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wisconsin Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

46. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alaska


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alaska Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alaska Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

47. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arizona


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arizona Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arizona Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

48. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 California


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 California Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 California Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

49. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Colorado


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Colorado Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Colorado Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

50. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Dakota


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Dakota Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Dakota Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

51. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Utah


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Utah Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Utah Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

52. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Washington


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Washington Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Washington Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

53. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Mexico


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Mexico Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Mexico Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

54. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oregon


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oregon Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oregon Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

55. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Hawaii


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Hawaii Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Hawaii Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

56. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Montana


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Montana Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Montana Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

57. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nevada


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nevada Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nevada Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

58. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wyoming


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wyoming Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wyoming Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

59. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Dakota


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Dakota Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Dakota Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

60. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Idaho


	The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in ...
	Citation Citation Citation Abstract Copy Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Idaho Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696 Title: Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Idaho Author: National Oceanic and Atmospheric Administration Year: 1982 The climatological normals presented in this publication are based on records for the 30-year period 1951-80, inclusive, Data are assembled by individual States. Data are presented in the order shown in the title. Units used in this publication are of for temperature and inches for precipitation. Heating and cooling degree day (base 65°F) normals are derived from the monthly normal temperatures using the technique developed by Thom (1), (2). Degree day normals also have been computed to other bases and may be obtained at cost from the National Climatic Center, Asheville, NC 28801-2696

61. [Image] The Cody Hydrothermal System


	The hot springs of Colter's Hell are the surface manifestations of a much larger hydrothermal system. That system has been studied to define its extent, maximum temperature, and mechanism of operation. ...
	Citation Citation Citation Abstract Copy Title: The Cody Hydrothermal System Author: Heasler, H.P. Year: 1982 The hot springs of Colter's Hell are the surface manifestations of a much larger hydrothermal system. That system has been studied to define its extent, maximum temperature, and mechanism of operation. The study area covers 2700 km/sup 2/ (1040 mi/sup 2/) in northwest Wyoming. Research and field work included locating and sampling the hot springs, geologic mapping, thermal logging of available wells, measuring thermal conductivities, analyzing over 200 oil and gas well bottom-hole temperatures, and compiling and analyzing hydrologic data. These data were used to generate a model for the hydrothermal system Title: The Cody Hydrothermal System Author: Heasler, H.P. Year: 1982 The hot springs of Colter's Hell are the surface manifestations of a much larger hydrothermal system. That system has been studied to define its extent, maximum temperature, and mechanism of operation. The study area covers 2700 km/sup 2/ (1040 mi/sup 2/) in northwest Wyoming. Research and field work included locating and sampling the hot springs, geologic mapping, thermal logging of available wells, measuring thermal conductivities, analyzing over 200 oil and gas well bottom-hole temperatures, and compiling and analyzing hydrologic data. These data were used to generate a model for the hydrothermal system

62. [Image] Interactive Fracture Design Model


	A computer program is described that can be used to design a fracture stimulation treatment for a geothermal reservoir. The program uses state-of-the-art methods to calculate the temperature of the fracture ...
	Citation Citation Citation Abstract Copy Title: Interactive Fracture Design Model Author: Petroleum Training and Technical Services Year: 1980 A computer program is described that can be used to design a fracture stimulation treatment for a geothermal reservoir. The program uses state-of-the-art methods to calculate the temperature of the fracture fluid as a function of time and distance in the fracture. This information is used to determine the temperature dependent properties of the fracture fluid. These fluid properties are utilized to calculate the fracture geometry as a function of time. The fracture geometry and temperature distribution of the fracture fluid are coupled so the subroutines that calculate these distributions have been made interactive Title: Interactive Fracture Design Model Author: Petroleum Training and Technical Services Year: 1980 A computer program is described that can be used to design a fracture stimulation treatment for a geothermal reservoir. The program uses state-of-the-art methods to calculate the temperature of the fracture fluid as a function of time and distance in the fracture. This information is used to determine the temperature dependent properties of the fracture fluid. These fluid properties are utilized to calculate the fracture geometry as a function of time. The fracture geometry and temperature distribution of the fracture fluid are coupled so the subroutines that calculate these distributions have been made interactive

63. [Image] High Temperature Electronics and Instrumentation Seminar: December 3-4, 1979


	The purpose of this two day seminar is to review the state-of-the-art and the recent substantial progress in High Temperature Electronics and Instrumentation. This seminar comes at a critical time and ...
	Citation Citation Citation Abstract Copy Title: High Temperature Electronics and Instrumentation Seminar: December 3-4, 1979 Author: U.S. Department of Energy (USDOE) Year: 1979 The purpose of this two day seminar is to review the state-of-the-art and the recent substantial progress in High Temperature Electronics and Instrumentation. This seminar comes at a critical time and it addresses a vital subject. The frontiers of technology are rapidly moving beyond the conventional 125°C boundary. Already, special “hostile environment" instruments routinely operate up to 180 C1 , a few prototype systems have been field tested to 275°C, new development is underway for 300°C integrated circuits 3, and research continues on components up to 500°C Title: High Temperature Electronics and Instrumentation Seminar: December 3-4, 1979 Author: U.S. Department of Energy (USDOE) Year: 1979 The purpose of this two day seminar is to review the state-of-the-art and the recent substantial progress in High Temperature Electronics and Instrumentation. This seminar comes at a critical time and it addresses a vital subject. The frontiers of technology are rapidly moving beyond the conventional 125°C boundary. Already, special “hostile environment" instruments routinely operate up to 180 C1 , a few prototype systems have been field tested to 275°C, new development is underway for 300°C integrated circuits 3, and research continues on components up to 500°C

64. [Image] Chloride/Magnesium Ratio of Shallow Groundwaters as a Regional Geothermal Indicator in Hawaii


	This report discusses some of the problems in using the Si02-temperature criteria for shallow groundwater assessment and the applications of the Cl/Mg ratio. Also presented are those areas within the state ...
	Citation Citation Citation Abstract Copy Title: Chloride/Magnesium Ratio of Shallow Groundwaters as a Regional Geothermal Indicator in Hawaii Author: Cox, M. E. Year: 1979 This report discusses some of the problems in using the Si02-temperature criteria for shallow groundwater assessment and the applications of the Cl/Mg ratio. Also presented are those areas within the state that are considered to possess potential on the basis of their Cl/Mg ratio Title: Chloride/Magnesium Ratio of Shallow Groundwaters as a Regional Geothermal Indicator in Hawaii Author: Cox, M. E. Year: 1979 This report discusses some of the problems in using the Si02-temperature criteria for shallow groundwater assessment and the applications of the Cl/Mg ratio. Also presented are those areas within the state that are considered to possess potential on the basis of their Cl/Mg ratio

65. [Image] Neutron Formation Temperature Gauge and Neutron Activation Analysis Brine Flow Meter. Final Report, October 1, 1976--March 31, 1978


	Feasibility studies of nuclear techniques applicable to the determination of geothermal formation temperature and two-phase brine flow downhole have been performed. The formation temperature gauging technique ...
	Citation Citation Citation Abstract Copy Title: Neutron Formation Temperature Gauge and Neutron Activation Analysis Brine Flow Meter. Final Report, October 1, 1976--March 31, 1978 Author: Vagelatos, N. Year: 1978 Feasibility studies of nuclear techniques applicable to the determination of geothermal formation temperature and two-phase brine flow downhole have been performed. The formation temperature gauging technique involves injection of fast neutrons into the formation and analysis of the moderated slow neutron energy distribution by appropriately filtered neutron detectors. The scientific feasibility of the method has been demonstrated by analytical computational and experimental evaluation of the system response. A data analysis method has been developed to determine unambiguously the temperature, neutron absorption cross section and neutron moderating power of an arbitrary medium. The initial phase of a program to demonstrate the engineering feasibility of the technique has been performed. A sonde mockup was fabricated and measurements have been performed in a test stand designed to simulate a geothermal well. The results indicate that the formation temperature determined by this method is independent of differences between the temperature in the borehole fluid and the formation, borehole fluid density, and borehole fluid salinity. Estimates of performance specifications for a formation temperature sonde have been made on the basis of information obtained in this study and a conceptual design of a logging system has been developed. The technique for the determination of fluid flow in a well is based on neutron activation analysis of elements present in the brine. An analytical evaluation of the method has been performed. The results warrant further, experimental evaluation Title: Neutron Formation Temperature Gauge and Neutron Activation Analysis Brine Flow Meter. Final Report, October 1, 1976--March 31, 1978 Author: Vagelatos, N. Year: 1978 Feasibility studies of nuclear techniques applicable to the determination of geothermal formation temperature and two-phase brine flow downhole have been performed. The formation temperature gauging technique involves injection of fast neutrons into the formation and analysis of the moderated slow neutron energy distribution by appropriately filtered neutron detectors. The scientific feasibility of the method has been demonstrated by analytical computational and experimental evaluation of the system response. A data analysis method has been developed to determine unambiguously the temperature, neutron absorption cross section and neutron moderating power of an arbitrary medium. The initial phase of a program to demonstrate the engineering feasibility of the technique has been performed. A sonde mockup was fabricated and measurements have been performed in a test stand designed to simulate a geothermal well. The results indicate that the formation temperature determined by this method is independent of differences between the temperature in the borehole fluid and the formation, borehole fluid density, and borehole fluid salinity. Estimates of performance specifications for a formation temperature sonde have been made on the basis of information obtained in this study and a conceptual design of a logging system has been developed. The technique for the determination of fluid flow in a well is based on neutron activation analysis of elements present in the brine. An analytical evaluation of the method has been performed. The results warrant further, experimental evaluation

66. [Image] Assessment of geothermal resources of Caliente, Nevada


	An assessment of the geothermal resources of Caliente, Nevada was made to provide information on resource characteristics and to site 2 (two) 500 ft (152 m) test wells to confirm the resource. The strategy ...
	Citation Citation Citation Abstract Copy Title: Assessment of geothermal resources of Caliente, Nevada Author: Trexler, D.T. Year: 1980 An assessment of the geothermal resources of Caliente, Nevada was made to provide information on resource characteristics and to site 2 (two) 500 ft (152 m) test wells to confirm the resource. The strategy used in the resource assessment employed a logical sequence of work elements that included 1) baseline data collection, 2) field investigations, 3) laboratory analyses and 4) data interpretation and synthesis. Airphoto interpretation indicated that a series of normal faults produced a stepped arrangement in the canyon walls on the west side of Meadow Valley Wash north of downtown Caiente. This area coincides with the area of known geothermal occurrences. Temperature measurements in existing wells indicate a rapid cooling of the geothermal waters as they mix with cold groundwater flows in Meadow Valley Wash. Soil mercury analyses range from 15 ppB to as high as 120 ppB. Trends in soil mercury content may indicate the presence of buried faults. Temperature measured in 2-meter deep auger holes indicated temperatures as high as 40/sup 0/C in an area north of the Lincoln County Medical Facility. Interpretation of chemical analyses, both major and minor, of waters collected from wells and streams in the area failed to conclusively show any mechanisms for the mixing of thermal and nonthermal waters. The selection of sites for the 2 (two) 500 ft (152 m) reservoir confirmation wells was made using the results of temperature surveys, geologic structure and historic observations; DOE/NV/10039-1 Title: Assessment of geothermal resources of Caliente, Nevada Author: Trexler, D.T. Year: 1980 An assessment of the geothermal resources of Caliente, Nevada was made to provide information on resource characteristics and to site 2 (two) 500 ft (152 m) test wells to confirm the resource. The strategy used in the resource assessment employed a logical sequence of work elements that included 1) baseline data collection, 2) field investigations, 3) laboratory analyses and 4) data interpretation and synthesis. Airphoto interpretation indicated that a series of normal faults produced a stepped arrangement in the canyon walls on the west side of Meadow Valley Wash north of downtown Caiente. This area coincides with the area of known geothermal occurrences. Temperature measurements in existing wells indicate a rapid cooling of the geothermal waters as they mix with cold groundwater flows in Meadow Valley Wash. Soil mercury analyses range from 15 ppB to as high as 120 ppB. Trends in soil mercury content may indicate the presence of buried faults. Temperature measured in 2-meter deep auger holes indicated temperatures as high as 40/sup 0/C in an area north of the Lincoln County Medical Facility. Interpretation of chemical analyses, both major and minor, of waters collected from wells and streams in the area failed to conclusively show any mechanisms for the mixing of thermal and nonthermal waters. The selection of sites for the 2 (two) 500 ft (152 m) reservoir confirmation wells was made using the results of temperature surveys, geologic structure and historic observations; DOE/NV/10039-1

67. [Image] Geochemistry of the Colado geothermal area, Pershing County, Nevada


	Multielement geochemical analysis of drill cuttings from 18 shallow and 2 intermediate-depth temperature gradient holes outlines an area of anomalous geochemistry related to the fluid flow and temperature ...
	Citation Citation Citation Abstract Copy Title: Geochemistry of the Colado geothermal area, Pershing County, Nevada Author: Christensen, O.D. Year: 1980 Multielement geochemical analysis of drill cuttings from 18 shallow and 2 intermediate-depth temperature gradient holes outlines an area of anomalous geochemistry related to the fluid flow and temperature distribution within the Colado geothermal area. The concentrations of Hg, As, Li, and Be belong to more than one statistical population and provide the clearest expression of hydrothermal processes. Enrichments of these four elements define anomalous zones which are spatially coincident with a measured temperature anomaly. The spatial distribution suggests that thermal fluid rises into alluvium in the vicinity of a major Basin and Range fault to depths of 200 to 400 feet (60 to 120 m), then flows laterally within shallow alluvial aquifers down the local hydrologic gradient. As the fluid cools, Li, Be, As, and Hg are deposited in response to changing physical and chemical conditions. As and Be appear to be deposited early in higher temperature zones; Li begins to deposit early but forms a rather dispersed geochemical anomaly; Hg is anomalous throughout the entire geothermal area but is concentrated in a shallow halo above the As and Be anomalies. The distributions suggest that the entry of thermal fluids from depth into the alluvium is spatially restricted to a small area and that the larger area of the observed thermal anomaly is due to the flow of warm fluid within shallow aquifers; DOE/ID/12079-9; ESL-39 Title: Geochemistry of the Colado geothermal area, Pershing County, Nevada Author: Christensen, O.D. Year: 1980 Multielement geochemical analysis of drill cuttings from 18 shallow and 2 intermediate-depth temperature gradient holes outlines an area of anomalous geochemistry related to the fluid flow and temperature distribution within the Colado geothermal area. The concentrations of Hg, As, Li, and Be belong to more than one statistical population and provide the clearest expression of hydrothermal processes. Enrichments of these four elements define anomalous zones which are spatially coincident with a measured temperature anomaly. The spatial distribution suggests that thermal fluid rises into alluvium in the vicinity of a major Basin and Range fault to depths of 200 to 400 feet (60 to 120 m), then flows laterally within shallow alluvial aquifers down the local hydrologic gradient. As the fluid cools, Li, Be, As, and Hg are deposited in response to changing physical and chemical conditions. As and Be appear to be deposited early in higher temperature zones; Li begins to deposit early but forms a rather dispersed geochemical anomaly; Hg is anomalous throughout the entire geothermal area but is concentrated in a shallow halo above the As and Be anomalies. The distributions suggest that the entry of thermal fluids from depth into the alluvium is spatially restricted to a small area and that the larger area of the observed thermal anomaly is due to the flow of warm fluid within shallow aquifers; DOE/ID/12079-9; ESL-39

68. [Image] Static Downhole Characteristics of Well CGEH-1 at Coso Hot Springs, China Lake, California


	A series of measurements was made in the exploratory well CGEH-1 at Coso Hot Springs. The temperature measurements provide estimates for the thermal equilibration of the well and indicate that the fractures ...
	Citation Citation Citation Abstract Copy Title: Static Downhole Characteristics of Well CGEH-1 at Coso Hot Springs, China Lake, California Author: Goranson, C. Year: 1978 A series of measurements was made in the exploratory well CGEH-1 at Coso Hot Springs. The temperature measurements provide estimates for the thermal equilibration of the well and indicate that the fractures intersecting the well have different temperatures. The hottest fractures are in the upper-cased portion of the well. Downhole chemical sampling suggests that the borehole still contains remnants of drilling materials. The well has never been extensively flowed at this time Title: Static Downhole Characteristics of Well CGEH-1 at Coso Hot Springs, China Lake, California Author: Goranson, C. Year: 1978 A series of measurements was made in the exploratory well CGEH-1 at Coso Hot Springs. The temperature measurements provide estimates for the thermal equilibration of the well and indicate that the fractures intersecting the well have different temperatures. The hottest fractures are in the upper-cased portion of the well. Downhole chemical sampling suggests that the borehole still contains remnants of drilling materials. The well has never been extensively flowed at this time

69. [Image] Formation Temperature Gauge Feasibility Study. Volume II, Interim Report


	The present status of the formation temperature gauge feasibility study is reported. It also demonstrates the feasibility of the technique in the simplified situations examined to date both analytically ...
	Citation Citation Citation Abstract Copy Title: Formation Temperature Gauge Feasibility Study. Volume II, Interim Report Author: IRT Corporation Year: 1977 The present status of the formation temperature gauge feasibility study is reported. It also demonstrates the feasibility of the technique in the simplified situations examined to date both analytically and experimentally. The first section deals with the theory underlying the technique. The next three sections describe the temperature gauge, the simplified model calculations of the gauge response, and the preliminary experimental measurements performed to verify the results of the computational study. The final section describes the formation temperature test stand designed to demonstrate the feasibility of the technique in the geothermal well geometry. This test stand has been assembled and measurements of the gauge response will begin shortly. These are outlined at the end of this report Title: Formation Temperature Gauge Feasibility Study. Volume II, Interim Report Author: IRT Corporation Year: 1977 The present status of the formation temperature gauge feasibility study is reported. It also demonstrates the feasibility of the technique in the simplified situations examined to date both analytically and experimentally. The first section deals with the theory underlying the technique. The next three sections describe the temperature gauge, the simplified model calculations of the gauge response, and the preliminary experimental measurements performed to verify the results of the computational study. The final section describes the formation temperature test stand designed to demonstrate the feasibility of the technique in the geothermal well geometry. This test stand has been assembled and measurements of the gauge response will begin shortly. These are outlined at the end of this report

70. [Image] Water quality monitoring : technical guide book


	"July 1999."
	Citation Citation Citation Abstract Copy Title: Water quality monitoring : technical guide book Author: Oregon. Governor's Watershed Enhancement Board Year: 1999, 2005, 2004 "July 1999." Title: Water quality monitoring : technical guide book Author: Oregon. Governor's Watershed Enhancement Board Year: 1999, 2005, 2004 "July 1999."

71. [Image] Diesel Heat Pump for District Heating Plants and for the Heating of Large Housing Blocks


	The aim of this project is to investigate technical, economic, and environmental aspects of large diesel driven heat pump plants for district heating and for central heating of large buildings
	Citation Citation Citation Abstract Copy Title: Diesel Heat Pump for District Heating Plants and for the Heating of Large Housing Blocks Author: Petersen, B. Year: 1980 The aim of this project is to investigate technical, economic, and environmental aspects of large diesel driven heat pump plants for district heating and for central heating of large buildings Title: Diesel Heat Pump for District Heating Plants and for the Heating of Large Housing Blocks Author: Petersen, B. Year: 1980 The aim of this project is to investigate technical, economic, and environmental aspects of large diesel driven heat pump plants for district heating and for central heating of large buildings

72. [Image] Low-Temperature Geothermal Potential of the Ojo Caliente Warm Springs Area, Northern New Mexico


	A detailed geochemical investigation of 17 waters (thermal and cold, mineralized and dilute) was performed in the Ojo Caliente-La Madera area. Two types of thermomineral waters have separate and distinctive ...
	Citation Citation Citation Abstract Copy Title: Low-Temperature Geothermal Potential of the Ojo Caliente Warm Springs Area, Northern New Mexico Author: Vuataz, F.D. Year: 1984 A detailed geochemical investigation of 17 waters (thermal and cold, mineralized and dilute) was performed in the Ojo Caliente-La Madera area. Two types of thermomineral waters have separate and distinctive geologic, geochemical, and geothermal characteristics. The water from Ojo Caliente Resort emerges with temperatures less than or equal to 54/sup 0/C from a Precambrian metarhyolite. Its chemistry, typically Na-HCO/sub 3/, has a total mineralization of 3600 mg/l. Isotopic studies have shown that the thermal water emerges from the springs and a hot well without significant mixing with the cold shallow aquifer of the valley alluvium. However, the cold aquifer adjacent to the resort does contain varying amounts of thermal water that originates from the warm spring system. Geothermometry calculations indicate that the thermal water may be as hot as 85/sup 0/C at depth before its ascent toward surface. Thermodynamic computations on the reaction states of numerous mineral phases suggest that the thermal water will not cause major scaling problems if the hot water is utilized for direct-use geothermal applications. By means of a network of very shallow holes, temperature and electrical conductivity anomalies have been found elsewhere in the valley around Ojo Caliente, and resistivity soundings have confirmed the presence of a plume of thermal water entering the shallow aquifer. The group of lukewarm springs around La Madera, with temperatures less than or equal to 29/sup 0/C, chemical type of NaCaMg-HCO/sub 3/Cl and with a total mineralization less than or equal to 1500 mg/l behaves as a different system without any Apparent relation to the Ojo Caliente system. Its temperature at depth is not believed to exceed 35 to 40/sup 0/C Title: Low-Temperature Geothermal Potential of the Ojo Caliente Warm Springs Area, Northern New Mexico Author: Vuataz, F.D. Year: 1984 A detailed geochemical investigation of 17 waters (thermal and cold, mineralized and dilute) was performed in the Ojo Caliente-La Madera area. Two types of thermomineral waters have separate and distinctive geologic, geochemical, and geothermal characteristics. The water from Ojo Caliente Resort emerges with temperatures less than or equal to 54/sup 0/C from a Precambrian metarhyolite. Its chemistry, typically Na-HCO/sub 3/, has a total mineralization of 3600 mg/l. Isotopic studies have shown that the thermal water emerges from the springs and a hot well without significant mixing with the cold shallow aquifer of the valley alluvium. However, the cold aquifer adjacent to the resort does contain varying amounts of thermal water that originates from the warm spring system. Geothermometry calculations indicate that the thermal water may be as hot as 85/sup 0/C at depth before its ascent toward surface. Thermodynamic computations on the reaction states of numerous mineral phases suggest that the thermal water will not cause major scaling problems if the hot water is utilized for direct-use geothermal applications. By means of a network of very shallow holes, temperature and electrical conductivity anomalies have been found elsewhere in the valley around Ojo Caliente, and resistivity soundings have confirmed the presence of a plume of thermal water entering the shallow aquifer. The group of lukewarm springs around La Madera, with temperatures less than or equal to 29/sup 0/C, chemical type of NaCaMg-HCO/sub 3/Cl and with a total mineralization less than or equal to 1500 mg/l behaves as a different system without any Apparent relation to the Ojo Caliente system. Its temperature at depth is not believed to exceed 35 to 40/sup 0/C

73. [Image] Low Temperature Geothermal Assessment of the Jordan Valley: Salt Lake County, Utah


	The Utah Geological and Mineral Survey (UGMS) has been conducting research to identify low-temperature geothermal resources in Utah as per U.S. Department of Energy (DOE) Contract OE-AS07-77ET28393. This ...
	Citation Citation Citation Abstract Copy Title: Low Temperature Geothermal Assessment of the Jordan Valley: Salt Lake County, Utah Author: Klauk, R.H. Year: 1984 The Utah Geological and Mineral Survey (UGMS) has been conducting research to identify low-temperature geothermal resources in Utah as per U.S. Department of Energy (DOE) Contract OE-AS07-77ET28393. This report, which is part of an area-wide geothermal research program along the Wasatch Front, is the culmination of the study conducted in the Jordan Valley, Salt Lake County, Utah Title: Low Temperature Geothermal Assessment of the Jordan Valley: Salt Lake County, Utah Author: Klauk, R.H. Year: 1984 The Utah Geological and Mineral Survey (UGMS) has been conducting research to identify low-temperature geothermal resources in Utah as per U.S. Department of Energy (DOE) Contract OE-AS07-77ET28393. This report, which is part of an area-wide geothermal research program along the Wasatch Front, is the culmination of the study conducted in the Jordan Valley, Salt Lake County, Utah

74. [Image] Drilling fluid/formation interaction at simulated in situ geothermal conditions. Final report


	Interaction of drilling fluids with a geothermal reservoir formation can result in significant permeability impairment and therefore reduced well productivity. This interaction is studied under simulated ...
	Citation Citation Citation Abstract Copy Title: Drilling fluid/formation interaction at simulated in situ geothermal conditions. Final report Author: Enniss, D.O Year: 1980 Interaction of drilling fluids with a geothermal reservoir formation can result in significant permeability impairment and therefore reduced well productivity. This interaction is studied under simulated in situ geothermal conditions of overburden stress, pore fluid pressure, temperature, and pore fluid chemistry. Permeability impairment of an East Mesa KGRA reservoir material is evaluated as a function of stagnation time, drilling fluid, and temperature. Results indicate that all of these parameters contribute significantly to the magnitude and the reversibility of the impairment. Title: Drilling fluid/formation interaction at simulated in situ geothermal conditions. Final report Author: Enniss, D.O Year: 1980 Interaction of drilling fluids with a geothermal reservoir formation can result in significant permeability impairment and therefore reduced well productivity. This interaction is studied under simulated in situ geothermal conditions of overburden stress, pore fluid pressure, temperature, and pore fluid chemistry. Permeability impairment of an East Mesa KGRA reservoir material is evaluated as a function of stagnation time, drilling fluid, and temperature. Results indicate that all of these parameters contribute significantly to the magnitude and the reversibility of the impairment.

75. [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 Citation Abstract Copy 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) 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)

76. [Image] Geothermal District Heating Projects


	The geothermal energy stored within the interior of the earth amounts to a significant quantity which, if fully exploited, could supply the energy needs of man for a millennia. Low temperature hydrothermal ...
	Citation Citation Citation Abstract Copy Title: Geothermal District Heating Projects Author: Lineau, P. J. The geothermal energy stored within the interior of the earth amounts to a significant quantity which, if fully exploited, could supply the energy needs of man for a millennia. Low temperature hydrothermal resources underlie vast areas of the United States as illustrated on Figure 1, particularly in the western half of the country. The U.S. Geological Survey has identified 1,346 hydrothermal convection systems of which 1,294 have temperatures less than 300°F and are considered suitable for direct heat applications (Reed, '1983). Resource temperatures greater than 300°F are considered economic for electrical generation. Quantitative estimates of identified low and intermediate temperature (less than 300°F) geothermal systems contain 68.3 million billion Btu's of beneficial heat for 30 years Title: Geothermal District Heating Projects Author: Lineau, P. J. The geothermal energy stored within the interior of the earth amounts to a significant quantity which, if fully exploited, could supply the energy needs of man for a millennia. Low temperature hydrothermal resources underlie vast areas of the United States as illustrated on Figure 1, particularly in the western half of the country. The U.S. Geological Survey has identified 1,346 hydrothermal convection systems of which 1,294 have temperatures less than 300°F and are considered suitable for direct heat applications (Reed, '1983). Resource temperatures greater than 300°F are considered economic for electrical generation. Quantitative estimates of identified low and intermediate temperature (less than 300°F) geothermal systems contain 68.3 million billion Btu's of beneficial heat for 30 years

77. [Image] Idaho Geothermal Commercialization Planning, Semi-Annual Progress Report, January 1, 1979 - June 30, 1979


	This report is a summary of the task accomplished during the first six months of the cooperative agreement between the U.S. Department of Energy and the Idaho Office of Energy. The report concentrates ...
	Citation Citation Citation Abstract Copy Title: Idaho Geothermal Commercialization Planning, Semi-Annual Progress Report, January 1, 1979 - June 30, 1979 Author: McClain, D.W. Year: 1979 This report is a summary of the task accomplished during the first six months of the cooperative agreement between the U.S. Department of Energy and the Idaho Office of Energy. The report concentrates on geothermal resource data, regional and local development plans, energy, and economic factors and institutional factors Title: Idaho Geothermal Commercialization Planning, Semi-Annual Progress Report, January 1, 1979 - June 30, 1979 Author: McClain, D.W. Year: 1979 This report is a summary of the task accomplished during the first six months of the cooperative agreement between the U.S. Department of Energy and the Idaho Office of Energy. The report concentrates on geothermal resource data, regional and local development plans, energy, and economic factors and institutional factors

78. [Image] Geotechnical Studies of Geothermal Reservoirs


	Maximum temperatures found in the reservoir were approximately 700°F in the Imperial Valley, California, but drill bit temperatures may be considerably higher in the Geysers geothermal area. Temperatures ...
	Citation Citation Citation Abstract Copy Title: Geotechnical Studies of Geothermal Reservoirs Author: Pratt, H. R. Year: 1976 Maximum temperatures found in the reservoir were approximately 700°F in the Imperial Valley, California, but drill bit temperatures may be considerably higher in the Geysers geothermal area. Temperatures reached up to 900°F because of frictional heating and possibly inefficient cooling. Rock types found in the high temperature environments range from hard abrasive granites and metamorphosed sandstones to unconsolidated sediments and friable sandstones. The rocks are highly fractured at reservoir depths Title: Geotechnical Studies of Geothermal Reservoirs Author: Pratt, H. R. Year: 1976 Maximum temperatures found in the reservoir were approximately 700°F in the Imperial Valley, California, but drill bit temperatures may be considerably higher in the Geysers geothermal area. Temperatures reached up to 900°F because of frictional heating and possibly inefficient cooling. Rock types found in the high temperature environments range from hard abrasive granites and metamorphosed sandstones to unconsolidated sediments and friable sandstones. The rocks are highly fractured at reservoir depths

79. [Image] September 2002 Klamath River fish-kill : final analysis of contributing factors and impacts


	"July 2004"
	Citation Citation Citation Abstract Copy Title: September 2002 Klamath River fish-kill : final analysis of contributing factors and impacts Author: California. Dept. of Fish and Game Year: 2004, 2005 "July 2004" Title: September 2002 Klamath River fish-kill : final analysis of contributing factors and impacts Author: California. Dept. of Fish and Game Year: 2004, 2005 "July 2004"

80. [Image] Ground-Source Heat Pump System near Helena, Montana: Loop Temperature Analysis


	This document looks closely into many aspects of a specific Heat Pump in Montana that is being used to heat a house
	Citation Citation Citation Abstract Copy Title: Ground-Source Heat Pump System near Helena, Montana: Loop Temperature Analysis Author: Van Voast, W. Year: 1996 This document looks closely into many aspects of a specific Heat Pump in Montana that is being used to heat a house Title: Ground-Source Heat Pump System near Helena, Montana: Loop Temperature Analysis Author: Van Voast, W. Year: 1996 This document looks closely into many aspects of a specific Heat Pump in Montana that is being used to heat a house

81. [Image] California Laws for Conservation of Geothermal Resources


	California laws for the conservation of geothermal resources. This covers rules for drilling geothermal wells
	Citation Citation Citation Abstract Copy Title: California Laws for Conservation of Geothermal Resources Author: State of California Year: 1978 California laws for the conservation of geothermal resources. This covers rules for drilling geothermal wells Title: California Laws for Conservation of Geothermal Resources Author: State of California Year: 1978 California laws for the conservation of geothermal resources. This covers rules for drilling geothermal wells

82. [Image] California Laws for Conservation of Geothermal Resources, January 1989


	California laws for the conservation of geothermal resources. This covers rules for drilling geothermal wells
	Citation Citation Citation Abstract Copy Title: California Laws for Conservation of Geothermal Resources, January 1989 Author: State of California Year: 1989 California laws for the conservation of geothermal resources. This covers rules for drilling geothermal wells Title: California Laws for Conservation of Geothermal Resources, January 1989 Author: State of California Year: 1989 California laws for the conservation of geothermal resources. This covers rules for drilling geothermal wells

83. [Image] Seal/lubricant systems for geothermal drilling equipment


	The development and testing of seals and lubricants for journal-type roller-cone rock bits for drilling into geothermal reservoirs at temperatures over 260/sup 0/C (500/sup 0/F) are described. The conditions ...
	Citation Citation Citation Abstract Copy Title: Seal/lubricant systems for geothermal drilling equipment Author: Hendrickson, R.R. Year: 1980 The development and testing of seals and lubricants for journal-type roller-cone rock bits for drilling into geothermal reservoirs at temperatures over 260/sup 0/C (500/sup 0/F) are described. The conditions experienced by seals and lubricants subjected to geothermal drilling are reviewed along with the basic design requirements for roller-cone bit seals and journal bearing lubricants. Two unique test facilities are described: a seal test machine which simulates pressures, temperatures, and mechanical eccentricities, and a lubricant tester capable of evaluating load-bearing ability at temperature and pressure. Three candidate elastomeric compounds demonstrated 288/sup 0/C (550/sup 0/F) capability and several others demonstrated 260/sup 0/C (500/sup 0/F) or greater capability. Successful elastomeric seal candidates were proprietary compounds based on EPDM, Kalrez, and/or Viton polymers. Three mechanical seals for reservoir temperatures over 288/sup 0/C (550/sup 0/F) are presented. Lubricant screening tests on more than 50 products are summarized, and several newly developed lubricants which meet both the compatibility and lubrication requirements are described. Several seal/lubricant systems are recommended for laboratory or field geothermal drilling tests in roller-cone drill bits. The future availability of drill bits for geothermal use is discussed, as well as the potential spinoffs of the program findings for nongeothermal roller-cone bits; SAND-80-7101 Title: Seal/lubricant systems for geothermal drilling equipment Author: Hendrickson, R.R. Year: 1980 The development and testing of seals and lubricants for journal-type roller-cone rock bits for drilling into geothermal reservoirs at temperatures over 260/sup 0/C (500/sup 0/F) are described. The conditions experienced by seals and lubricants subjected to geothermal drilling are reviewed along with the basic design requirements for roller-cone bit seals and journal bearing lubricants. Two unique test facilities are described: a seal test machine which simulates pressures, temperatures, and mechanical eccentricities, and a lubricant tester capable of evaluating load-bearing ability at temperature and pressure. Three candidate elastomeric compounds demonstrated 288/sup 0/C (550/sup 0/F) capability and several others demonstrated 260/sup 0/C (500/sup 0/F) or greater capability. Successful elastomeric seal candidates were proprietary compounds based on EPDM, Kalrez, and/or Viton polymers. Three mechanical seals for reservoir temperatures over 288/sup 0/C (550/sup 0/F) are presented. Lubricant screening tests on more than 50 products are summarized, and several newly developed lubricants which meet both the compatibility and lubrication requirements are described. Several seal/lubricant systems are recommended for laboratory or field geothermal drilling tests in roller-cone drill bits. The future availability of drill bits for geothermal use is discussed, as well as the potential spinoffs of the program findings for nongeothermal roller-cone bits; SAND-80-7101

84. [Image] A Geological and Geophysical Study of the Geothermal Energy Potential of Pilgrim Springs, Alaska


	The Pilgrim Springs geothermal area, located about 75 km north of Nome, was the subject of an intensive, reconnaissance-level geophysical and geological study during a 90-day period in the summer of 1979. ...
	Citation Citation Citation Abstract Copy Title: A Geological and Geophysical Study of the Geothermal Energy Potential of Pilgrim Springs, Alaska Author: Turner, Donald L. [ed.] Year: 1980 The Pilgrim Springs geothermal area, located about 75 km north of Nome, was the subject of an intensive, reconnaissance-level geophysical and geological study during a 90-day period in the summer of 1979. The thermal springs are located in a northeast-oriented, oval area of thawed ground approximately 1.5 km{sup 2} in size, bordered on the north by the Pilgrim River. A second, much smaller, thermal anomaly was discovered about 3 km northeast of the main thawed area. Continuous permafrost in the surrounding region is on the order of 100 m thick. Present surface thermal spring discharge is {approx} 4.2 x 10{sup -3} m{sup 3} s{sup -1} (67 gallons/minute) of alkali-chloride-type water at a temperature of 81 C. The reason for its high salinity is not yet understood because of conflicting evidence for seawater vs. other possible water sources. Preliminary Na-K-Ca geothermometry suggests deep reservoir temperatures approaching 150 C, but interpretation of these results is difficult because of their dependence on an unknown water mixing history. Based on these estimates, and present surface and drill hole water temperatures, Pilgrim Springs would be classified as an intermediate-temperature, liquid-dominated geothermal system; UAG-R-271 Title: A Geological and Geophysical Study of the Geothermal Energy Potential of Pilgrim Springs, Alaska Author: Turner, Donald L. [ed.] Year: 1980 The Pilgrim Springs geothermal area, located about 75 km north of Nome, was the subject of an intensive, reconnaissance-level geophysical and geological study during a 90-day period in the summer of 1979. The thermal springs are located in a northeast-oriented, oval area of thawed ground approximately 1.5 km{sup 2} in size, bordered on the north by the Pilgrim River. A second, much smaller, thermal anomaly was discovered about 3 km northeast of the main thawed area. Continuous permafrost in the surrounding region is on the order of 100 m thick. Present surface thermal spring discharge is {approx} 4.2 x 10{sup -3} m{sup 3} s{sup -1} (67 gallons/minute) of alkali-chloride-type water at a temperature of 81 C. The reason for its high salinity is not yet understood because of conflicting evidence for seawater vs. other possible water sources. Preliminary Na-K-Ca geothermometry suggests deep reservoir temperatures approaching 150 C, but interpretation of these results is difficult because of their dependence on an unknown water mixing history. Based on these estimates, and present surface and drill hole water temperatures, Pilgrim Springs would be classified as an intermediate-temperature, liquid-dominated geothermal system; UAG-R-271

85. [Image] A Computer Program for Determining the Thermodynamic Properties of Freon Refrigerants


	This program was written to be used as a subroutine. The program determines the thermodynamics of Freon refrigerants. The following refrigerants can be analyzed F-ll, F-12, F-13, F-14, F-21, F-22, F-23, ...
	Citation Citation Citation Abstract Copy Title: A Computer Program for Determining the Thermodynamic Properties of Freon Refrigerants Author: Riemer, D.H. Year: 1977 This program was written to be used as a subroutine. The program determines the thermodynamics of Freon refrigerants. The following refrigerants can be analyzed F-ll, F-12, F-13, F-14, F-21, F-22, F-23, F-113, and F-114. The subroutine can evaluate a thermodynamic state for these refrigerants given any of the following pairs of state quantities: pressure and quality, pressure and entropy, pressure and enthalpy, temperature and quality, temperature and specific volume and temperature and pressure. These six pairs of knowns allow the user to analyze any thermodynamic cycle utilizing a refrigerant as the working fluid. The Downing form of the Martin equation of state was used. This report contains a brief description, flow chart and listing of all subroutines required Title: A Computer Program for Determining the Thermodynamic Properties of Freon Refrigerants Author: Riemer, D.H. Year: 1977 This program was written to be used as a subroutine. The program determines the thermodynamics of Freon refrigerants. The following refrigerants can be analyzed F-ll, F-12, F-13, F-14, F-21, F-22, F-23, F-113, and F-114. The subroutine can evaluate a thermodynamic state for these refrigerants given any of the following pairs of state quantities: pressure and quality, pressure and entropy, pressure and enthalpy, temperature and quality, temperature and specific volume and temperature and pressure. These six pairs of knowns allow the user to analyze any thermodynamic cycle utilizing a refrigerant as the working fluid. The Downing form of the Martin equation of state was used. This report contains a brief description, flow chart and listing of all subroutines required

86. [Image] Thermal Drawdown and Recovery of Singly and Multiply Fractured Hot Dry Rock Reservoirs


	To calculate heat extraction and thermal recovery in hot dry rock geothermal reservoirs, a computer code was written to solve the differential equations for rock-water heat conduction and convection by ...
	Citation Citation Citation Abstract Copy Title: Thermal Drawdown and Recovery of Singly and Multiply Fractured Hot Dry Rock Reservoirs Author: Wunder, R. Year: 1978 To calculate heat extraction and thermal recovery in hot dry rock geothermal reservoirs, a computer code was written to solve the differential equations for rock-water heat conduction and convection by finite differences. Temperature versus time functions for multiple fractures separated by various spacings are presented in dimensional and in nondimensional plots. The results were specialized for the limiting case of a single fracture in unbounded rock and for the other limiting case where the rock is so extensively fractured that thermal breakthrough phenomena can occur. Fracture temperatures were calculated during the thermal recovery following various extraction periods. For the single-fracture case these temperature recoveries could, with slight approximation, be represented as a single curve depending only upon the ratio of the total elapsed time and the extraction time Title: Thermal Drawdown and Recovery of Singly and Multiply Fractured Hot Dry Rock Reservoirs Author: Wunder, R. Year: 1978 To calculate heat extraction and thermal recovery in hot dry rock geothermal reservoirs, a computer code was written to solve the differential equations for rock-water heat conduction and convection by finite differences. Temperature versus time functions for multiple fractures separated by various spacings are presented in dimensional and in nondimensional plots. The results were specialized for the limiting case of a single fracture in unbounded rock and for the other limiting case where the rock is so extensively fractured that thermal breakthrough phenomena can occur. Fracture temperatures were calculated during the thermal recovery following various extraction periods. For the single-fracture case these temperature recoveries could, with slight approximation, be represented as a single curve depending only upon the ratio of the total elapsed time and the extraction time

87. [Image] A Thermodynamic Model of the Hydrolysis of Microcline in Acid Sulfate Solutions


	A theoretical model of the hydrolysis of microcline by a hydrothermal solution has been determined for a closed system at constant temperature. Hypothetical solution compositions and temperatures were ...
	Citation Citation Citation Abstract Copy Title: A Thermodynamic Model of the Hydrolysis of Microcline in Acid Sulfate Solutions Author: Dedolph, R.E. Year: 1976 A theoretical model of the hydrolysis of microcline by a hydrothermal solution has been determined for a closed system at constant temperature. Hypothetical solution compositions and temperatures were chosen to match the known geothermal system at Roosevelt Hot Springs, Utah. The calculated reaction paths indicate that the overall reaction process is an exchange of potassium from the reactant mineral, microcline, for hydrogen from the solution. Aluminum is nearly conserved among solid phases. The amount of microcline reacted per kilogram of solution before overall equilibrium is reached is a function of temperature and initial solution pH. Since the system is closed and at constant temperature natural conditions are not reproduced well enough to apply the model as a geothermometer. The reaction paths suggest qualitative models of alteration mineral zoning patterns that are similar to zoning at Roosevelt Hot Springs, Utah; Steamboat Springs, Nevada, and Butte, Montana. The models presented view alteration zoning as a function of temperature and pH gradients within homogeneous host rocks where microcline and quartz are abundant Title: A Thermodynamic Model of the Hydrolysis of Microcline in Acid Sulfate Solutions Author: Dedolph, R.E. Year: 1976 A theoretical model of the hydrolysis of microcline by a hydrothermal solution has been determined for a closed system at constant temperature. Hypothetical solution compositions and temperatures were chosen to match the known geothermal system at Roosevelt Hot Springs, Utah. The calculated reaction paths indicate that the overall reaction process is an exchange of potassium from the reactant mineral, microcline, for hydrogen from the solution. Aluminum is nearly conserved among solid phases. The amount of microcline reacted per kilogram of solution before overall equilibrium is reached is a function of temperature and initial solution pH. Since the system is closed and at constant temperature natural conditions are not reproduced well enough to apply the model as a geothermometer. The reaction paths suggest qualitative models of alteration mineral zoning patterns that are similar to zoning at Roosevelt Hot Springs, Utah; Steamboat Springs, Nevada, and Butte, Montana. The models presented view alteration zoning as a function of temperature and pH gradients within homogeneous host rocks where microcline and quartz are abundant

88. [Image] Geological and Geophysical Analysis of Coso Geothermal Exploration Hole No. 1 (CGEH-1), Coso Hot Springs KGRA, California


	The Coso Geothermal Exploration Hole number one (CGEH-1) was drilled in the Coso Hot Springs KGRA, California from September 2 to December 2, 1977. Chip samples were collected at ten foot intervals and ...
	Citation Citation Citation Abstract Copy Title: Geological and Geophysical Analysis of Coso Geothermal Exploration Hole No. 1 (CGEH-1), Coso Hot Springs KGRA, California Author: Galbraith, R.M. Year: 1978 The Coso Geothermal Exploration Hole number one (CGEH-1) was drilled in the Coso Hot Springs KGRA, California from September 2 to December 2, 1977. Chip samples were collected at ten foot intervals and extensive geophysical logging surveys were conducted to document the geologic character of the geothermal system as penetrated by CGEH-1. The major rock units encountered include a mafic metamorphic sequence and a leucogranite which intruded the metamorphic rocks. Only weak hydrothermal alteration was noted in these rocks. Drillhole surveys and drilling rate data indicate that the geothermal system is structurally controlled and that the drillhole itself was strongly influenced by structural zones. Water chemistry indicates that this geothermal resource is a hot-water rather than a vapor-dominated system. Several geophysical logs were employed to characterize the drillhole geology. The natural gamma and neutron porosity logs indicate gross rock type and the acoustic logs indicate fractured rock and potentially permeable zones. A series of temperature logs run as a function of time during and after the completion of Drilling were most Useful in delineating the zones of maximum heat flux. Convective heat flow and temperatures greater than 350/sup 0/F appear to occur only along an open fracture system encountered between depths of 1850 and 2775 feet. Temperature logs indicate a negative thermal gradient below 3000 feet Title: Geological and Geophysical Analysis of Coso Geothermal Exploration Hole No. 1 (CGEH-1), Coso Hot Springs KGRA, California Author: Galbraith, R.M. Year: 1978 The Coso Geothermal Exploration Hole number one (CGEH-1) was drilled in the Coso Hot Springs KGRA, California from September 2 to December 2, 1977. Chip samples were collected at ten foot intervals and extensive geophysical logging surveys were conducted to document the geologic character of the geothermal system as penetrated by CGEH-1. The major rock units encountered include a mafic metamorphic sequence and a leucogranite which intruded the metamorphic rocks. Only weak hydrothermal alteration was noted in these rocks. Drillhole surveys and drilling rate data indicate that the geothermal system is structurally controlled and that the drillhole itself was strongly influenced by structural zones. Water chemistry indicates that this geothermal resource is a hot-water rather than a vapor-dominated system. Several geophysical logs were employed to characterize the drillhole geology. The natural gamma and neutron porosity logs indicate gross rock type and the acoustic logs indicate fractured rock and potentially permeable zones. A series of temperature logs run as a function of time during and after the completion of Drilling were most Useful in delineating the zones of maximum heat flux. Convective heat flow and temperatures greater than 350/sup 0/F appear to occur only along an open fracture system encountered between depths of 1850 and 2775 feet. Temperature logs indicate a negative thermal gradient below 3000 feet

89. [Image] Growth response of whitebark pine to climate in the Pacific Northwest


	ill.; Thesis (M.S.)--Saint Joseph's University, 2003; Includes bibliographical references (leaves 71-78)
	Citation Citation Citation Abstract Copy Title: Growth response of whitebark pine to climate in the Pacific Northwest Author: Daneshgar, Pedram Patrick Year: 2003, 2010 ill.; Thesis (M.S.)--Saint Joseph's University, 2003; Includes bibliographical references (leaves 71-78) Title: Growth response of whitebark pine to climate in the Pacific Northwest Author: Daneshgar, Pedram Patrick Year: 2003, 2010 ill.; Thesis (M.S.)--Saint Joseph's University, 2003; Includes bibliographical references (leaves 71-78)

90. [Image] Wet Geothermal Potential of the Kingman-Williams Region, Arizona


	The Kingman-Williams region, Arizona, possesses few thermal waters of deep origin. Evaluation of 33 waters (8 thermal) reveals that thermal waters are restricted to the Basin and Range tectonic province; ...
	Citation Citation Citation Abstract Copy Title: Wet Geothermal Potential of the Kingman-Williams Region, Arizona Author: Goff, F.E. Year: 1979 The Kingman-Williams region, Arizona, possesses few thermal waters of deep origin. Evaluation of 33 waters (8 thermal) reveals that thermal waters are restricted to the Basin and Range tectonic province; no thermal waters were found on the west margin of the Colorado Plateau. The thermal waters appear to rise along north-trending normal faults or flow in deep aquifers in Quaternary sedimentary basins of the Basin and Range province. All thermal waters have distinctive chemistry and discharge at temperatures ranjinj from 28-46°C. They Apparently issue from small isolated jeothermal reservoirs. Geothermometry and chemistry indicate that these are low-temperature reservoirs that probably do not exceed 115°C Title: Wet Geothermal Potential of the Kingman-Williams Region, Arizona Author: Goff, F.E. Year: 1979 The Kingman-Williams region, Arizona, possesses few thermal waters of deep origin. Evaluation of 33 waters (8 thermal) reveals that thermal waters are restricted to the Basin and Range tectonic province; no thermal waters were found on the west margin of the Colorado Plateau. The thermal waters appear to rise along north-trending normal faults or flow in deep aquifers in Quaternary sedimentary basins of the Basin and Range province. All thermal waters have distinctive chemistry and discharge at temperatures ranjinj from 28-46°C. They Apparently issue from small isolated jeothermal reservoirs. Geothermometry and chemistry indicate that these are low-temperature reservoirs that probably do not exceed 115°C

91. [Image] Klamath Christian Center Heating System


	On December 6, 1983, Dave South well contacted the Geo-Heat Center requesting information and possible assistance in analyzing problems with the geothermal wells and heating system. About a week later, ...
	Citation Citation Citation Abstract Copy Title: Klamath Christian Center Heating System Author: Culver, G. Year: 1984 On December 6, 1983, Dave South well contacted the Geo-Heat Center requesting information and possible assistance in analyzing problems with the geothermal wells and heating system. About a week later, Geo-Heat Center personnel met with Dave and discussed the meager amount of information then available. It was decided that the Geo-Heat Center would attempt to obtain more well data and, if possible, temperature profile the wells to determine what the problem was since available data indicated the wells should produce more heat than they were. At that time the down hole heat exchanger would provide only 116°F to 118°F water during colder periods and 125°F maximum during more moderate weather. The well was being pumped from 76 feet by a jet pump and producing about 25 gpm which was being discharged into the storm drain. Title: Klamath Christian Center Heating System Author: Culver, G. Year: 1984 On December 6, 1983, Dave South well contacted the Geo-Heat Center requesting information and possible assistance in analyzing problems with the geothermal wells and heating system. About a week later, Geo-Heat Center personnel met with Dave and discussed the meager amount of information then available. It was decided that the Geo-Heat Center would attempt to obtain more well data and, if possible, temperature profile the wells to determine what the problem was since available data indicated the wells should produce more heat than they were. At that time the down hole heat exchanger would provide only 116°F to 118°F water during colder periods and 125°F maximum during more moderate weather. The well was being pumped from 76 feet by a jet pump and producing about 25 gpm which was being discharged into the storm drain.

92. [Image] Temperatures in Crater Lake during the summer of 1937


	ill.; Draft report title; Alternate title was scratched through on this draft copy
	Citation Citation Citation Abstract Copy Title: Temperatures in Crater Lake during the summer of 1937 Author: Hassler, Arthur D. Year: 1937, 2008, 2009 ill.; Draft report title; Alternate title was scratched through on this draft copy Title: Temperatures in Crater Lake during the summer of 1937 Author: Hassler, Arthur D. Year: 1937, 2008, 2009 ill.; Draft report title; Alternate title was scratched through on this draft copy

93. [Image] Geothermal Direct-Heat Utilization Assistance, Final Report: September 26, 1990 to March 31, 1999


	The objectives of the use of the money awarded to the Geo-Heat Center were to obtain increased utilization of the large low-to-moderate temperature geothermal resource base by providing users with: (1) ...
	Citation Citation Citation Abstract Copy Title: Geothermal Direct-Heat Utilization Assistance, Final Report: September 26, 1990 to March 31, 1999 Author: Geo-Heat Center Year: 1999 The objectives of the use of the money awarded to the Geo-Heat Center were to obtain increased utilization of the large low-to-moderate temperature geothermal resource base by providing users with: (1) direct-use geothermal project technical and development assistance that offered preliminary system design/economic analysis, equipment/material selection, solutions to operational problems and information/data on resources; (2) research to address current industry needs in the area of cost containment, equipment performance/application and system design, and (3) information, educational materials and services to stimulate development through the publication of an industry quarterly Bulletin, handbooks, presentations, software, website and geothermal library Title: Geothermal Direct-Heat Utilization Assistance, Final Report: September 26, 1990 to March 31, 1999 Author: Geo-Heat Center Year: 1999 The objectives of the use of the money awarded to the Geo-Heat Center were to obtain increased utilization of the large low-to-moderate temperature geothermal resource base by providing users with: (1) direct-use geothermal project technical and development assistance that offered preliminary system design/economic analysis, equipment/material selection, solutions to operational problems and information/data on resources; (2) research to address current industry needs in the area of cost containment, equipment performance/application and system design, and (3) information, educational materials and services to stimulate development through the publication of an industry quarterly Bulletin, handbooks, presentations, software, website and geothermal library

94. [Image] The 1980-1982 Geothermal Resource Assessment Program in Washington


	Since 1978, the Division of Geology and Earth Resources of the Washington Department of Natural Resources has participated in the U.S. Department of Energy's (USDOE) StateCoupled Geothermal Resource Program. ...
	Citation Citation Citation Abstract Copy Title: The 1980-1982 Geothermal Resource Assessment Program in Washington Author: Korosec, M. A. Year: 1983 Since 1978, the Division of Geology and Earth Resources of the Washington Department of Natural Resources has participated in the U.S. Department of Energy's (USDOE) StateCoupled Geothermal Resource Program. Federal and state funds have been used to investigate and evaluate the potential for geothermal resources, on both a reconnaissance and area-specific level. Preliminary results and progress reports for the period up through mid-1980 have already been released as a Division Open File Report (Korosec, Schuster, and others, 1981). Preliminary results and progress summaries of work carried out from mid-1980 through the end of 1982 are presented in this report Title: The 1980-1982 Geothermal Resource Assessment Program in Washington Author: Korosec, M. A. Year: 1983 Since 1978, the Division of Geology and Earth Resources of the Washington Department of Natural Resources has participated in the U.S. Department of Energy's (USDOE) StateCoupled Geothermal Resource Program. Federal and state funds have been used to investigate and evaluate the potential for geothermal resources, on both a reconnaissance and area-specific level. Preliminary results and progress reports for the period up through mid-1980 have already been released as a Division Open File Report (Korosec, Schuster, and others, 1981). Preliminary results and progress summaries of work carried out from mid-1980 through the end of 1982 are presented in this report

95. [Image] An Investigation of the Technical and Economic Feasibility of Using Low Temperature Geothermal Sources in Colorado


	A preliminary feasibility study of utilizing low temperature geothermal sources in Colorado to heat buildings has been completed. It is concluded that the technology for using geothermal sources to heat ...
	Citation Citation Citation Abstract Copy Title: An Investigation of the Technical and Economic Feasibility of Using Low Temperature Geothermal Sources in Colorado Author: Nannen, L. W. Year: 1975 A preliminary feasibility study of utilizing low temperature geothermal sources in Colorado to heat buildings has been completed. It is concluded that the technology for using geothermal sources to heat buildings exists and that the cost of heat will be between $ 2 and 5 per million Btu delivered. Although geothermal heating is more expensive than heating with natural gas at current prices, it is considerably less expensive than heating by means of current solar thermal conversion methods. It is, therefore, recommended that an exploratory well be drilled in a place such as Glenwood Springs, Colorado, to define the thermal, chemical, and geological characteristics of a geothermal source in detail as a first step toward utilization of geothermal energy on a commercial scale in Colorado Title: An Investigation of the Technical and Economic Feasibility of Using Low Temperature Geothermal Sources in Colorado Author: Nannen, L. W. Year: 1975 A preliminary feasibility study of utilizing low temperature geothermal sources in Colorado to heat buildings has been completed. It is concluded that the technology for using geothermal sources to heat buildings exists and that the cost of heat will be between $ 2 and 5 per million Btu delivered. Although geothermal heating is more expensive than heating with natural gas at current prices, it is considerably less expensive than heating by means of current solar thermal conversion methods. It is, therefore, recommended that an exploratory well be drilled in a place such as Glenwood Springs, Colorado, to define the thermal, chemical, and geological characteristics of a geothermal source in detail as a first step toward utilization of geothermal energy on a commercial scale in Colorado

96. [Image] Heat Flow of Oregon


	An extensive new heat flow and geothermal gradient data set for the State of Oregon is presented on a contour map of heat flow at a scale of 1:1,000,000 and is summarized in several figures and tables. ...
	Citation Citation Citation Abstract Copy Title: Heat Flow of Oregon Author: Blackwell, D.D. Year: 1978 An extensive new heat flow and geothermal gradient data set for the State of Oregon is presented on a contour map of heat flow at a scale of 1:1,000,000 and is summarized in several figures and tables. The 1:1,000,000 scale heat flow map is contoured at 20 mW/m/sup 2/ (0.5 HFU) intervals. Also presented are maps of heat flow and temperature at a depth of 1 km averaged for 1/sup 0/ x 1/sup 0/ intervals. Histograms and averages of geothermal gradient and heat flow for the State of Oregon and for the various physiographic provinces within Oregon are also included. The unweighted mean flow for Oregon is 81.3 +- 2.7 mW/m/sup 2/ (1.94 +- 0.06 HFU). The average unweighted geothermal gradient is 65.3 +- 2.5/sup 0/C/km. The average heat flow value weighted on the basis of geographic area is 68 +- 5 mW/m/sup 2/ (1.63 +- 0.12 HFU) and the average weighted geothermal gradient is 55.0 +- 5/sup 0/C/km Title: Heat Flow of Oregon Author: Blackwell, D.D. Year: 1978 An extensive new heat flow and geothermal gradient data set for the State of Oregon is presented on a contour map of heat flow at a scale of 1:1,000,000 and is summarized in several figures and tables. The 1:1,000,000 scale heat flow map is contoured at 20 mW/m/sup 2/ (0.5 HFU) intervals. Also presented are maps of heat flow and temperature at a depth of 1 km averaged for 1/sup 0/ x 1/sup 0/ intervals. Histograms and averages of geothermal gradient and heat flow for the State of Oregon and for the various physiographic provinces within Oregon are also included. The unweighted mean flow for Oregon is 81.3 +- 2.7 mW/m/sup 2/ (1.94 +- 0.06 HFU). The average unweighted geothermal gradient is 65.3 +- 2.5/sup 0/C/km. The average heat flow value weighted on the basis of geographic area is 68 +- 5 mW/m/sup 2/ (1.63 +- 0.12 HFU) and the average weighted geothermal gradient is 55.0 +- 5/sup 0/C/km

97. [Image] Potential of Low-Temperature Geothermal Resources in Northern California. Report No. TR13


	Economically feasible uses for geothermal heat at temperatures too low for conventional electrical power generation at present are delineated. Several geothermal resource areas in northern California that ...
	Citation Citation Citation Abstract Copy Title: Potential of Low-Temperature Geothermal Resources in Northern California. Report No. TR13 Author: Hannah, J.L. Year: 1975 Economically feasible uses for geothermal heat at temperatures too low for conventional electrical power generation at present are delineated. Several geothermal resource areas in northern California that have development potential are described, and applications of the heat found in each area are suggested. Plates are included of the following field study areas: the east side of the Sierra-Cascade Range north of Bishop, and the northern Coast Range from San Francisco Bay to Clear Lake. The counties included in the study area are Mo doc, Lassen, Sierra, Plumas, Placer, Alpine, Mono, Mendocino, Lake, and Sonoma. (LBS) Title: Potential of Low-Temperature Geothermal Resources in Northern California. Report No. TR13 Author: Hannah, J.L. Year: 1975 Economically feasible uses for geothermal heat at temperatures too low for conventional electrical power generation at present are delineated. Several geothermal resource areas in northern California that have development potential are described, and applications of the heat found in each area are suggested. Plates are included of the following field study areas: the east side of the Sierra-Cascade Range north of Bishop, and the northern Coast Range from San Francisco Bay to Clear Lake. The counties included in the study area are Mo doc, Lassen, Sierra, Plumas, Placer, Alpine, Mono, Mendocino, Lake, and Sonoma. (LBS)

98. [Image] Geothermal Heating System for the Children's Museum of Utah


	The results of a study to determine the engineering and economic feasibility of using the Wasatch Hot Spring resource for space heating of the Children's Library building are presented. The Wasatch Hot ...
	Citation Citation Citation Abstract Copy Title: Geothermal Heating System for the Children's Museum of Utah Author: Karlsson, T. Year: 1984 The results of a study to determine the engineering and economic feasibility of using the Wasatch Hot Spring resource for space heating of the Children's Library building are presented. The Wasatch Hot Spring with a reported flow of about 63 gpm (240 l/min) at an average temperature of 104/sup 0/F is not capable of furnishing the needed heat for the Children's Museum building. The underground paths along which the thermal waters flow to their outlets at the Warm Springs Fault are not presently known. It is possible if the thermal water ascends from the deep layers of the earth along the Warm Springs Fault that increased geothermal flow at a higher temperature can be produced by drilling into the fault. Assuming that sufficient geothermal fluid quantity is produced by drilling in the area, an analysis is made of a geothermal heating system for the building based on different fluid temperatures. It is assumed that the present and planned heating systems be left intact with the gas fired boilers taking over during cold periods when the geothermal system fails to provide sufficient heat. Economic analysis shows that the geothermal system is very attractive, even for the lowest geothermal fluid temperature considered (110/sup 0/F) Title: Geothermal Heating System for the Children's Museum of Utah Author: Karlsson, T. Year: 1984 The results of a study to determine the engineering and economic feasibility of using the Wasatch Hot Spring resource for space heating of the Children's Library building are presented. The Wasatch Hot Spring with a reported flow of about 63 gpm (240 l/min) at an average temperature of 104/sup 0/F is not capable of furnishing the needed heat for the Children's Museum building. The underground paths along which the thermal waters flow to their outlets at the Warm Springs Fault are not presently known. It is possible if the thermal water ascends from the deep layers of the earth along the Warm Springs Fault that increased geothermal flow at a higher temperature can be produced by drilling into the fault. Assuming that sufficient geothermal fluid quantity is produced by drilling in the area, an analysis is made of a geothermal heating system for the building based on different fluid temperatures. It is assumed that the present and planned heating systems be left intact with the gas fired boilers taking over during cold periods when the geothermal system fails to provide sufficient heat. Economic analysis shows that the geothermal system is very attractive, even for the lowest geothermal fluid temperature considered (110/sup 0/F)

99. [Image] Assessment of low- to moderate-temperature geothermal resources of Nevada. Final report, April 1978-June 1979


	The ultimate goal of the project was to produce a geothermal resource map of Nevada that provided detailed information on low- to moderate-temperature geothermal systems, and that also evaluated their ...
	Citation Citation Citation Abstract Copy Title: Assessment of low- to moderate-temperature geothermal resources of Nevada. Final report, April 1978-June 1979 Author: Trexler, D.T Year: 1979 The ultimate goal of the project was to produce a geothermal resource map of Nevada that provided detailed information on low- to moderate-temperature geothermal systems, and that also evaluated their potential for direct non-electric utilization. The investigation consisted of these six tasks: edit and verify existing USGS GEOTHERM file for springs and wells in Nevada; supplement GEOTHERM file with NBMG data; digitize the location of springs and wells on 1:250,000 scale maps of Nevada; update water chemistry by sampling areas devoid of data; field check springs and wells designated as hot or warm; and prepare a 1:500,000 scale map of Nevada that evaluates geothermal resource areas of potential for direct use. This report described the completed tasks, delineates problems encountered, and presents additional miscellaneous information that augments the investigation. The information shown on the accompanying map can be divided into two categories: spot data and regional assessment (or potential evaluation). Specific geochemical information, such as temperature, pH, and chemical species, is represented by approximately 300 circle and diamond-shaped symbols. Thirty-seven larger regions were evaluated for their potential for direct-use on the basis of a numerical technique, which is fully described in this report. An additional 15 sites were designated as areas that may provide a basis for investigations, but that lack sufficient data for a detailed potential evaluation at this time. ; NVO-01556-1 Title: Assessment of low- to moderate-temperature geothermal resources of Nevada. Final report, April 1978-June 1979 Author: Trexler, D.T Year: 1979 The ultimate goal of the project was to produce a geothermal resource map of Nevada that provided detailed information on low- to moderate-temperature geothermal systems, and that also evaluated their potential for direct non-electric utilization. The investigation consisted of these six tasks: edit and verify existing USGS GEOTHERM file for springs and wells in Nevada; supplement GEOTHERM file with NBMG data; digitize the location of springs and wells on 1:250,000 scale maps of Nevada; update water chemistry by sampling areas devoid of data; field check springs and wells designated as hot or warm; and prepare a 1:500,000 scale map of Nevada that evaluates geothermal resource areas of potential for direct use. This report described the completed tasks, delineates problems encountered, and presents additional miscellaneous information that augments the investigation. The information shown on the accompanying map can be divided into two categories: spot data and regional assessment (or potential evaluation). Specific geochemical information, such as temperature, pH, and chemical species, is represented by approximately 300 circle and diamond-shaped symbols. Thirty-seven larger regions were evaluated for their potential for direct-use on the basis of a numerical technique, which is fully described in this report. An additional 15 sites were designated as areas that may provide a basis for investigations, but that lack sufficient data for a detailed potential evaluation at this time. ; NVO-01556-1

100. [Image] Development of the high-temperature redox electrode. Interim report ending March 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 ...
	Citation Citation Citation Abstract Copy 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 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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1. [Image] Temperatures of Springs in the vicinity of Crater Lake, Oregon in Relation to Air and Ground Temperatures

2. [Image] Steady-State and Transient Wellbore Temperatures during Drilling

3. [Image] Guidance for evaluating and recommending temperature regimes to protect fish

4. [Image] Influences of human activity on stream temperatures and existence of cold-water fish in streams with elevated temperature: report of a workshop: Independent Multidisciplinary Science Team, Corvallis, OR, October 5-6, 2000

5. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maryland-District of Columbia

6. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Virginia-District of Columbia

7. [Image] Potential Uses for a High-Temperature Borehole Gravimeter

8. [Image] Fluid-Temperature Logs for Selected Wells in Eastern Washington

9. [Image] Low Temperature Geothermal Resource Management

10. [Image] C. D. Hopkins, et al. , No. 2. Geothermal Well-Of-Opportunity, Wayne County, Georgia. Operational Report

11. [Image] Optimization of Residential Size Heat Pumps for Use With Geothermal Energy

12. [Image] Production of Ethanol for Automotive Fuel Employing Geothermal Energy

13. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arkansas

14. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alabama

15. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Connecticut

16. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Delaware

17. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Georgia

18. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Florida

19. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Illinois

20. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Indiana

21. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Iowa

22. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kansas

23. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Kentucky

24. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Louisiana

25. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Maine

26. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Massachusetts

27. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Michigan

28. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Minnesota

29. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Mississippi

30. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Missouri

31. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nebraska

32. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Hampshire

33. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Jersey

34. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New York

35. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Carolina

36. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Ohio

37. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oklahoma

38. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Pennsylvania

39. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Rhode Island

40. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Carolina

41. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Tennessee

42. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Texas

43. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Vermont

44. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 West Virginia

45. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wisconsin

46. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Alaska

47. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Arizona

48. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 California

49. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Colorado

50. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 South Dakota

51. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Utah

52. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Washington

53. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 New Mexico

54. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Oregon

55. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Hawaii

56. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Montana

57. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Nevada

58. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Wyoming

59. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 North Dakota

60. [Image] Monthly Normals of Temperature, Precipitation, and Heating and Cooling Degree Days 1951-1980 Idaho

61. [Image] The Cody Hydrothermal System

62. [Image] Interactive Fracture Design Model

63. [Image] High Temperature Electronics and Instrumentation Seminar: December 3-4, 1979

64. [Image] Chloride/Magnesium Ratio of Shallow Groundwaters as a Regional Geothermal Indicator in Hawaii

65. [Image] Neutron Formation Temperature Gauge and Neutron Activation Analysis Brine Flow Meter. Final Report, October 1, 1976--March 31, 1978

66. [Image] Assessment of geothermal resources of Caliente, Nevada

67. [Image] Geochemistry of the Colado geothermal area, Pershing County, Nevada

68. [Image] Static Downhole Characteristics of Well CGEH-1 at Coso Hot Springs, China Lake, California

69. [Image] Formation Temperature Gauge Feasibility Study. Volume II, Interim Report

70. [Image] Water quality monitoring : technical guide book

71. [Image] Diesel Heat Pump for District Heating Plants and for the Heating of Large Housing Blocks