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• 1. [Article] Diurnal timing of warmer air under climate change affects magnitude, timing and duration of stream temperature change

  To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by John Wiley ...

  Citation × Citation Citation Abstract Copy Title: Diurnal timing of warmer air under climate change affects magnitude, timing and duration of stream temperature change Author: Haggerty, Roy, Wondzell, Steven M., Diabat, Mousa To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by John Wiley & Sons Ltd. and can be found at: http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)1099-1085. Title: Diurnal timing of warmer air under climate change affects magnitude, timing and duration of stream temperature change Author: Haggerty, Roy, Wondzell, Steven M., Diabat, Mousa To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by John Wiley & Sons Ltd. and can be found at: http://onlinelibrary.wiley.com/journal/10.1002/(ISSN)1099-1085. Close

• 2. [Article] Can air temperature be used to project influences of climate change on stream temperature?

  To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by the Institute ...

  Citation × Citation Citation Abstract Copy Title: Can air temperature be used to project influences of climate change on stream temperature? Author: Arismendi, Ivan, Johnson, Sherri L., Safeeq, Mohammad, Dunham, Jason B. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by the Institute of Physics Publishing and can be found at: http://iopscience.iop.org/1748-9326/. Title: Can air temperature be used to project influences of climate change on stream temperature? Author: Arismendi, Ivan, Johnson, Sherri L., Safeeq, Mohammad, Dunham, Jason B. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by the Institute of Physics Publishing and can be found at: http://iopscience.iop.org/1748-9326/. Close

• 3. [Article] Formulation of surface heat flux: application to BOREAS

  The aerodynamic temperature is required for prediction of the surface heat flux using Monin-Obukhov similarity. This "fictitious" temperature is not systematically equal to the actual air temperature near ...

  Citation × Citation Citation Abstract Copy Title: Formulation of surface heat flux: application to BOREAS Author: Mahrt, Larry, Jensen, N.O., MacPherson, J.I., Sun, Jielun, Desjardins, R.L. The aerodynamic temperature is required for prediction of the surface heat flux using Monin-Obukhov similarity. This "fictitious" temperature is not systematically equal to the actual air temperature near the surface and is not directly available from observations or in numerical models. The aerodynamic temperature is normally replaced with either the canopy air temperature or the surface radiation temperature, sometimes accompanied by adjustment of the thermal roughness length or specification of an excess resistance. In this study, the relationship between the aerodynamic temperature and the surface radiation temperature is examined in terms of the surface energy budget and simple representation of canopy structure. Previous inconsistencies are discussed. The observed behavior of the aerodynamic temperature is studied using Canadian Twin Otter aircraft data from BOREAS over nine different forested and nonforested sites. Variation of the behavior of the aerodynamic temperature between different parts of the boreal forest is found to be strongly correlated with the red reflectance. Title: Formulation of surface heat flux: application to BOREAS Author: Mahrt, Larry, Jensen, N.O., MacPherson, J.I., Sun, Jielun, Desjardins, R.L. The aerodynamic temperature is required for prediction of the surface heat flux using Monin-Obukhov similarity. This "fictitious" temperature is not systematically equal to the actual air temperature near the surface and is not directly available from observations or in numerical models. The aerodynamic temperature is normally replaced with either the canopy air temperature or the surface radiation temperature, sometimes accompanied by adjustment of the thermal roughness length or specification of an excess resistance. In this study, the relationship between the aerodynamic temperature and the surface radiation temperature is examined in terms of the surface energy budget and simple representation of canopy structure. Previous inconsistencies are discussed. The observed behavior of the aerodynamic temperature is studied using Canadian Twin Otter aircraft data from BOREAS over nine different forested and nonforested sites. Variation of the behavior of the aerodynamic temperature between different parts of the boreal forest is found to be strongly correlated with the red reflectance. Close

• 4. [Article] The influence of air and soil temperatures on the growth and development of Easter lily, Lilium longiflorum, during different growth phases

  Greenhouse-grown, September-harvested Lilium longiflorum cv. 'Nellie white' bulbs were used to determine temperature requirements during 5 pre-bloom and 1 post-bloom phases of development each of 1 month's ...

  Citation × Citation Citation Abstract Copy Title: The influence of air and soil temperatures on the growth and development of Easter lily, Lilium longiflorum, during different growth phases Author: Wang, Yin-Tung Greenhouse-grown, September-harvested Lilium longiflorum cv. 'Nellie white' bulbs were used to determine temperature requirements during 5 pre-bloom and 1 post-bloom phases of development each of 1 month's duration. Plantes were subjected to 3 air temperatures(24°day/ 18°C night, 18°/13° and 13°/10°) in combination with soil temperatures at 30°, 24°, and equal to or lower than ambient air temperature during each growth phase and evaluated by growth analysis at the termination of each phase. This study has substantiated that top growth needs high air temperature and daughter scale initiation and filling require high soil temperature. An air and soil temperature of 24°C was required for rapid flowering, leaf unfolding and stem elongation but at the expense of reserves in mother scales. Air temperature approaching 18°/13° during the month prior to anthesis favored maintenance of mother scales. Growth of daughter scales during the pre-bloom period was directly related to soil temperature rather than air temperature with 30° soil temperature being no better than 24°. Soil temperature had no effect on flower bud expansion after buds-visible stage, air temperature being the determining factor thereafter. Growth of the flower bud, leaf unfolding rate or stem elongation were of equal value in monitoring crop growth rate and status. Soil temperatures approaching 24°C. favored scale primordia initiation, regardless of air temperature. Daughter meristem diameter, as well as the rate of scale primordia initiation decreased progressively from daughter bulb appearance toward anthesis of the mother axis. High soil temperatures also reduced daughter bulb apex diameter during early growth phases. Since prevailing air and soil temperatures in the commercial lily growing sites are below those required for maximum growth and development of above- and below-ground organs during the pre-bloom period, it is concluded that air temperatures alone are adequate in monitoring field crop status and predicting ultimate yield potential during this period. Title: The influence of air and soil temperatures on the growth and development of Easter lily, Lilium longiflorum, during different growth phases Author: Wang, Yin-Tung Greenhouse-grown, September-harvested Lilium longiflorum cv. 'Nellie white' bulbs were used to determine temperature requirements during 5 pre-bloom and 1 post-bloom phases of development each of 1 month's duration. Plantes were subjected to 3 air temperatures(24°day/ 18°C night, 18°/13° and 13°/10°) in combination with soil temperatures at 30°, 24°, and equal to or lower than ambient air temperature during each growth phase and evaluated by growth analysis at the termination of each phase. This study has substantiated that top growth needs high air temperature and daughter scale initiation and filling require high soil temperature. An air and soil temperature of 24°C was required for rapid flowering, leaf unfolding and stem elongation but at the expense of reserves in mother scales. Air temperature approaching 18°/13° during the month prior to anthesis favored maintenance of mother scales. Growth of daughter scales during the pre-bloom period was directly related to soil temperature rather than air temperature with 30° soil temperature being no better than 24°. Soil temperature had no effect on flower bud expansion after buds-visible stage, air temperature being the determining factor thereafter. Growth of the flower bud, leaf unfolding rate or stem elongation were of equal value in monitoring crop growth rate and status. Soil temperatures approaching 24°C. favored scale primordia initiation, regardless of air temperature. Daughter meristem diameter, as well as the rate of scale primordia initiation decreased progressively from daughter bulb appearance toward anthesis of the mother axis. High soil temperatures also reduced daughter bulb apex diameter during early growth phases. Since prevailing air and soil temperatures in the commercial lily growing sites are below those required for maximum growth and development of above- and below-ground organs during the pre-bloom period, it is concluded that air temperatures alone are adequate in monitoring field crop status and predicting ultimate yield potential during this period. Close

• 5. [Article] Influences of Human Activity on Stream Temperatures and Existence of Cold-Water Fish in Streams with Elevated Temperature: Report of a Workshop

  This report was prepared by the Independent Multidisciplinary Science Team of the Oregon Plan for Salmon and Watersheds

  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 Author: Independent Multidisciplinary Science Team (Or.) This report was prepared by the Independent Multidisciplinary Science Team of the Oregon Plan for Salmon and Watersheds Title: Influences of Human Activity on Stream Temperatures and Existence of Cold-Water Fish in Streams with Elevated Temperature: Report of a Workshop Author: Independent Multidisciplinary Science Team (Or.) This report was prepared by the Independent Multidisciplinary Science Team of the Oregon Plan for Salmon and Watersheds Close

• 6. [Article] Oxygen consumption of three species of sea urchins at different temperatures

  Metabolic rate-temperature responses of three related species of sea urchins were determined using oxygen consumption rate measurements. The three species used were Strongylocentrotus purpuratus, Strongylocentrotus ...

  Citation × Citation Citation Abstract Copy Title: Oxygen consumption of three species of sea urchins at different temperatures Author: Ulbricht, Richard Jules Metabolic rate-temperature responses of three related species of sea urchins were determined using oxygen consumption rate measurements. The three species used were Strongylocentrotus purpuratus, Strongylocentrotus franciscanus, and Allocentrotus fragilis. All measurements were made using an oxygen macro-electrode, physiological gas analyzer, and sealed respiratory container. Two series of experiments--field-acclimatized and temperature-acclimated--were conducted. In each case, oxygen consumption was determined at 3° intervals over a temperature range extending from 6° to 24°. The results of the field-acclimatized animals, maintained in the laboratory for only short periods after collection, are consistent with the temperature fluctuations of the respective habitats. The benthic A. fragilis did not possess any rate-temperature independence. The partly intertidal S. franciscanus possessed little independence. The largely intertidal S. purpuratus possessed a great deal of rate-temperature independence, especially from 12° to 21°. S. purpuratus and S. franciscanus were used in the temperature acclimation study. Both species were maintained at 9° and 18° for a month. The results of both species clearly show "reverse" compensation--i.e. the rate mean of the warm-acclimated animals exceeds that of the cold-acclimated animals at the same test temperature. Temperature-acclimated S. purpuratus possessed considerable temperature compensation. Cold-acclimated animals had greater rate-temperature independence between 9° and 15°, whereas warm-acclimated animals had greater independence between 15° and 24°. Temperature-acclimated S. franciscanus possessed little temperature compensation. Cold-acclimated animals had no rate-temperature independence. Warm-acclimated animals had some independence over the upper end of the temperature range tested. Comparison of the "field-acclimatized" metabolic rate-temperature curve with the appropriate "temperature-acclimated" curves suggests that summer-acclimatized S. purpuratus is more warm-acclimated and summer-acclimatized S. franciscanus is more cold-acclimated. Title: Oxygen consumption of three species of sea urchins at different temperatures Author: Ulbricht, Richard Jules Metabolic rate-temperature responses of three related species of sea urchins were determined using oxygen consumption rate measurements. The three species used were Strongylocentrotus purpuratus, Strongylocentrotus franciscanus, and Allocentrotus fragilis. All measurements were made using an oxygen macro-electrode, physiological gas analyzer, and sealed respiratory container. Two series of experiments--field-acclimatized and temperature-acclimated--were conducted. In each case, oxygen consumption was determined at 3° intervals over a temperature range extending from 6° to 24°. The results of the field-acclimatized animals, maintained in the laboratory for only short periods after collection, are consistent with the temperature fluctuations of the respective habitats. The benthic A. fragilis did not possess any rate-temperature independence. The partly intertidal S. franciscanus possessed little independence. The largely intertidal S. purpuratus possessed a great deal of rate-temperature independence, especially from 12° to 21°. S. purpuratus and S. franciscanus were used in the temperature acclimation study. Both species were maintained at 9° and 18° for a month. The results of both species clearly show "reverse" compensation--i.e. the rate mean of the warm-acclimated animals exceeds that of the cold-acclimated animals at the same test temperature. Temperature-acclimated S. purpuratus possessed considerable temperature compensation. Cold-acclimated animals had greater rate-temperature independence between 9° and 15°, whereas warm-acclimated animals had greater independence between 15° and 24°. Temperature-acclimated S. franciscanus possessed little temperature compensation. Cold-acclimated animals had no rate-temperature independence. Warm-acclimated animals had some independence over the upper end of the temperature range tested. Comparison of the "field-acclimatized" metabolic rate-temperature curve with the appropriate "temperature-acclimated" curves suggests that summer-acclimatized S. purpuratus is more warm-acclimated and summer-acclimatized S. franciscanus is more cold-acclimated. Close

• 7. [Article] Appendix C - Stream Temperature Model.zip

  Citation × Citation Citation Abstract Copy Title: Appendix C - Stream Temperature Model.zip Author: Arik, Aida D. Title: Appendix C - Stream Temperature Model.zip Author: Arik, Aida D. Close

• 8. [Article] Geothermics and climate change : 2. joint analysis of borehole temperature and meteorological data

  copyrighted by American Geophysical Union

  Citation × Citation Citation Abstract Copy Title: Geothermics and climate change : 2. joint analysis of borehole temperature and meteorological data Author: Chapman, David S., Harris, Robert N. copyrighted by American Geophysical Union Title: Geothermics and climate change : 2. joint analysis of borehole temperature and meteorological data Author: Chapman, David S., Harris, Robert N. copyrighted by American Geophysical Union Close

• 9. [Article] A distributed stream temperature model using high resolution temperature observations

  This is the publisher’s final pdf. The published article is copyrighted by European Geosciences Union and can be found at: http://www.egu.eu/.

  Citation × Citation Citation Abstract Copy Title: A distributed stream temperature model using high resolution temperature observations Author: Westhoff, M. C., Selker, J. S., Pfister, L., van de Giesen, N. C., Savenije, H. H. G., Stelling, G. S., Luxemburg, W. M. J ., Uhlenbrook, S. This is the publisher’s final pdf. The published article is copyrighted by European Geosciences Union and can be found at: http://www.egu.eu/. Title: A distributed stream temperature model using high resolution temperature observations Author: Westhoff, M. C., Selker, J. S., Pfister, L., van de Giesen, N. C., Savenije, H. H. G., Stelling, G. S., Luxemburg, W. M. J ., Uhlenbrook, S. This is the publisher’s final pdf. The published article is copyrighted by European Geosciences Union and can be found at: http://www.egu.eu/. Close

• 10. [Article] Bed conduction impact on fiber optic distributed temperature sensing water temperature measurements

  This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by Copernicus Publications on behalf of the European Geosciences Union. The published article can ...

  Citation × Citation Citation Abstract Copy Title: Bed conduction impact on fiber optic distributed temperature sensing water temperature measurements Author: O'Donnell Meininger, T., Selker, J. S. This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by Copernicus Publications on behalf of the European Geosciences Union. The published article can be found at: http://www.geoscientific-instrumentation-methods-and-data-systems.net/ Title: Bed conduction impact on fiber optic distributed temperature sensing water temperature measurements Author: O'Donnell Meininger, T., Selker, J. S. This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by Copernicus Publications on behalf of the European Geosciences Union. The published article can be found at: http://www.geoscientific-instrumentation-methods-and-data-systems.net/ Close

• 11. [Article] Repeat temperature measurements in boreholes from northwestern Utah link ground and air temperature changes at the decadal time scale

  Borehole temperature profiles provide a record of ground surface temperature (GST) change at the decadal to centennial time scale. GST histories reconstructed from boreholes are particularly useful in ...

  Citation × Citation Citation Abstract Copy Title: Repeat temperature measurements in boreholes from northwestern Utah link ground and air temperature changes at the decadal time scale Author: Chapman, David S., Harris, Robert N., Davis, Michael G. Borehole temperature profiles provide a record of ground surface temperature (GST) change at the decadal to centennial time scale. GST histories reconstructed from boreholes are particularly useful in climate reconstruction if changes in GST and surface air temperature (SAT) are effectively coupled at decadal and longer time periods and it can be shown that borehole temperatures respond faithfully to surface temperature changes. We test these assumptions using three boreholes in northwestern Utah that have been repeatedly logged for temperature over a time span of 29 years. We report 13 temperaturedepth logs at the Emigrant Pass Observatory borehole GC‐1, eight at borehole SI‐1 and five at borehole DM‐1, acquired between 1978 and 2007. Systematic subsurface temperature changes of up to 0.6°C are observed over this time span in the upper sections of the boreholes; below approximately 100 m any temperature transients are within observational noise. We difference the temperature logs to highlight subsurface transients and to remove any ambiguity resulting from steady state source of curvature. Synthetic temperature profiles computed from SAT data at nearby meteorological stations reproduce both the amplitude and pattern of the transient temperature observations, fitting the observations to within 0.03°C or better. This observational confirmation of the strong coupling between surface temperature change and borehole temperature transients lends further support to the use of borehole temperatures to complement SAT and multiproxy reconstructions of climate change. Title: Repeat temperature measurements in boreholes from northwestern Utah link ground and air temperature changes at the decadal time scale Author: Chapman, David S., Harris, Robert N., Davis, Michael G. Borehole temperature profiles provide a record of ground surface temperature (GST) change at the decadal to centennial time scale. GST histories reconstructed from boreholes are particularly useful in climate reconstruction if changes in GST and surface air temperature (SAT) are effectively coupled at decadal and longer time periods and it can be shown that borehole temperatures respond faithfully to surface temperature changes. We test these assumptions using three boreholes in northwestern Utah that have been repeatedly logged for temperature over a time span of 29 years. We report 13 temperaturedepth logs at the Emigrant Pass Observatory borehole GC‐1, eight at borehole SI‐1 and five at borehole DM‐1, acquired between 1978 and 2007. Systematic subsurface temperature changes of up to 0.6°C are observed over this time span in the upper sections of the boreholes; below approximately 100 m any temperature transients are within observational noise. We difference the temperature logs to highlight subsurface transients and to remove any ambiguity resulting from steady state source of curvature. Synthetic temperature profiles computed from SAT data at nearby meteorological stations reproduce both the amplitude and pattern of the transient temperature observations, fitting the observations to within 0.03°C or better. This observational confirmation of the strong coupling between surface temperature change and borehole temperature transients lends further support to the use of borehole temperatures to complement SAT and multiproxy reconstructions of climate change. Close

• 12. [Article] Summer stream temperatures and channel characteristics of a southwestern Oregon coastal stream

  The Elk River Basin drains 93 sq ml of steep forested terrain on the west side of the Klamath Mountains in Southwest Oregon. This river and its tributaries support a diverse and abundant population of ...

  Citation × Citation Citation Abstract Copy Title: Summer stream temperatures and channel characteristics of a southwestern Oregon coastal stream Author: McSwain, Michelle D. The Elk River Basin drains 93 sq ml of steep forested terrain on the west side of the Klamath Mountains in Southwest Oregon. This river and its tributaries support a diverse and abundant population of anadromous fish; a hatchery located at river mile 13 (km 21) supplements these native populations. Clear weather in combination with dry summers and low streamflow produce warm water temperatures. Historical data indicate that summer stream temperatures as high as 76°F (24.4°C) have occurred in the mainstem of the Elk River. This study was undertaken to evaluate summer stream temperatures and to what extent they were affected by natural factors and land use. In selected tributaries and along the mainstem of the Elk River, measurements were made on canopy cover, stream surface width, and thalweg depth during the summers of 1984 and 1985. Recording thermographs and maximum/minimum thermometers were used to determine the overall temperature pattern of the basin. In genera.l, maximum stream temperatures appear to be declining since 1970, following a period of increased landslide activity in the basin. The trend of decreasing maximum temperatures was not associated with changes in summer streamflow or summer precipitation patterns, suggesting that a recovery of streamside vegetation and/or change in channel morphology is proceeding within the basin. Tributaries with relatively large width / depth ratios (exceeding 14 or more), generally exhibited large diurnal fluctuations in temperature indicating solar heating was occurring. For drainages of similar size, large diurnal temperature fluctuations were associated with large surface area to volume ratios. Tributaries found to be especially low in maximum temperatures generally flow subsurface as a result of channel aggradation. In the 1984 and 1985 field seasons, maximum stream temperatures in the tributaries never exceeded the maximum temperature of 69°F (20.6°C) found in the mainstem. The upper reaches of the mainstem, which is wide and aggraded, was the portion of the basin found to have the highest maximum stream temperatures. Five pools were sampled to determine vertical profiles of temperature and dissolved oxygen. Temperatures and dissolved oxygen concentrations did not vary with depth. Title: Summer stream temperatures and channel characteristics of a southwestern Oregon coastal stream Author: McSwain, Michelle D. The Elk River Basin drains 93 sq ml of steep forested terrain on the west side of the Klamath Mountains in Southwest Oregon. This river and its tributaries support a diverse and abundant population of anadromous fish; a hatchery located at river mile 13 (km 21) supplements these native populations. Clear weather in combination with dry summers and low streamflow produce warm water temperatures. Historical data indicate that summer stream temperatures as high as 76°F (24.4°C) have occurred in the mainstem of the Elk River. This study was undertaken to evaluate summer stream temperatures and to what extent they were affected by natural factors and land use. In selected tributaries and along the mainstem of the Elk River, measurements were made on canopy cover, stream surface width, and thalweg depth during the summers of 1984 and 1985. Recording thermographs and maximum/minimum thermometers were used to determine the overall temperature pattern of the basin. In genera.l, maximum stream temperatures appear to be declining since 1970, following a period of increased landslide activity in the basin. The trend of decreasing maximum temperatures was not associated with changes in summer streamflow or summer precipitation patterns, suggesting that a recovery of streamside vegetation and/or change in channel morphology is proceeding within the basin. Tributaries with relatively large width / depth ratios (exceeding 14 or more), generally exhibited large diurnal fluctuations in temperature indicating solar heating was occurring. For drainages of similar size, large diurnal temperature fluctuations were associated with large surface area to volume ratios. Tributaries found to be especially low in maximum temperatures generally flow subsurface as a result of channel aggradation. In the 1984 and 1985 field seasons, maximum stream temperatures in the tributaries never exceeded the maximum temperature of 69°F (20.6°C) found in the mainstem. The upper reaches of the mainstem, which is wide and aggraded, was the portion of the basin found to have the highest maximum stream temperatures. Five pools were sampled to determine vertical profiles of temperature and dissolved oxygen. Temperatures and dissolved oxygen concentrations did not vary with depth. Close

• 13. [Article] Stream Temperature Modeling for Marys River Watershed

  High water temperatures in rivers have detrimental effects on riverine water quality and ecology. In this study, two river temperature models, within the agricultural watershed model Soil and Water Assessment ...

  Citation × Citation Citation Abstract Copy Title: Stream Temperature Modeling for Marys River Watershed Author: Mustafa, Mamoon High water temperatures in rivers have detrimental effects on riverine water quality and ecology. In this study, two river temperature models, within the agricultural watershed model Soil and Water Assessment Tool (SWAT), were investigated for their ability to simulate water temperatures accurately throughout the year. The original temperature model within SWAT uses a linear approach to estimate stream temperature based on air temperature and does not account for hydrological components for calculating stream temperature. Recently, a new stream temperature model for SWAT was developed that combines meteorological with hydrological components such as lateral flow, snowmelt, groundwater flow and surface runoff. The model also uses three elements for the stream temperature calculations – specifically, within a sub-basin (temperature and flow rate), upstream of sub-basin (temperature and incoming flow), and air-water temperature heat exchange transfer. The goal of this research was to improve the recently developed temperature model further by incorporating different types of heat exchange sources, in addition to air-water heat transfer. The edited model was tested for Marys River, a west tributary of the Willamette River in Oregon. The output from the edited model was then compared with observed stream temperatures, for different spatial locations within the watershed to assess the model efficiency. The results showed a good agreement for forested region compared to Ficklin’s default model with RMSE of both models matching. However, there were over predictions and more noise in predicting stream temperature for agricultural region within the watershed in which resulted in higher RMSE for edited model. Title: Stream Temperature Modeling for Marys River Watershed Author: Mustafa, Mamoon High water temperatures in rivers have detrimental effects on riverine water quality and ecology. In this study, two river temperature models, within the agricultural watershed model Soil and Water Assessment Tool (SWAT), were investigated for their ability to simulate water temperatures accurately throughout the year. The original temperature model within SWAT uses a linear approach to estimate stream temperature based on air temperature and does not account for hydrological components for calculating stream temperature. Recently, a new stream temperature model for SWAT was developed that combines meteorological with hydrological components such as lateral flow, snowmelt, groundwater flow and surface runoff. The model also uses three elements for the stream temperature calculations – specifically, within a sub-basin (temperature and flow rate), upstream of sub-basin (temperature and incoming flow), and air-water temperature heat exchange transfer. The goal of this research was to improve the recently developed temperature model further by incorporating different types of heat exchange sources, in addition to air-water heat transfer. The edited model was tested for Marys River, a west tributary of the Willamette River in Oregon. The output from the edited model was then compared with observed stream temperatures, for different spatial locations within the watershed to assess the model efficiency. The results showed a good agreement for forested region compared to Ficklin’s default model with RMSE of both models matching. However, there were over predictions and more noise in predicting stream temperature for agricultural region within the watershed in which resulted in higher RMSE for edited model. Close

• 14. [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) Close

• 15. [Article] Evaluation of stream temperature spatial variation using distributed temperature sensing

  Water temperature in rivers and streams is an important factor for aquatic ecosystem health. Measurement of stream temperature has traditionally been accomplished by point temperature measurements, continuous ...

  Citation × Citation Citation Abstract Copy Title: Evaluation of stream temperature spatial variation using distributed temperature sensing Author: O'Donnell, Tara Water temperature in rivers and streams is an important factor for aquatic ecosystem health. Measurement of stream temperature has traditionally been accomplished by point temperature measurements, continuous point temperature loggers, and more recently, airborne remote sensing techniques such as Forward-Looking Infrared Radar (FLIR) or Thermal Infrared Radiometry. While each of these measurement techniques has certain advantages, none allows for the combined spatial and temporal information provided by Distributed Temperature Sensing (DTS). DTS employs fiber optic signals to measure temperature and is a relatively new temperature measurement technology for hydrologic sensing applications. Nine DTS stream temperature datasets were collected in the Middle Fork John Day River (MFJDR) as part of a basin-wide stream monitoring effort. The datasets encompassed five 1-3 kilometer long reaches, some monitored over three summers (2009-2011). In contrast to existing stream temperature measurement technologies, DTS can provide stream temperature data in both the spatial and temporal domains. Techniques and challenges of interpreting DTS stream temperature data were documented, and three applications of the technology to stream temperature monitoring were explored. Cold water patches, potentially used by fish as thermal refugia during stream temperature maximums, were located using DTS. No identified cold patch exceeded 2.31°C cooler than ambient stream temperature. Tributary inflows provided some of the most temperature-differentiated cold patches. These findings provide a reference for the degree of thermal heterogeneity in the MFJDR system and beg the question of whether fish respond to small (<3°C) spatial temperature variations. Theoretical predictions of stream mixing potential (Richardson number and cavity flow mixing predictions) suggested that increasing stream thermal heterogeneity would require channel modification to decrease stream flow velocity in select areas. The combined spatial and temporal coverage of a DTS stream temperature dataset on the Oxbow Conservation Area allowed diagnosis of a 2°C longitudinal stream temperature decrease observed in multiple Thermal Infrared Radiometry (TIR) and Forward-Looking Infrared Radiometry (FLIR) datasets collected on that reach. Advection velocity and channel depth, rather than groundwater or tributary inflows, were the main cause of the decrease, and the magnitude of the decrease peaked in the early afternoon, disappearing completely by evening. This finding suggests caution for interpretation of FLIR and TIR stream temperature datasets, which represent "snapshot" temperature measurements. For these datasets, knowledge of flow conditions (velocity and depth) may help avoid misinterpretation of temporally-transient temperature anomalies. Diurnal slope periodicity was observed in linear-like spatial trends in four DTS datasets, and an analysis was made to examine this subtle spatially and temporally varying phenomenon. The phase of the diurnal slope variation differed between river reaches, suggesting that propagation of larger-scale thermal waves might be one driving mechanism. Temporally-constant offsets between slope magnitudes within reaches suggested some intra-reach differences in heat fluxes. Title: Evaluation of stream temperature spatial variation using distributed temperature sensing Author: O'Donnell, Tara Water temperature in rivers and streams is an important factor for aquatic ecosystem health. Measurement of stream temperature has traditionally been accomplished by point temperature measurements, continuous point temperature loggers, and more recently, airborne remote sensing techniques such as Forward-Looking Infrared Radar (FLIR) or Thermal Infrared Radiometry. While each of these measurement techniques has certain advantages, none allows for the combined spatial and temporal information provided by Distributed Temperature Sensing (DTS). DTS employs fiber optic signals to measure temperature and is a relatively new temperature measurement technology for hydrologic sensing applications. Nine DTS stream temperature datasets were collected in the Middle Fork John Day River (MFJDR) as part of a basin-wide stream monitoring effort. The datasets encompassed five 1-3 kilometer long reaches, some monitored over three summers (2009-2011). In contrast to existing stream temperature measurement technologies, DTS can provide stream temperature data in both the spatial and temporal domains. Techniques and challenges of interpreting DTS stream temperature data were documented, and three applications of the technology to stream temperature monitoring were explored. Cold water patches, potentially used by fish as thermal refugia during stream temperature maximums, were located using DTS. No identified cold patch exceeded 2.31°C cooler than ambient stream temperature. Tributary inflows provided some of the most temperature-differentiated cold patches. These findings provide a reference for the degree of thermal heterogeneity in the MFJDR system and beg the question of whether fish respond to small (<3°C) spatial temperature variations. Theoretical predictions of stream mixing potential (Richardson number and cavity flow mixing predictions) suggested that increasing stream thermal heterogeneity would require channel modification to decrease stream flow velocity in select areas. The combined spatial and temporal coverage of a DTS stream temperature dataset on the Oxbow Conservation Area allowed diagnosis of a 2°C longitudinal stream temperature decrease observed in multiple Thermal Infrared Radiometry (TIR) and Forward-Looking Infrared Radiometry (FLIR) datasets collected on that reach. Advection velocity and channel depth, rather than groundwater or tributary inflows, were the main cause of the decrease, and the magnitude of the decrease peaked in the early afternoon, disappearing completely by evening. This finding suggests caution for interpretation of FLIR and TIR stream temperature datasets, which represent "snapshot" temperature measurements. For these datasets, knowledge of flow conditions (velocity and depth) may help avoid misinterpretation of temporally-transient temperature anomalies. Diurnal slope periodicity was observed in linear-like spatial trends in four DTS datasets, and an analysis was made to examine this subtle spatially and temporally varying phenomenon. The phase of the diurnal slope variation differed between river reaches, suggesting that propagation of larger-scale thermal waves might be one driving mechanism. Temporally-constant offsets between slope magnitudes within reaches suggested some intra-reach differences in heat fluxes. Close

• 16. [Article] Effects of modifying the environment on flowering, fruiting, and biochemical composition of the snap bean (Phaseolus vulgaris L.)

  The effects of modifying air temperature, soil temperature, and soil moisture levels on flowering, fruiting, and chemical composition of Tendercrop snap beans were studied in experiments in the field and ...

  Citation × Citation Citation Abstract Copy Title: Effects of modifying the environment on flowering, fruiting, and biochemical composition of the snap bean (Phaseolus vulgaris L.) Author: Singh, Jyotendra Narain The effects of modifying air temperature, soil temperature, and soil moisture levels on flowering, fruiting, and chemical composition of Tendercrop snap beans were studied in experiments in the field and in the greenhouse during 1961, 1962, and 1963. High maximum temperatures of 95-105° F. during bloom reduced the percent set and number and weight of pods of bean plants. Plants appeared to be most sensitive to temperatures at six to eight days after first bloom. Air temperatures in the field were increased 8-10° F. above controls by use of clear polyethylene plastic cages. The carbohydrate content of leaves and stems of plants subjected to high temperatures was decreased with a greater relative reduction of starch than of other sugars. Air temperature appeared also to affect the protein metabolism since cystine was not detected in plants subjected- to high temperature. Furthermore, threonine was detected in plants exposed to high temperatures, but not in control plants. Soil temperatures ranging from 55° to 90° F. had a pronounced effect on growth, flowering, and yield of snap beans, with best growth of plants and highest number of flowers and pods and weight of pods being obtained at soil temperatures of 75° to 80° F. Diurnal fluctuation of soil temperature had no advantage over comparable constant mean soil temperature for growth of plants. An exception was at fluctuating soil temperatures of 50-60° F- compared to constant temperature of 55° F. Soil temperature did not affect levels of total sugar and reducing sugar, but the starch content was decreased with an increase in soil temperature. Sucrose content of plants at fluctuating soil temperatures tended to be higher than in plants grown at comparable constant mean temperatures. Dry weight of shoots and roots and P and K content of plants increased with increased soil temperature. Magnesium content tended to decrease with an increase of soil temperature while Ca content of plants was variable. Snap bean plants which received the highest amount and frequency of irrigation from planting to harvest had the highest dry weight of shoots, number of flowers, percent set, and yield of pods when compared to plants subjected to moisture stress, either before or after bloom, or during both periods. On a dry weight basis, the carbohydrate content of leaves and stems of plants was highest when amount and frequency of irrigation was highest, but on the fresh weight basis, the carbohydrate content decreased with an increase in soil moisture. The stems and leaves of plants at the high moisture treatments contained highest levels of P and K while N and Mg levels of the same plants were lowest. A higher concentration of arginine was found in plants at high moisture levels than at low moisture levels. Tyrosine was detected in plants grown at the higher moisture, but not in plants subjected to moisture stress. Data suggest that soil moisture levels affected protein metabolism. Sucrose sprays had no significant effect on production of pods and carbohydrate content of bean plants. When soil temperature and moisture levels were varied, significant correlation co-efficients were obtained between weight of plants and number of pods, and between weight of plants and weight of pods. Data suggest that for highest yield, environmental factors should favor production of a large vigorous plant, with large photosynthetic capacity for bearing flowers and fruits. Bean plants appear to be especially sensitive to adverse temperature and moisture conditions during the period of anthesis and early pod development. Although adverse effects of high temperature and of moisture stress on pollination and fertilization were not studied, per se, in the present investigations, these adverse conditions caused a lower production of pods, lower carbohydrates levels, and appeared also to affect protein metabolism in snap beans. Further research is needed, especially to elucidate the adverse effects of high temperatures and moisture stress on biochemical processes and constituents of the snap bean and the significant relationship of these to growth, flowering, and fruiting. Title: Effects of modifying the environment on flowering, fruiting, and biochemical composition of the snap bean (Phaseolus vulgaris L.) Author: Singh, Jyotendra Narain The effects of modifying air temperature, soil temperature, and soil moisture levels on flowering, fruiting, and chemical composition of Tendercrop snap beans were studied in experiments in the field and in the greenhouse during 1961, 1962, and 1963. High maximum temperatures of 95-105° F. during bloom reduced the percent set and number and weight of pods of bean plants. Plants appeared to be most sensitive to temperatures at six to eight days after first bloom. Air temperatures in the field were increased 8-10° F. above controls by use of clear polyethylene plastic cages. The carbohydrate content of leaves and stems of plants subjected to high temperatures was decreased with a greater relative reduction of starch than of other sugars. Air temperature appeared also to affect the protein metabolism since cystine was not detected in plants subjected- to high temperature. Furthermore, threonine was detected in plants exposed to high temperatures, but not in control plants. Soil temperatures ranging from 55° to 90° F. had a pronounced effect on growth, flowering, and yield of snap beans, with best growth of plants and highest number of flowers and pods and weight of pods being obtained at soil temperatures of 75° to 80° F. Diurnal fluctuation of soil temperature had no advantage over comparable constant mean soil temperature for growth of plants. An exception was at fluctuating soil temperatures of 50-60° F- compared to constant temperature of 55° F. Soil temperature did not affect levels of total sugar and reducing sugar, but the starch content was decreased with an increase in soil temperature. Sucrose content of plants at fluctuating soil temperatures tended to be higher than in plants grown at comparable constant mean temperatures. Dry weight of shoots and roots and P and K content of plants increased with increased soil temperature. Magnesium content tended to decrease with an increase of soil temperature while Ca content of plants was variable. Snap bean plants which received the highest amount and frequency of irrigation from planting to harvest had the highest dry weight of shoots, number of flowers, percent set, and yield of pods when compared to plants subjected to moisture stress, either before or after bloom, or during both periods. On a dry weight basis, the carbohydrate content of leaves and stems of plants was highest when amount and frequency of irrigation was highest, but on the fresh weight basis, the carbohydrate content decreased with an increase in soil moisture. The stems and leaves of plants at the high moisture treatments contained highest levels of P and K while N and Mg levels of the same plants were lowest. A higher concentration of arginine was found in plants at high moisture levels than at low moisture levels. Tyrosine was detected in plants grown at the higher moisture, but not in plants subjected to moisture stress. Data suggest that soil moisture levels affected protein metabolism. Sucrose sprays had no significant effect on production of pods and carbohydrate content of bean plants. When soil temperature and moisture levels were varied, significant correlation co-efficients were obtained between weight of plants and number of pods, and between weight of plants and weight of pods. Data suggest that for highest yield, environmental factors should favor production of a large vigorous plant, with large photosynthetic capacity for bearing flowers and fruits. Bean plants appear to be especially sensitive to adverse temperature and moisture conditions during the period of anthesis and early pod development. Although adverse effects of high temperature and of moisture stress on pollination and fertilization were not studied, per se, in the present investigations, these adverse conditions caused a lower production of pods, lower carbohydrates levels, and appeared also to affect protein metabolism in snap beans. Further research is needed, especially to elucidate the adverse effects of high temperatures and moisture stress on biochemical processes and constituents of the snap bean and the significant relationship of these to growth, flowering, and fruiting. Close

• 17. [Article] The effects of thermal processing on the mechanical properties of AA2024, 2014 and 2618 aluminum alloys

  This study determined the independent effects of various homogenization cycles and precipitation treatments on the elevated temperature workability and the final ambient temperature mechanical properties ...

  Citation × Citation Citation Abstract Copy Title: The effects of thermal processing on the mechanical properties of AA2024, 2014 and 2618 aluminum alloys Author: Li, Xiao, 1963- This study determined the independent effects of various homogenization cycles and precipitation treatments on the elevated temperature workability and the final ambient temperature mechanical properties of AA2024 aluminum alloy and on the T3 tensile properties of 2014 aluminum alloy as well as T6 tensile properties of 2618 and 2618 (Curich) aluminum alloys. The elevated-temperature tensile and extrusion tests indicate that the workability of AA2024 alloy improves with elevated-temperature precipitation treatment as suggested by earlier investigations. The precipitation treatments do not appear to degrade the ambient-temperature T3 and T8 tensile properties. The time at the precipitation temperature appears to affect the T3 and T8 tensile properties in unextruded ingot, longer times especially providing both relatively high ambient-temperature strength and ductility of AA2024 alloy. The time at the standard homogenization temperature and the heat-up and cool-down rates do not dramatically affect the T3 tensile properties of unextruded ingot of AA2024 and 2014 alloys. However, long soak times at the homogenization temperature and more rapid cooling rates may improve the properties somewhat of AA2024 alloy and longer heat-up times and rapid cooling rates may slightly improve the properties of 2014 alloy. The higher standard solution temperature appears to increase both strength and ductility of 2014 alloy over lower temperatures. The homogenization temperature affects the T6 tensile properties of 2618 and 2618 (Cu-rich) alloys, a high homogenization temperature (compare to standard homogenization temperature) providing both high strength and ductility. Increased manganese and copper appears to increase the strength, but slightly decreases the ductility. The standard aging temperature and time produce higher strength but lower the ductility than lower temperatures at the same or shorter aging times in 2618 (Cu-rich) alloy. Title: The effects of thermal processing on the mechanical properties of AA2024, 2014 and 2618 aluminum alloys Author: Li, Xiao, 1963- This study determined the independent effects of various homogenization cycles and precipitation treatments on the elevated temperature workability and the final ambient temperature mechanical properties of AA2024 aluminum alloy and on the T3 tensile properties of 2014 aluminum alloy as well as T6 tensile properties of 2618 and 2618 (Curich) aluminum alloys. The elevated-temperature tensile and extrusion tests indicate that the workability of AA2024 alloy improves with elevated-temperature precipitation treatment as suggested by earlier investigations. The precipitation treatments do not appear to degrade the ambient-temperature T3 and T8 tensile properties. The time at the precipitation temperature appears to affect the T3 and T8 tensile properties in unextruded ingot, longer times especially providing both relatively high ambient-temperature strength and ductility of AA2024 alloy. The time at the standard homogenization temperature and the heat-up and cool-down rates do not dramatically affect the T3 tensile properties of unextruded ingot of AA2024 and 2014 alloys. However, long soak times at the homogenization temperature and more rapid cooling rates may improve the properties somewhat of AA2024 alloy and longer heat-up times and rapid cooling rates may slightly improve the properties of 2014 alloy. The higher standard solution temperature appears to increase both strength and ductility of 2014 alloy over lower temperatures. The homogenization temperature affects the T6 tensile properties of 2618 and 2618 (Cu-rich) alloys, a high homogenization temperature (compare to standard homogenization temperature) providing both high strength and ductility. Increased manganese and copper appears to increase the strength, but slightly decreases the ductility. The standard aging temperature and time produce higher strength but lower the ductility than lower temperatures at the same or shorter aging times in 2618 (Cu-rich) alloy. Close

• 18. [Article] Contributions of riparian vegetation and stream morphology to headwater stream temperature patterns in the Oregon Coast Range

  The role of riparian forests in maintaining temperatures of headwater streams is well established and is a foundation of forest practice rules designed to protect streamwater quality. However, detailed ...

  Citation × Citation Citation Abstract Copy Title: Contributions of riparian vegetation and stream morphology to headwater stream temperature patterns in the Oregon Coast Range Author: Smith, Danielle D. The role of riparian forests in maintaining temperatures of headwater streams is well established and is a foundation of forest practice rules designed to protect streamwater quality. However, detailed investigation is still needed quantifying specific characteristics of stream systems that affect streamwater temperature including riparian features, stream morphology, and subsurface interactions. The objectives of this research were to investigate summertime streamwater temperature patterns and identify characteristics within headwater streams and riparian zones that influence stream temperature. This study was designed to evaluate these relationships prior to logging in 38 perennial headwater catchments of the Oregon Coast Range. Stream reaches of greater than 1000 m were instrumented with temperature probes and selected stream and riparian characteristics were measured at 60-m intervals within each study reach in 2002 and 2003. A subset of the streams was examined in 2003 to determine the potential influence of streamwater residence time on temperature patterns. Findings suggest that canopy cover is the driving factor controlling summer stream temperature in these small headwater streams, but other stream and riparian characteristics should not be discarded. Longitudinal stream temperature patterns were quite variable for these forested streams and results suggest a high degree of complexity in small headwater streams. Maximum 7-day moving average temperatures ranged from 11.4°C to 16.8°C, with three streams above the standard 16°C threshold. Effects of stream and riparian characteristics on stream temperature were strongest when average of the weekly high temperature was assessed, suggesting this may be a more sensitive index of stream temperature than the commonly used maximum 7-day moving average. Results of tracer dilution tests were inconclusive in that temperature was not consistently correlated to residence time in streams. Title: Contributions of riparian vegetation and stream morphology to headwater stream temperature patterns in the Oregon Coast Range Author: Smith, Danielle D. The role of riparian forests in maintaining temperatures of headwater streams is well established and is a foundation of forest practice rules designed to protect streamwater quality. However, detailed investigation is still needed quantifying specific characteristics of stream systems that affect streamwater temperature including riparian features, stream morphology, and subsurface interactions. The objectives of this research were to investigate summertime streamwater temperature patterns and identify characteristics within headwater streams and riparian zones that influence stream temperature. This study was designed to evaluate these relationships prior to logging in 38 perennial headwater catchments of the Oregon Coast Range. Stream reaches of greater than 1000 m were instrumented with temperature probes and selected stream and riparian characteristics were measured at 60-m intervals within each study reach in 2002 and 2003. A subset of the streams was examined in 2003 to determine the potential influence of streamwater residence time on temperature patterns. Findings suggest that canopy cover is the driving factor controlling summer stream temperature in these small headwater streams, but other stream and riparian characteristics should not be discarded. Longitudinal stream temperature patterns were quite variable for these forested streams and results suggest a high degree of complexity in small headwater streams. Maximum 7-day moving average temperatures ranged from 11.4°C to 16.8°C, with three streams above the standard 16°C threshold. Effects of stream and riparian characteristics on stream temperature were strongest when average of the weekly high temperature was assessed, suggesting this may be a more sensitive index of stream temperature than the commonly used maximum 7-day moving average. Results of tracer dilution tests were inconclusive in that temperature was not consistently correlated to residence time in streams. Close

• 19. [Article] Monitoring Restoration in South Sister Creek : The Effect of Stream Enhancement Structures on Water Temperature

  This pilot study of South Sister Creek (8 km length) examined stream-scale (i.e., longitudinal trends) and sub-reach scale (less than 100 m) water temperature. Hourly summer temperature time-series data ...

  Citation × Citation Citation Abstract Copy Title: Monitoring Restoration in South Sister Creek : The Effect of Stream Enhancement Structures on Water Temperature Author: Harewood, Alessandra Greer This pilot study of South Sister Creek (8 km length) examined stream-scale (i.e., longitudinal trends) and sub-reach scale (less than 100 m) water temperature. Hourly summer temperature time-series data were gathered at four to seven locations along South Sister Creek in 2006, 2012, and 2013 and were used to explore whether restoration projects (in 2007 to 2011) affected stream temperature. Calculated seven-day maximum temperatures were cooler in post-treatment years (2012 and 2013) than the pre-treatment year (2006) at all four multi-year sites with the greatest differences near the mouth of the creek (4 to 5ºC cooler). While median stream temperature values were highest in 2013 for all four of the multi-year sites, the upper quartiles of measured hourly temperature for 2006 compared to 2012 and 2013 indicated more extreme high temperatures in 2006 than in subsequent years. Cross-correlation between stream and air temperature were used as an indicator of hyporheic flow. All peak CCF coefficients indicated a strong (.70) positive correlation in the early summer period between air and stream temperature, with lags ranging from 3 to 6 hours between peak air temperature and peak stream temperature. In the late summer period, most sites demonstrated lower correlations and longer lag times, patterns consistent with greater groundwater influence during low summer flows. There was no observable difference between pre- and post-treatment air-stream temperature cross correlation relationships. At a sub-reach scale, sites with more in-stream structural complexity -- including designed structures -- displayed greater spatial temperature variability than bedrock dominated reaches with simpler geomorphology. Title: Monitoring Restoration in South Sister Creek : The Effect of Stream Enhancement Structures on Water Temperature Author: Harewood, Alessandra Greer This pilot study of South Sister Creek (8 km length) examined stream-scale (i.e., longitudinal trends) and sub-reach scale (less than 100 m) water temperature. Hourly summer temperature time-series data were gathered at four to seven locations along South Sister Creek in 2006, 2012, and 2013 and were used to explore whether restoration projects (in 2007 to 2011) affected stream temperature. Calculated seven-day maximum temperatures were cooler in post-treatment years (2012 and 2013) than the pre-treatment year (2006) at all four multi-year sites with the greatest differences near the mouth of the creek (4 to 5ºC cooler). While median stream temperature values were highest in 2013 for all four of the multi-year sites, the upper quartiles of measured hourly temperature for 2006 compared to 2012 and 2013 indicated more extreme high temperatures in 2006 than in subsequent years. Cross-correlation between stream and air temperature were used as an indicator of hyporheic flow. All peak CCF coefficients indicated a strong (.70) positive correlation in the early summer period between air and stream temperature, with lags ranging from 3 to 6 hours between peak air temperature and peak stream temperature. In the late summer period, most sites demonstrated lower correlations and longer lag times, patterns consistent with greater groundwater influence during low summer flows. There was no observable difference between pre- and post-treatment air-stream temperature cross correlation relationships. At a sub-reach scale, sites with more in-stream structural complexity -- including designed structures -- displayed greater spatial temperature variability than bedrock dominated reaches with simpler geomorphology. Close

• 20. [Article] The effect of cold acclimation on the temperature preference of the goldfish, Carassius auratus, and the brown bullhead, Ictalurus nebulosus

  Two species of fish, Carassius auratus and Ictalurus nebulosus, were subjected to cold acclimation regimes. Acclimation temperatures were slowly lowered to 3°c, then held for a period of time. At various ...

  Citation × Citation Citation Abstract Copy Title: The effect of cold acclimation on the temperature preference of the goldfish, Carassius auratus, and the brown bullhead, Ictalurus nebulosus Author: Lord, Alfred Year: 1987 Two species of fish, Carassius auratus and Ictalurus nebulosus, were subjected to cold acclimation regimes. Acclimation temperatures were slowly lowered to 3°c, then held for a period of time. At various times during this regime, fish were taken out and allowed to spend time in a temperature gradient to determine their preferred temperatures. Carassius were left in the gradient just long enough to determine a measure of the acute temperature preference, while Ictalurus were left in the temperature gradient for longer periods of time to observe any changes that might occur as the fish adjusted to selected temperatures. In both species of fish, lower acclimation temperatures and increased time spent at low temperatures caused a preference for lower temperatures in the gradient. Title: The effect of cold acclimation on the temperature preference of the goldfish, Carassius auratus, and the brown bullhead, Ictalurus nebulosus Author: Lord, Alfred Year: 1987 Two species of fish, Carassius auratus and Ictalurus nebulosus, were subjected to cold acclimation regimes. Acclimation temperatures were slowly lowered to 3°c, then held for a period of time. At various times during this regime, fish were taken out and allowed to spend time in a temperature gradient to determine their preferred temperatures. Carassius were left in the gradient just long enough to determine a measure of the acute temperature preference, while Ictalurus were left in the temperature gradient for longer periods of time to observe any changes that might occur as the fish adjusted to selected temperatures. In both species of fish, lower acclimation temperatures and increased time spent at low temperatures caused a preference for lower temperatures in the gradient. Close

• 21. [Article] Heat source : stream, river and open channel temperature prediction

  Reach defined analysis concentrated on the water temperature change that occurred in a stream/river segment over the course of one full diurnal cycle. Digital thermistors, data loggers and computer model ...

  Citation × Citation Citation Abstract Copy Title: Heat source : stream, river and open channel temperature prediction Author: Boyd, Matthew S. Reach defined analysis concentrated on the water temperature change that occurred in a stream/river segment over the course of one full diurnal cycle. Digital thermistors, data loggers and computer model development were utilized in reach analysis to link parameters of the stream system to a specific temperature change. The methodology employed was relatively simple and fast, and many successive stream segments were analyzed simultaneously. Reach analysis of stream temperature change identified the existing components of the stream system that caused increased water temperature and predicted the effectiveness of managed improvements to the stream system. Stream and river temperature regulation has focused on system and basin wide management. Often, the source of increased water temperature originates in only a part of the stream system. Reach defined analysis identified the portions of the stream system in which most water temperature change occurred, offered an explanation for the temperature response and provided specific information about the alternate strategies that may ameliorate undesired water temperatures. The development of the computer model Heat Source included physically based mathematical descriptions of stream energy and hydrologic processes. An implicit finite difference numerical method was implemented for simultaneous solution. The methodology presented in Heat Source is portable and applicable to all streams, rivers and open channels. Title: Heat source : stream, river and open channel temperature prediction Author: Boyd, Matthew S. Reach defined analysis concentrated on the water temperature change that occurred in a stream/river segment over the course of one full diurnal cycle. Digital thermistors, data loggers and computer model development were utilized in reach analysis to link parameters of the stream system to a specific temperature change. The methodology employed was relatively simple and fast, and many successive stream segments were analyzed simultaneously. Reach analysis of stream temperature change identified the existing components of the stream system that caused increased water temperature and predicted the effectiveness of managed improvements to the stream system. Stream and river temperature regulation has focused on system and basin wide management. Often, the source of increased water temperature originates in only a part of the stream system. Reach defined analysis identified the portions of the stream system in which most water temperature change occurred, offered an explanation for the temperature response and provided specific information about the alternate strategies that may ameliorate undesired water temperatures. The development of the computer model Heat Source included physically based mathematical descriptions of stream energy and hydrologic processes. An implicit finite difference numerical method was implemented for simultaneous solution. The methodology presented in Heat Source is portable and applicable to all streams, rivers and open channels. Close

• 22. [Article] Small-Scale Sea Surface Temperature Structure

  Observations of sea surface temperature and wave height were made from a large, manned spar buoy (R/P FLIP) ~100 km off the coast of Baja California. Surface temperature was measured with a radiation thermometer ...

  Citation × Citation Citation Abstract Copy Title: Small-Scale Sea Surface Temperature Structure Author: Paulson, Clayton A., Simpson, James J. Observations of sea surface temperature and wave height were made from a large, manned spar buoy (R/P FLIP) ~100 km off the coast of Baja California. Surface temperature was measured with a radiation thermometer which viewed a disc on the surface 12 cm in diameter. The instrument responded to frequencies up to 3 Hz. Wave height was measured with a resistance gage located close to the field of view of the radiometer. Log-log plots of spectra of sea surface temperature exhibit a plateau between 0.05 and 0.5 Hz, followed by a rapid decrease in energy at frequencies >1 Hz. A coherence of 0.5 between waves and surface temperature occurs at the same frequency as the peak in the wave spectrum. Phase spectra show that warm temperatures associated with the thinning of the surface viscous layer occur systematically upwind of the crests of the dominant gravity waves and downwind of the crests of steeply sloping, shorter period gravity waves. The warm temperatures are hypothesized to be caused by enhanced wind stress upwind from the crests and by surface instability and surface convergence downwind from the crests. The magnitude of the mean temperature difference between the surface and the warmer, well-mixed water below is estimated from the surface temperature record. It is assumed that the warmest surface temperatures observed are associated with thinning of the viscous layer and are representative of the well-mixed water below. The dimensionless constant in a formula due to Saunders (1967), which relates the temperature difference to wind stress and heat flux, is found to be seven. Title: Small-Scale Sea Surface Temperature Structure Author: Paulson, Clayton A., Simpson, James J. Observations of sea surface temperature and wave height were made from a large, manned spar buoy (R/P FLIP) ~100 km off the coast of Baja California. Surface temperature was measured with a radiation thermometer which viewed a disc on the surface 12 cm in diameter. The instrument responded to frequencies up to 3 Hz. Wave height was measured with a resistance gage located close to the field of view of the radiometer. Log-log plots of spectra of sea surface temperature exhibit a plateau between 0.05 and 0.5 Hz, followed by a rapid decrease in energy at frequencies >1 Hz. A coherence of 0.5 between waves and surface temperature occurs at the same frequency as the peak in the wave spectrum. Phase spectra show that warm temperatures associated with the thinning of the surface viscous layer occur systematically upwind of the crests of the dominant gravity waves and downwind of the crests of steeply sloping, shorter period gravity waves. The warm temperatures are hypothesized to be caused by enhanced wind stress upwind from the crests and by surface instability and surface convergence downwind from the crests. The magnitude of the mean temperature difference between the surface and the warmer, well-mixed water below is estimated from the surface temperature record. It is assumed that the warmest surface temperatures observed are associated with thinning of the viscous layer and are representative of the well-mixed water below. The dimensionless constant in a formula due to Saunders (1967), which relates the temperature difference to wind stress and heat flux, is found to be seven. Close

• 23. [Article] The Effect of Temperature on the Survival of Chinook Eggs and Fry

  Temperature data from above and below the Cougar Dam collected by the U.S. Geological Survey prior to the construction of the temperature control structure was analyzed to determine how the di®ering temperature ...

  Citation × Citation Citation Abstract Copy Title: The Effect of Temperature on the Survival of Chinook Eggs and Fry Author: Teose, Maarika Temperature data from above and below the Cougar Dam collected by the U.S. Geological Survey prior to the construction of the temperature control structure was analyzed to determine how the di®ering temperature regimes a®ect the growth and survival of threatened spring- run Chinook salmon. An ARIMA time-series model was used to approximate each temperature record and a MATLAB program was written to simulate the growth of an individual Chinook salmon from egg to fry. Given a spawning distribution, the model was used to grow several hundred ¯sh in each temperature regime for a given period of time, and the distributions of ¯sh weights were recorded in histograms. The distributions of ¯sh weights above and below the dam were signi¯cantly di®erent (p < 0:001) and the temperature regime above the dam produced larger ¯sh than the temperature regime below the dam (p < 0:001). We conclude that the temperature regime below the dam (prior to the construction of the temperature control structure) is less conducive to the survival of Chinook than the temperature regime above. Title: The Effect of Temperature on the Survival of Chinook Eggs and Fry Author: Teose, Maarika Temperature data from above and below the Cougar Dam collected by the U.S. Geological Survey prior to the construction of the temperature control structure was analyzed to determine how the di®ering temperature regimes a®ect the growth and survival of threatened spring- run Chinook salmon. An ARIMA time-series model was used to approximate each temperature record and a MATLAB program was written to simulate the growth of an individual Chinook salmon from egg to fry. Given a spawning distribution, the model was used to grow several hundred ¯sh in each temperature regime for a given period of time, and the distributions of ¯sh weights were recorded in histograms. The distributions of ¯sh weights above and below the dam were signi¯cantly di®erent (p < 0:001) and the temperature regime above the dam produced larger ¯sh than the temperature regime below the dam (p < 0:001). We conclude that the temperature regime below the dam (prior to the construction of the temperature control structure) is less conducive to the survival of Chinook than the temperature regime above. Close

• 24. [Article] Water temperature prediction and control study, Umpqua River Basin

  Tiller Reservoir In an average year the reservoir is capable of holding water temperatures in South Umpqua River below 70° F. for a wide range of regulation schedules. In a year of maximum temperature, ...

  Citation × Citation Citation Abstract Copy Title: Water temperature prediction and control study, Umpqua River Basin Author: Delay, William H. Tiller Reservoir In an average year the reservoir is capable of holding water temperatures in South Umpqua River below 70° F. for a wide range of regulation schedules. In a year of maximum temperature, it will also hold temperatures below 700 F. but flexibility of operation will be restricted. Regulations designed to control water temperatures in South Umpqua River will have no significant influence on water temperatures in the main stem of the Umpqua River because of the large volume contributed by the unregulated North Umpqua River. Galesville Reservoir The reservoir has the capability to hold water temperatures in Cow Creek below 70° F. in an average year provided nearly the entire storage capacity is regulated for temperature control. In a year of maximum temperature, only about one-half of the length of Cow Creek below the reservoir can be held below 70° F. for the entire summer. Hinkle Reservoir The reservoir is capable of holding water temperatures in Calapooya Creek below 70° F. for all meteorological conditions. Substantial flexibility of reservoir regulation will be available in average years. Title: Water temperature prediction and control study, Umpqua River Basin Author: Delay, William H. Tiller Reservoir In an average year the reservoir is capable of holding water temperatures in South Umpqua River below 70° F. for a wide range of regulation schedules. In a year of maximum temperature, it will also hold temperatures below 700 F. but flexibility of operation will be restricted. Regulations designed to control water temperatures in South Umpqua River will have no significant influence on water temperatures in the main stem of the Umpqua River because of the large volume contributed by the unregulated North Umpqua River. Galesville Reservoir The reservoir has the capability to hold water temperatures in Cow Creek below 70° F. in an average year provided nearly the entire storage capacity is regulated for temperature control. In a year of maximum temperature, only about one-half of the length of Cow Creek below the reservoir can be held below 70° F. for the entire summer. Hinkle Reservoir The reservoir is capable of holding water temperatures in Calapooya Creek below 70° F. for all meteorological conditions. Substantial flexibility of reservoir regulation will be available in average years. Close

• 25. [Article] Long-term tracking of climate change by underground temperatures

  Copyrighted by American Geophysical Union.

  Citation × Citation Citation Abstract Copy Title: Long-term tracking of climate change by underground temperatures Author: Harris, Robert N., Ferguson, Grant, Beltrami, Hugo Copyrighted by American Geophysical Union. Title: Long-term tracking of climate change by underground temperatures Author: Harris, Robert N., Ferguson, Grant, Beltrami, Hugo Copyrighted by American Geophysical Union. Close

• 26. [Article] The effect of ultra-high pressure on the emf of thermocouples

  The effect of ultra-high pressure on the thermal emf of a chromelialumel thermocouple is investigated using an indirect method which does not require a direct knowledge of the temperature of the pressurized ...

  Citation × Citation Citation Abstract Copy Title: The effect of ultra-high pressure on the emf of thermocouples Author: Eide, Stuart Ames The effect of ultra-high pressure on the thermal emf of a chromelialumel thermocouple is investigated using an indirect method which does not require a direct knowledge of the temperature of the pressurized junction. The unknown temperature is written parametrically as a function of a directly measured quantity, the electrical power delivered to the internal furnace. The emf of the pressurized thermocouple is then written as a function of the temperature and a set of unknown coefficients. Combining the two functions to eliminate the unknown junction temperature, the pressurized emf is given as a function of the furnace power. The coefficients of both the temperature-versus-power function and the pressure-corrected emfver sus -temperature function are then obtained simultaneously by per forming a nonlinear least-squares fit to the directly measured emfversus -furnace power data. Results for the temperature correction due to pressure are compared with estimates obtained by other methods for pressures between 25.0 kbar and 60.6 kbar and temperatures up to approximately 900°C. Title: The effect of ultra-high pressure on the emf of thermocouples Author: Eide, Stuart Ames The effect of ultra-high pressure on the thermal emf of a chromelialumel thermocouple is investigated using an indirect method which does not require a direct knowledge of the temperature of the pressurized junction. The unknown temperature is written parametrically as a function of a directly measured quantity, the electrical power delivered to the internal furnace. The emf of the pressurized thermocouple is then written as a function of the temperature and a set of unknown coefficients. Combining the two functions to eliminate the unknown junction temperature, the pressurized emf is given as a function of the furnace power. The coefficients of both the temperature-versus-power function and the pressure-corrected emfver sus -temperature function are then obtained simultaneously by per forming a nonlinear least-squares fit to the directly measured emfversus -furnace power data. Results for the temperature correction due to pressure are compared with estimates obtained by other methods for pressures between 25.0 kbar and 60.6 kbar and temperatures up to approximately 900°C. Close

• 27. [Article] A study of stream temperature using distributed temperature sensing fiber optics technology in Big Boulder Creek, a tributary to the Middle Fork John Day River in eastern Oregon

  Citation × Citation Citation Abstract Copy Title: A study of stream temperature using distributed temperature sensing fiber optics technology in Big Boulder Creek, a tributary to the Middle Fork John Day River in eastern Oregon Author: Arik, Aida D. Title: A study of stream temperature using distributed temperature sensing fiber optics technology in Big Boulder Creek, a tributary to the Middle Fork John Day River in eastern Oregon Author: Arik, Aida D. Close

• 28. [Article] Temperature Monitoring and Modeling of the Mary's River Watershed

  Abstract -- Stream temperatures were monitored at 42 sites in the summer of 1998 and at 26 sites in the summer of 1999 throughout the Mary's River watershed. Segments of streams were identified where reduced ...

  Citation × Citation Citation Abstract Copy Title: Temperature Monitoring and Modeling of the Mary's River Watershed Abstract -- Stream temperatures were monitored at 42 sites in the summer of 1998 and at 26 sites in the summer of 1999 throughout the Mary's River watershed. Segments of streams were identified where reduced temperatures would benefit native cutthroat trout. Computer modeling of riparian shade enhancement predicted temperature reductions. Title: Temperature Monitoring and Modeling of the Mary's River Watershed Abstract -- Stream temperatures were monitored at 42 sites in the summer of 1998 and at 26 sites in the summer of 1999 throughout the Mary's River watershed. Segments of streams were identified where reduced temperatures would benefit native cutthroat trout. Computer modeling of riparian shade enhancement predicted temperature reductions. Close

• 29. [Article] Growth and food consumption of juvenile coho salmon exposed to natural and elevated fluctuating temperatures

  The growth and food consumption of juvenile coho salmon [Oncorhynchus kisutch (Walbaum)] exposed to natural and elevated fluctuating temperatures were studied in the laboratory with wild fish collected ...

  Citation × Citation Citation Abstract Copy Title: Growth and food consumption of juvenile coho salmon exposed to natural and elevated fluctuating temperatures Author: Everson, Larry B. The growth and food consumption of juvenile coho salmon [Oncorhynchus kisutch (Walbaum)] exposed to natural and elevated fluctuating temperatures were studied in the laboratory with wild fish collected from a salmonid rearing stream. Control temperatures were similar to the temperature regime of a natural stream and the elevated temperatures were increased incrementally 3-4 C and 7-8 C. Short-term, 30-day experiments were conducted during five different seasonal periods in 1969 and 1970. Concurrent long-term studies were carried out during the entire experimental period. Relationships between rates of food consumption, growth and food assimilation of the fish were determined for the different experimental temperature conditions during the short-term experiments. Relationships between maintenance ration and temperature were derived from curves relating rates of food consumption and growth. The efficiency of food assimilation was determined from measurements of the quantities of the food consumed and the amounts of fecal wastes produced. Caloric measurements were obtained from oxygen bomb calorimetry of the fish and food consumed, and from wet combustion of the fecal wastes collected during short intervals within each experiment. Bioenergetic measurements were used to estimate the major fates of the energy of food consumed under the different temperature conditions during a period of fluctuating high summer temperatures. Long-term studies were conducted over eight-month and four-month periods under temperature conditions similar to those of the short-term experiments. Growth rates of the juvenile coho salmon were obtained from measurement of changes in their wet weight during 15-day intervals. The growth rates of salmon at equivalent ration levels were compared between the short- and long-term experiments. Growth rates of juvenile coho salmon kept as controls were generally greater than those of fish exposed to elevated temperatures for each of the five short-term experiments. Increases of ration size generally ameliorated the effects of elevated temperatures on the salmon growth rates. Comparisons of the caloric values of coho salmon recorded for a natural rearing stream with those of experimentally fed fish suggest that wild fish subsist on a restricted ration. Results of the long-term studies showed that salmon exposed to naturally fluctuating temperatures in the laboratory and fed restricted rations reached sizes typical of downstream smolts in Oregon coastal streams, whereas the fish exposed to incremental temperature increases of 3-4 C and 7-8 C were respectively 25 and 47 percent smaller than the control fish. Comparison of results of studies based upon naturally fluctuating temperatures with those of other workers based upon constant temperatures indicates that at average temperatures above 20 C the fluctuation of temperature is favorable for coho salmon growth. The results of the study suggest that temperature criteria for juvenile coho salmon derived from measurements based upon constant temperatures may not be satisfactory for protecting the fish during the extended period of their freshwater existence. Measurements of the growth of the young salmon during long-term experiments indicated that any substantial increases of temperature would result in a reduction in the size of smolts. Significant reductions of juvenile salmon growth resulting from elevated stream temperatures could influence the production of salmon populations through decreased marine survival. Long-term studies of the fish as well as other components of stream communities influenced by elevated temperatures are necessary for establishing meaningful temperature criteria. Title: Growth and food consumption of juvenile coho salmon exposed to natural and elevated fluctuating temperatures Author: Everson, Larry B. The growth and food consumption of juvenile coho salmon [Oncorhynchus kisutch (Walbaum)] exposed to natural and elevated fluctuating temperatures were studied in the laboratory with wild fish collected from a salmonid rearing stream. Control temperatures were similar to the temperature regime of a natural stream and the elevated temperatures were increased incrementally 3-4 C and 7-8 C. Short-term, 30-day experiments were conducted during five different seasonal periods in 1969 and 1970. Concurrent long-term studies were carried out during the entire experimental period. Relationships between rates of food consumption, growth and food assimilation of the fish were determined for the different experimental temperature conditions during the short-term experiments. Relationships between maintenance ration and temperature were derived from curves relating rates of food consumption and growth. The efficiency of food assimilation was determined from measurements of the quantities of the food consumed and the amounts of fecal wastes produced. Caloric measurements were obtained from oxygen bomb calorimetry of the fish and food consumed, and from wet combustion of the fecal wastes collected during short intervals within each experiment. Bioenergetic measurements were used to estimate the major fates of the energy of food consumed under the different temperature conditions during a period of fluctuating high summer temperatures. Long-term studies were conducted over eight-month and four-month periods under temperature conditions similar to those of the short-term experiments. Growth rates of the juvenile coho salmon were obtained from measurement of changes in their wet weight during 15-day intervals. The growth rates of salmon at equivalent ration levels were compared between the short- and long-term experiments. Growth rates of juvenile coho salmon kept as controls were generally greater than those of fish exposed to elevated temperatures for each of the five short-term experiments. Increases of ration size generally ameliorated the effects of elevated temperatures on the salmon growth rates. Comparisons of the caloric values of coho salmon recorded for a natural rearing stream with those of experimentally fed fish suggest that wild fish subsist on a restricted ration. Results of the long-term studies showed that salmon exposed to naturally fluctuating temperatures in the laboratory and fed restricted rations reached sizes typical of downstream smolts in Oregon coastal streams, whereas the fish exposed to incremental temperature increases of 3-4 C and 7-8 C were respectively 25 and 47 percent smaller than the control fish. Comparison of results of studies based upon naturally fluctuating temperatures with those of other workers based upon constant temperatures indicates that at average temperatures above 20 C the fluctuation of temperature is favorable for coho salmon growth. The results of the study suggest that temperature criteria for juvenile coho salmon derived from measurements based upon constant temperatures may not be satisfactory for protecting the fish during the extended period of their freshwater existence. Measurements of the growth of the young salmon during long-term experiments indicated that any substantial increases of temperature would result in a reduction in the size of smolts. Significant reductions of juvenile salmon growth resulting from elevated stream temperatures could influence the production of salmon populations through decreased marine survival. Long-term studies of the fish as well as other components of stream communities influenced by elevated temperatures are necessary for establishing meaningful temperature criteria. Close

• 30. [Article] ArikAidaD2011.pdf

  Citation × Citation Citation Abstract Copy Title: ArikAidaD2011.pdf Author: Arik, Aida D. Title: ArikAidaD2011.pdf Author: Arik, Aida D. Close

• 31. [Article] Appendix B - Data Collected 1-June 2008.zip

  Citation × Citation Citation Abstract Copy Title: Appendix B - Data Collected 1-June 2008.zip Author: Arik, Aida D. Title: Appendix B - Data Collected 1-June 2008.zip Author: Arik, Aida D. Close

• 32. [Article] Appendix B - Data Collected 2-Sept 2008.zip

  Citation × Citation Citation Abstract Copy Title: Appendix B - Data Collected 2-Sept 2008.zip Author: Arik, Aida D. Title: Appendix B - Data Collected 2-Sept 2008.zip Author: Arik, Aida D. Close

• 33. [Article] Appendix B - Data Collected 3-July 2009.zip

  Citation × Citation Citation Abstract Copy Title: Appendix B - Data Collected 3-July 2009.zip Author: Arik, Aida D. Title: Appendix B - Data Collected 3-July 2009.zip Author: Arik, Aida D. Close

• 34. [Article] Appendix B - Data Collected 4-Aug 2009.zip

  Citation × Citation Citation Abstract Copy Title: Appendix B - Data Collected 4-Aug 2009.zip Author: Arik, Aida D. Title: Appendix B - Data Collected 4-Aug 2009.zip Author: Arik, Aida D. Close

• 35. [Article] A study of wind, oceanic temperature and hydrography in the upwelling area off Peru

  Observations of sea temperature, wind and hydrography obtained during the three months' period of MAM 77 - CUEA experiment (JOINT-II) along the C-line, near 15°S are described. Wind and temperature observations ...

  Citation × Citation Citation Abstract Copy Title: A study of wind, oceanic temperature and hydrography in the upwelling area off Peru Author: Medina, Francisco A. Observations of sea temperature, wind and hydrography obtained during the three months' period of MAM 77 - CUEA experiment (JOINT-II) along the C-line, near 15°S are described. Wind and temperature observations made during March - May 1977 are compared to demonstrate that a relationship exists. Linear correlation analysis was performed on the temperature data and on the alongshore component of wind and wind stress. Auto-correlations and cross-correlations were computed for the temperature and wind. These analyses show that the alongshore fluctuations of the wind are very similar at the different stations, and the wind at each location was favorable for upwelling throughout the period of measurements. Temperature fluctuations in the near-surface, the nearshore and the near-bottom water over the shelf are coherent with temperature changes at a depth of 150 - 200 m over the upper slope. Temperature-wind analysis show that there is a good response of the near-surface temperature to the wind force. The time lag between the wind and the near-surface temperature was about 24 hours nearshore; the wind always led the temperature. Subsurface temperatures were not as well correlated with the alongshore wind, both negative and positive correlations were observed in this analysis, and the time lag between the wind and temperature was variable; on a few occasions the temperature led the wind. Vertical sections of sigma-t and temperature indicate the existence of conditions consistent with upwelling. Oscillation in the wind with periods of several days caused significant changes in the region inshore of 25 km. Title: A study of wind, oceanic temperature and hydrography in the upwelling area off Peru Author: Medina, Francisco A. Observations of sea temperature, wind and hydrography obtained during the three months' period of MAM 77 - CUEA experiment (JOINT-II) along the C-line, near 15°S are described. Wind and temperature observations made during March - May 1977 are compared to demonstrate that a relationship exists. Linear correlation analysis was performed on the temperature data and on the alongshore component of wind and wind stress. Auto-correlations and cross-correlations were computed for the temperature and wind. These analyses show that the alongshore fluctuations of the wind are very similar at the different stations, and the wind at each location was favorable for upwelling throughout the period of measurements. Temperature fluctuations in the near-surface, the nearshore and the near-bottom water over the shelf are coherent with temperature changes at a depth of 150 - 200 m over the upper slope. Temperature-wind analysis show that there is a good response of the near-surface temperature to the wind force. The time lag between the wind and the near-surface temperature was about 24 hours nearshore; the wind always led the temperature. Subsurface temperatures were not as well correlated with the alongshore wind, both negative and positive correlations were observed in this analysis, and the time lag between the wind and temperature was variable; on a few occasions the temperature led the wind. Vertical sections of sigma-t and temperature indicate the existence of conditions consistent with upwelling. Oscillation in the wind with periods of several days caused significant changes in the region inshore of 25 km. Close

• 36. [Article] A spatially explicit network-based model for estimating stream temperature distribution

  The WET-Temp (Watershed Evaluation Tool Temperature) model is designed to take advantage of spatially explicit datasets to predict stream temperature distribution. Datasets describing vegetation cover, ...

  Citation × Citation Citation Abstract Copy Title: A spatially explicit network-based model for estimating stream temperature distribution Author: Cox, Matthew M. The WET-Temp (Watershed Evaluation Tool Temperature) model is designed to take advantage of spatially explicit datasets to predict stream temperature distribution. Datasets describing vegetation cover, stream network locations, elevation and stream discharge are utilized by WET-Temp to quantify geometric relationships between the sun, stream channel and riparian areas. These relationships are used to estimate the energy gained or lost by the stream via various heat flux processes (solar and longwave radiation, evaporation, convection and advection). The sum of these processes is expressed as a differential energy balance equation applied at discrete locations across the stream network. The model describes diurnal temperature dynamics at each of these locations and thus temperature distribution across the entire network. WET-Temp is calibrated to a tributary of the South Santiam River in western Oregon, McDowell Creek. The mean differences between measured and modeled values in McDowell Creek were 0.6°C for daily maximum temperature and 1.3°C for daily minimum temperature. The model was then used to predict maximum and minimum temperatures in an adjacent tributary, Hamilton Creek. The mean differences between modeled and measured values in this paired basin were 1.8°C for daily maximum temperatures and 1.4°C for daily minimum temperatures. Influences of model parameters on modeled temperature distributions are explored in a sensitivity analysis. The ability of WET-Temp to utilize spatially explicit datasets in estimating temperature distributions across stream networks advances the state of the art in modeling stream temperature. Title: A spatially explicit network-based model for estimating stream temperature distribution Author: Cox, Matthew M. The WET-Temp (Watershed Evaluation Tool Temperature) model is designed to take advantage of spatially explicit datasets to predict stream temperature distribution. Datasets describing vegetation cover, stream network locations, elevation and stream discharge are utilized by WET-Temp to quantify geometric relationships between the sun, stream channel and riparian areas. These relationships are used to estimate the energy gained or lost by the stream via various heat flux processes (solar and longwave radiation, evaporation, convection and advection). The sum of these processes is expressed as a differential energy balance equation applied at discrete locations across the stream network. The model describes diurnal temperature dynamics at each of these locations and thus temperature distribution across the entire network. WET-Temp is calibrated to a tributary of the South Santiam River in western Oregon, McDowell Creek. The mean differences between measured and modeled values in McDowell Creek were 0.6°C for daily maximum temperature and 1.3°C for daily minimum temperature. The model was then used to predict maximum and minimum temperatures in an adjacent tributary, Hamilton Creek. The mean differences between modeled and measured values in this paired basin were 1.8°C for daily maximum temperatures and 1.4°C for daily minimum temperatures. Influences of model parameters on modeled temperature distributions are explored in a sensitivity analysis. The ability of WET-Temp to utilize spatially explicit datasets in estimating temperature distributions across stream networks advances the state of the art in modeling stream temperature. Close

• 37. [Article] Drop it like it’s Hot : Combining DTS and Temperature Modeling to Evaluate Stream Restoration on the Middle Fork of the John Day River

  Temperature is a key factor for salmonid health and is an important restoration metric on the Middle Fork of the John Day River in northeast Oregon. In the past century, dredge mining, deforestation, and ...

  Citation × Citation Citation Abstract Copy Title: Drop it like it’s Hot : Combining DTS and Temperature Modeling to Evaluate Stream Restoration on the Middle Fork of the John Day River Author: Hall, Austin (Austin Garrett) Temperature is a key factor for salmonid health and is an important restoration metric on the Middle Fork of the John Day River in northeast Oregon. In the past century, dredge mining, deforestation, and overgrazing have degraded stream habitat and resulted in greater daytime stream temperatures in the region. Recent restoration efforts have focused on mitigating these anthropogenic disturbances by reestablishing floodplain connections, replanting riparian vegetation, and improving instream habitat features and sediment. To evaluate these restoration projects, the Middle Fork of the John Day River was designated as an intensively monitored watershed in 2008, setting the stage for a 10-year temperature monitoring study. Temperatures measured during the summers of 2013 and 2014 add to the wealth of high resolution distributed temperature sensing (DTS) data collected by Oregon State University and serve as the first post-restoration data for a 2012 restoration project. Utilizing these data in coordination with the model, Heat Source, temperature change from two large restoration projects was quantified. Results from the study emphasize the significance of stream area and riparian vegetation on stream temperatures on the Middle Fork. Phase 2 of the Oxbow Tailings Restoration, completed in 2012, filled over a channel used for past dredge mining activities, reducing stream surface area and restoring the bifurcated channel to its historic south path. Findings show that this project has buffered daily stream temperatures, leading to decreases in maximum and daytime temperatures and increases in nightly temperatures for early August. Maximum and afternoon temperatures were shown to decrease by 0.65 °C and 0.91 °C, respectively, while nightly temperatures increased 0.85 °C. Continuing immediately downstream of the Phase 2 project, Phase 3 is currently in its final stages of construction. Objectives of Phase 3 seek to increase stream meanders, restore vegetation, and reconnect the stream to the adjacent valley and Ruby Creek tributary. Projecting future temperatures shows that the longer, wider restored channel increases afternoon temperature by 0.53 °C. Unlike Phase 2, changes to maximum and nightly temperatures were negligable. Altering the design width and vegetation for the restored channel revealed strong linear correlations to stream temperature, providing a simple tool that can be used to estimate temperature difference for future areal and shading scenarios. Title: Drop it like it’s Hot : Combining DTS and Temperature Modeling to Evaluate Stream Restoration on the Middle Fork of the John Day River Author: Hall, Austin (Austin Garrett) Temperature is a key factor for salmonid health and is an important restoration metric on the Middle Fork of the John Day River in northeast Oregon. In the past century, dredge mining, deforestation, and overgrazing have degraded stream habitat and resulted in greater daytime stream temperatures in the region. Recent restoration efforts have focused on mitigating these anthropogenic disturbances by reestablishing floodplain connections, replanting riparian vegetation, and improving instream habitat features and sediment. To evaluate these restoration projects, the Middle Fork of the John Day River was designated as an intensively monitored watershed in 2008, setting the stage for a 10-year temperature monitoring study. Temperatures measured during the summers of 2013 and 2014 add to the wealth of high resolution distributed temperature sensing (DTS) data collected by Oregon State University and serve as the first post-restoration data for a 2012 restoration project. Utilizing these data in coordination with the model, Heat Source, temperature change from two large restoration projects was quantified. Results from the study emphasize the significance of stream area and riparian vegetation on stream temperatures on the Middle Fork. Phase 2 of the Oxbow Tailings Restoration, completed in 2012, filled over a channel used for past dredge mining activities, reducing stream surface area and restoring the bifurcated channel to its historic south path. Findings show that this project has buffered daily stream temperatures, leading to decreases in maximum and daytime temperatures and increases in nightly temperatures for early August. Maximum and afternoon temperatures were shown to decrease by 0.65 °C and 0.91 °C, respectively, while nightly temperatures increased 0.85 °C. Continuing immediately downstream of the Phase 2 project, Phase 3 is currently in its final stages of construction. Objectives of Phase 3 seek to increase stream meanders, restore vegetation, and reconnect the stream to the adjacent valley and Ruby Creek tributary. Projecting future temperatures shows that the longer, wider restored channel increases afternoon temperature by 0.53 °C. Unlike Phase 2, changes to maximum and nightly temperatures were negligable. Altering the design width and vegetation for the restored channel revealed strong linear correlations to stream temperature, providing a simple tool that can be used to estimate temperature difference for future areal and shading scenarios. Close

• 38. [Article] Internal Temperature of Douglas-Fir Buds is Altered at Elevated Temperature

  Pseudotsuga menziesii (Douglas-fir) saplings were grown in sun-lit controlled environment chambers at ambient or elevated (4°C above ambient) temperature. We measured internal temperatures of vegetative ...

  Citation × Citation Citation Abstract Copy Title: Internal Temperature of Douglas-Fir Buds is Altered at Elevated Temperature Author: Apple, Martha E., Lucash, Melissa S., Olszyk, David M., Tingey, David T., Phillips, Donald L. Year: 1999 Pseudotsuga menziesii (Douglas-fir) saplings were grown in sun-lit controlled environment chambers at ambient or elevated (4°C above ambient) temperature. We measured internal temperatures of vegetative buds with thermocouple probes and compared temperatures of normal buds and abnormal buds with loosened, rosetted outer scales in elevated temperature chambers. The abnormal buds had higher and earlier peak daily temperatures than normal buds. Elevated temperature may influence the internal temperature of buds and contribute to the development of abnormal, rosetted buds with loosened outer scales. Abnormal bud development may alter branching patterns and allometry of Douglas-fir trees subjected to climatic change. Title: Internal Temperature of Douglas-Fir Buds is Altered at Elevated Temperature Author: Apple, Martha E., Lucash, Melissa S., Olszyk, David M., Tingey, David T., Phillips, Donald L. Year: 1999 Pseudotsuga menziesii (Douglas-fir) saplings were grown in sun-lit controlled environment chambers at ambient or elevated (4°C above ambient) temperature. We measured internal temperatures of vegetative buds with thermocouple probes and compared temperatures of normal buds and abnormal buds with loosened, rosetted outer scales in elevated temperature chambers. The abnormal buds had higher and earlier peak daily temperatures than normal buds. Elevated temperature may influence the internal temperature of buds and contribute to the development of abnormal, rosetted buds with loosened outer scales. Abnormal bud development may alter branching patterns and allometry of Douglas-fir trees subjected to climatic change. Close

• 39. [Article] Temperature and water potential effects on physiological functions of sudangrass (Sorghum vulgare var. Piper)

  Temperature and water potential effects on the growth, transpiration, total nonstructural carbohydrate (TNC) content, and nutrient uptake of sudangrass (Sorghum vulgare var. piper) were investigated in ...

  Citation × Citation Citation Abstract Copy Title: Temperature and water potential effects on physiological functions of sudangrass (Sorghum vulgare var. Piper) Author: Young, Richard Su-Shung Temperature and water potential effects on the growth, transpiration, total nonstructural carbohydrate (TNC) content, and nutrient uptake of sudangrass (Sorghum vulgare var. piper) were investigated in laboratory experiments. The effect of nitrogen supply on the growth and nutrient uptake at constant soil water potential was also investigated in this study. Two week old seedlings were used for all experiments. Soil temperatures of 10.0, 15.6, 21.1, 26.7, 32.2 and 37.8 C were tested. Plants were grown at soil water potentials of -0.35 and -2.50 bars for 10 days using the polyethylene glycol semi-permeable membrane technique for controlling soil water potential. Air temperature remained constant at 26.7 C during these experiments. Air temperatures of 18.3, 22.8, 26.7 and 32.2 C were tested in a second series of experiments, with the soil water potential and soil temperature constant at -0.35 bars and 26.7 C. Further experiment.; were conducted with nitrogen levels in the nutrient solutions of 0, 10, 25 and 100 ppm. The soil temperature and soil water potential were kept constant in these experiments. Finally, the effect of soil temperature and soil water potential on plant water potential at soil water potentials of -0.35, -0.70, -1.50 and -2.50 bars was measured. Growth rate increased with soil temperature up to an optimum temperature, then decreased at higher temperatures for both shoots and roots at both soil water potentials tested. The highest growth rate was at 30 C for the shoots and 26 C for the roots. The rate was higher at -0.35 bars than at -2.50 bars for both shoots and roots. By varying the air temperature, the rate of growth was found to be highest at the air temperature of 26.7 C. The nitrogen level of 100 ppm in the nutrient solution produced the highest growth rate. The dry matter weight increased exponentially with time in all experiments. It was concluded that the soil temperature of 30 C, air temperature of 26.7 C and a soil water potential of -0.35 bars was optimal for sudangrass growth. Transpiration rates increased exponentially as a function of time for all treatments. Transpiration rates (cm³/day) increased as the soil temperature increased at both soil water potentials. The rate at -2.50 bars was lower than at -0.35 bars. The transpiration rate also increased with increasing air temperature independent of RH differences. An equilibrium content of N, P, K, Ca, Mg, S, Mn and Zn in the plant material at each combination of treatment variables was determined based on the assumption that equilibrium was attained as time progressed. The maximum concentration of N occurred at a temperature of about 30 C in both shoots and roots, while the concentration was lower at -0.35 bars than at -2.50 bars. The concentration of P increased with soil temperature, in the shoot, but reached a maximum at 30 C in the roots. The concentration at -0.35 bars was lower than at -2.50 bars. The concentrations of K, Ca and S were not significantly different at the two water potentials. The concentration of K was highest at about 30 C in both shoots and roots. The concentration of Ca was highest at about 22 C in both shoots and roots. The suflfur concentration of the shoots increased as soil temperature increased, but a maximum concentration in the roots occurred at 30 C. The concentration of Mn was highest at 26.7 C in the shoots and at 21.1 C in the roots. Concentrations of Mn at -0.35 bars were lower than at -2.50 bars. The Zn concentration increased as soil temperature increased for both shoots and roots. The concentration at -0.35 bars was lower than at -2.50 bars. In the experiments with air temperature as the variable the concentration of N in the shoots was highest at 26.7 C, but decreased in the roots as air temperature increased. The concentration of P decreased with increasing air temperature in both shoots and roots. The concentration of K increased with increasing air temperature in the shoots but decreased in the roots. The concentration of Ca was highest at 26.7 C in the shoots, and increased with increasing air temperature in the roots. The concentration of Mg in the shoots was highest at 26.7 C, while the concentration in the roots slightly decreased with increasing air temperature. The concentration of S decreased with increasing air temperature in both shoots and roots. The Mn concentration was highest at 26.7 C in both shoots and roots. The concentration of Zn increased as air temperature increased. The increase in the roots was greater than in the shoots. The concentration of N, P. Ca and Mg in both shoots and roots increased as the nitrogen level of the nutrient solution increased. The concentration of K in the shoots increased with increasing N level, but in the roots, a maximum concentration occurred at 25 ppm. The concentration of S in the shoots increased as the nitrogen level increased but decreased in the roots. Mn concentrations increased in the shoots but decreased in the roots with increasing nitrogen supply. The Zn concentration increased in the shoots, but decreased in the roots as the N level increased. The total nonstructural carbohydrate (TNC) content decreased as the soil temperature increased. The decrease was 10 percent at a soil water potential of -0.35 bars and 2 percent at a soil water potential of -2.50 bars as the soil temperature increased from 10.0 to 32.2 C. The TNC also decreased as the air temperature increased. The decrease was 8.3 percent as the air temperature increased from 18.3 to 32.2 C. This decrease was attributed to increased respiration and increased translocation from shoots to roots. The leaf water potential (Ψ[subscript c]) and osmotic potential (Ψ[subscript π]) decreased with time at all soil temperature and soil water potential combinations. The decrease was greater at low temperatures than at high temperatures for all soil water potentials. As the soil water potential decreased from -0.35 to -2.50 bars, the leaf water potential (Ψ[subscript c]) and osmotic potential (Ψ[subscript π]) decreased at all soil temperatures. The decrease is osmotic potential (Ψ[subscript π]) was greater than the decrease in leaf water potential (Ψ[subscript c]). The turgor pressure decreased with decreasing soil temperature, and slightly increased with decreasing soil water potential. The growth rate was correlated with turgor pressure. The relationship between turgor pressure and growth rate varied with soil temperature and soil water potential. It was concluded that this relationship may have been the primary growth controlling mechanism. The rate of nutrient uptake increased with increasing water uptake at both water potentials of -0.35 and -2.50 bars. The ion concentration in the transpiration stream was lower at -0.35 bars than at -2.50 bars. The concentration increased slightly with increasing soil temperature at both soil water potentials tested, but relatively more at -2.50 bars. Title: Temperature and water potential effects on physiological functions of sudangrass (Sorghum vulgare var. Piper) Author: Young, Richard Su-Shung Temperature and water potential effects on the growth, transpiration, total nonstructural carbohydrate (TNC) content, and nutrient uptake of sudangrass (Sorghum vulgare var. piper) were investigated in laboratory experiments. The effect of nitrogen supply on the growth and nutrient uptake at constant soil water potential was also investigated in this study. Two week old seedlings were used for all experiments. Soil temperatures of 10.0, 15.6, 21.1, 26.7, 32.2 and 37.8 C were tested. Plants were grown at soil water potentials of -0.35 and -2.50 bars for 10 days using the polyethylene glycol semi-permeable membrane technique for controlling soil water potential. Air temperature remained constant at 26.7 C during these experiments. Air temperatures of 18.3, 22.8, 26.7 and 32.2 C were tested in a second series of experiments, with the soil water potential and soil temperature constant at -0.35 bars and 26.7 C. Further experiment.; were conducted with nitrogen levels in the nutrient solutions of 0, 10, 25 and 100 ppm. The soil temperature and soil water potential were kept constant in these experiments. Finally, the effect of soil temperature and soil water potential on plant water potential at soil water potentials of -0.35, -0.70, -1.50 and -2.50 bars was measured. Growth rate increased with soil temperature up to an optimum temperature, then decreased at higher temperatures for both shoots and roots at both soil water potentials tested. The highest growth rate was at 30 C for the shoots and 26 C for the roots. The rate was higher at -0.35 bars than at -2.50 bars for both shoots and roots. By varying the air temperature, the rate of growth was found to be highest at the air temperature of 26.7 C. The nitrogen level of 100 ppm in the nutrient solution produced the highest growth rate. The dry matter weight increased exponentially with time in all experiments. It was concluded that the soil temperature of 30 C, air temperature of 26.7 C and a soil water potential of -0.35 bars was optimal for sudangrass growth. Transpiration rates increased exponentially as a function of time for all treatments. Transpiration rates (cm³/day) increased as the soil temperature increased at both soil water potentials. The rate at -2.50 bars was lower than at -0.35 bars. The transpiration rate also increased with increasing air temperature independent of RH differences. An equilibrium content of N, P, K, Ca, Mg, S, Mn and Zn in the plant material at each combination of treatment variables was determined based on the assumption that equilibrium was attained as time progressed. The maximum concentration of N occurred at a temperature of about 30 C in both shoots and roots, while the concentration was lower at -0.35 bars than at -2.50 bars. The concentration of P increased with soil temperature, in the shoot, but reached a maximum at 30 C in the roots. The concentration at -0.35 bars was lower than at -2.50 bars. The concentrations of K, Ca and S were not significantly different at the two water potentials. The concentration of K was highest at about 30 C in both shoots and roots. The concentration of Ca was highest at about 22 C in both shoots and roots. The suflfur concentration of the shoots increased as soil temperature increased, but a maximum concentration in the roots occurred at 30 C. The concentration of Mn was highest at 26.7 C in the shoots and at 21.1 C in the roots. Concentrations of Mn at -0.35 bars were lower than at -2.50 bars. The Zn concentration increased as soil temperature increased for both shoots and roots. The concentration at -0.35 bars was lower than at -2.50 bars. In the experiments with air temperature as the variable the concentration of N in the shoots was highest at 26.7 C, but decreased in the roots as air temperature increased. The concentration of P decreased with increasing air temperature in both shoots and roots. The concentration of K increased with increasing air temperature in the shoots but decreased in the roots. The concentration of Ca was highest at 26.7 C in the shoots, and increased with increasing air temperature in the roots. The concentration of Mg in the shoots was highest at 26.7 C, while the concentration in the roots slightly decreased with increasing air temperature. The concentration of S decreased with increasing air temperature in both shoots and roots. The Mn concentration was highest at 26.7 C in both shoots and roots. The concentration of Zn increased as air temperature increased. The increase in the roots was greater than in the shoots. The concentration of N, P. Ca and Mg in both shoots and roots increased as the nitrogen level of the nutrient solution increased. The concentration of K in the shoots increased with increasing N level, but in the roots, a maximum concentration occurred at 25 ppm. The concentration of S in the shoots increased as the nitrogen level increased but decreased in the roots. Mn concentrations increased in the shoots but decreased in the roots with increasing nitrogen supply. The Zn concentration increased in the shoots, but decreased in the roots as the N level increased. The total nonstructural carbohydrate (TNC) content decreased as the soil temperature increased. The decrease was 10 percent at a soil water potential of -0.35 bars and 2 percent at a soil water potential of -2.50 bars as the soil temperature increased from 10.0 to 32.2 C. The TNC also decreased as the air temperature increased. The decrease was 8.3 percent as the air temperature increased from 18.3 to 32.2 C. This decrease was attributed to increased respiration and increased translocation from shoots to roots. The leaf water potential (Ψ[subscript c]) and osmotic potential (Ψ[subscript π]) decreased with time at all soil temperature and soil water potential combinations. The decrease was greater at low temperatures than at high temperatures for all soil water potentials. As the soil water potential decreased from -0.35 to -2.50 bars, the leaf water potential (Ψ[subscript c]) and osmotic potential (Ψ[subscript π]) decreased at all soil temperatures. The decrease is osmotic potential (Ψ[subscript π]) was greater than the decrease in leaf water potential (Ψ[subscript c]). The turgor pressure decreased with decreasing soil temperature, and slightly increased with decreasing soil water potential. The growth rate was correlated with turgor pressure. The relationship between turgor pressure and growth rate varied with soil temperature and soil water potential. It was concluded that this relationship may have been the primary growth controlling mechanism. The rate of nutrient uptake increased with increasing water uptake at both water potentials of -0.35 and -2.50 bars. The ion concentration in the transpiration stream was lower at -0.35 bars than at -2.50 bars. The concentration increased slightly with increasing soil temperature at both soil water potentials tested, but relatively more at -2.50 bars. Close

• 40. [Article] Development and Testing of Single-Parameter Precipitation Distributions

  This is the publisher’s final pdf. The published article is copyrighted by American Geophysical Union and can be found at: http://sites.agu.org/.

  Citation × Citation Citation Abstract Copy Title: Development and Testing of Single-Parameter Precipitation Distributions Author: Haith, Douglas A., Selker, John S. This is the publisher’s final pdf. The published article is copyrighted by American Geophysical Union and can be found at: http://sites.agu.org/. Title: Development and Testing of Single-Parameter Precipitation Distributions Author: Haith, Douglas A., Selker, John S. This is the publisher’s final pdf. The published article is copyrighted by American Geophysical Union and can be found at: http://sites.agu.org/. Close

• 41. [Article] Mid-Latitude (30°–60° N) climatic warming inferred by combining borehole temperatures with surface air temperatures

  copyrighted by American Geophysical Union

  Citation × Citation Citation Abstract Copy Title: Mid-Latitude (30°–60° N) climatic warming inferred by combining borehole temperatures with surface air temperatures Author: Harris, Robert N., Chapman, David S. copyrighted by American Geophysical Union Title: Mid-Latitude (30°–60° N) climatic warming inferred by combining borehole temperatures with surface air temperatures Author: Harris, Robert N., Chapman, David S. copyrighted by American Geophysical Union Close

• 42. [Article] Climate change in India inferred from geothermal observations

  copyrighted by American Geophysical Union

  Citation × Citation Citation Abstract Copy Title: Climate change in India inferred from geothermal observations Author: Harris, Robert N., Rao, R. U. M., Roy, Sukanta, Chapman, David S. copyrighted by American Geophysical Union Title: Climate change in India inferred from geothermal observations Author: Harris, Robert N., Rao, R. U. M., Roy, Sukanta, Chapman, David S. copyrighted by American Geophysical Union Close

• 43. [Article] Effects of temperature and other abiotic and biotic factors on development and survival of the immature stages of the alfalfa leafcutting bee, Megachile pacifica (Panzer) (=rotundata (F.)) (Hymenoptera:Megachilidae)

  Larval mortality of leafcutting bee, Megachile pacifica (Panzer) (= rotundata (F.)), is high, usually exceeding 50%. Parasites and predators are not a limiting factor in the survival of the progeny. The ...

  Citation × Citation Citation Abstract Copy Title: Effects of temperature and other abiotic and biotic factors on development and survival of the immature stages of the alfalfa leafcutting bee, Megachile pacifica (Panzer) (=rotundata (F.)) (Hymenoptera:Megachilidae) Author: Undurraga O., Jaime M. Larval mortality of leafcutting bee, Megachile pacifica (Panzer) (= rotundata (F.)), is high, usually exceeding 50%. Parasites and predators are not a limiting factor in the survival of the progeny. The disease chalk brood has been an important mortality factor since 1974. Inadequate food supply, pollen and nectar, may affect the survival of the progeny. Genetic differences within and between populations and the saponin content of alfalfa leaves do not affect brood production or survival. Domicile design and protection may also have a great influence on survival. Temperatures exceeding 50°C occur in cells when nesting material receives direct sunlight or when nesting material is housed in domiciles with poor ventilation and insulation. There are temperature differences between cells in a series, between nest positions within a domicile, and between types of nesting materials. There is no direct relationship between ambient and cell temperatures because the latter are influenced by exposure, nesting media, placement, and domicile structure. High internal bee body temperatures may occur during most bee activities, excluding resting. The effects of high temperatures on the adult bee or the eggs she contains are not known. Although larval development can proceed at temperatures below 21°C, survival is reduced. Adult activity, like metabolic larval development, can be conditioned to unusually high or low temperatures; thus, there is no absolute temperature threshold for development or activity in this bee. Eggs and young larvae reared at a constant 30°C had over 85% survival, in most years. An ambient temperature of 45°C applied for one to three hours resulted in a higher mortality of eggs and early instars than the control temperature of 30°C; at 50°C, mortality was complete. Exceptions were obtained for either situation. Half hour exposure at 50°C ambient temperature was also detrimental to immatures. An ambient temperature of 40°C in general does not affect survival of immatures. In-cell temperatures were at least 5°C lower than ambient temperatures in incubators during treatments. Repeating heat treatments on two or more days was not as severe as the duration of treatments. Larvae showed heat tolerance when exposed to two to three hours at 45°C but not to one hour, but some exceptions occurred. The mechanism for heat tolerance is not well understood, and may be related to a conditioning of individuals to high temperatures. A seasonal effect on survival was obtained and appears not to be related to the age of the laying females, nor to the generations, but rather to the thermal history to which the immatures were exposed. Heat susceptibility of eggs and early instars seemed to be similar. Fourth and fifth instars were the most heat tolerant of all larval stages. Exposure of young larvae to low temperatures before they were exposed to high temperatures did not increase mortality. However, sublethal high temperatures were generally less harmful to the immatures that were conditioned but this acclimation of the larvae did not occur in every test. Upper threshold temperature limits cannot be precisely defined, nevertheless, cell temperatures over 40°C result in egg and larval mortality. Brief exposure to 45°C was the upper limit that developing pupae could tolerate; 50°C was lethal. Pupae were most heat sensitive between three and six days before emergence. When exposed to high temperatures, pupae and emerging adults were able to arrest development. Pupae and emerging adults can be conditioned to tolerate short exposures to lethal temperatures up to seven days before emergence. Low temperatures did not affect the survival of pupae. Development of pupae and emerging adults could be arrested for up to a week at 15.6°C without harmful effect. Development and emergence proceed at 21 °C, but pupae need at least 2.5 hours per day of temperatures above 21°C to survive when not in an arrested state. Pupae not exposed to temperature above 29°C during 24 hours, emerged normally. Incubation at 29.5°C for less than 10 hours per day delayed the emergence. Pupae maintained at 15.6 °C for 22 hours per day for 8 days or for 20 hours per day for 16 days emerged after a delay longer than the period of cold. Cooling the emerging bees after high temperature treatment appeared to be more detrimental than cooling before exposures to high temperatures. The detrimental effect of extreme temperatures was shown on the survival of eggs, young larvae, and pupae, but possible chronic effects on later stadia were not studied. Title: Effects of temperature and other abiotic and biotic factors on development and survival of the immature stages of the alfalfa leafcutting bee, Megachile pacifica (Panzer) (=rotundata (F.)) (Hymenoptera:Megachilidae) Author: Undurraga O., Jaime M. Larval mortality of leafcutting bee, Megachile pacifica (Panzer) (= rotundata (F.)), is high, usually exceeding 50%. Parasites and predators are not a limiting factor in the survival of the progeny. The disease chalk brood has been an important mortality factor since 1974. Inadequate food supply, pollen and nectar, may affect the survival of the progeny. Genetic differences within and between populations and the saponin content of alfalfa leaves do not affect brood production or survival. Domicile design and protection may also have a great influence on survival. Temperatures exceeding 50°C occur in cells when nesting material receives direct sunlight or when nesting material is housed in domiciles with poor ventilation and insulation. There are temperature differences between cells in a series, between nest positions within a domicile, and between types of nesting materials. There is no direct relationship between ambient and cell temperatures because the latter are influenced by exposure, nesting media, placement, and domicile structure. High internal bee body temperatures may occur during most bee activities, excluding resting. The effects of high temperatures on the adult bee or the eggs she contains are not known. Although larval development can proceed at temperatures below 21°C, survival is reduced. Adult activity, like metabolic larval development, can be conditioned to unusually high or low temperatures; thus, there is no absolute temperature threshold for development or activity in this bee. Eggs and young larvae reared at a constant 30°C had over 85% survival, in most years. An ambient temperature of 45°C applied for one to three hours resulted in a higher mortality of eggs and early instars than the control temperature of 30°C; at 50°C, mortality was complete. Exceptions were obtained for either situation. Half hour exposure at 50°C ambient temperature was also detrimental to immatures. An ambient temperature of 40°C in general does not affect survival of immatures. In-cell temperatures were at least 5°C lower than ambient temperatures in incubators during treatments. Repeating heat treatments on two or more days was not as severe as the duration of treatments. Larvae showed heat tolerance when exposed to two to three hours at 45°C but not to one hour, but some exceptions occurred. The mechanism for heat tolerance is not well understood, and may be related to a conditioning of individuals to high temperatures. A seasonal effect on survival was obtained and appears not to be related to the age of the laying females, nor to the generations, but rather to the thermal history to which the immatures were exposed. Heat susceptibility of eggs and early instars seemed to be similar. Fourth and fifth instars were the most heat tolerant of all larval stages. Exposure of young larvae to low temperatures before they were exposed to high temperatures did not increase mortality. However, sublethal high temperatures were generally less harmful to the immatures that were conditioned but this acclimation of the larvae did not occur in every test. Upper threshold temperature limits cannot be precisely defined, nevertheless, cell temperatures over 40°C result in egg and larval mortality. Brief exposure to 45°C was the upper limit that developing pupae could tolerate; 50°C was lethal. Pupae were most heat sensitive between three and six days before emergence. When exposed to high temperatures, pupae and emerging adults were able to arrest development. Pupae and emerging adults can be conditioned to tolerate short exposures to lethal temperatures up to seven days before emergence. Low temperatures did not affect the survival of pupae. Development of pupae and emerging adults could be arrested for up to a week at 15.6°C without harmful effect. Development and emergence proceed at 21 °C, but pupae need at least 2.5 hours per day of temperatures above 21°C to survive when not in an arrested state. Pupae not exposed to temperature above 29°C during 24 hours, emerged normally. Incubation at 29.5°C for less than 10 hours per day delayed the emergence. Pupae maintained at 15.6 °C for 22 hours per day for 8 days or for 20 hours per day for 16 days emerged after a delay longer than the period of cold. Cooling the emerging bees after high temperature treatment appeared to be more detrimental than cooling before exposures to high temperatures. The detrimental effect of extreme temperatures was shown on the survival of eggs, young larvae, and pupae, but possible chronic effects on later stadia were not studied. Close

• 44. [Article] Effect of climate change on water temperature and attainment of water temperature criteria in the Yaquina Estuary, Oregon (USA)

  To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier ...

  Citation × Citation Citation Abstract Copy Title: Effect of climate change on water temperature and attainment of water temperature criteria in the Yaquina Estuary, Oregon (USA) Author: Sharp, Darrin, Collura, T. Chris Mochon, Brown, Cheryl A. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/estuarine-coastal-and-shelf-science/ Title: Effect of climate change on water temperature and attainment of water temperature criteria in the Yaquina Estuary, Oregon (USA) Author: Sharp, Darrin, Collura, T. Chris Mochon, Brown, Cheryl A. To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/estuarine-coastal-and-shelf-science/ Close

• 45. [Article] Processing effects on the ductility of chromium-vanadium alloys

  The next generation of high temperature structural alloys must exhibit exceptional resistance to fracture, creep, oxidation, and fatigue at high temperatures. Chromium is being considered due to its high ...

  Citation × Citation Citation Abstract Copy Title: Processing effects on the ductility of chromium-vanadium alloys Author: Murdock, Hailey M. The next generation of high temperature structural alloys must exhibit exceptional resistance to fracture, creep, oxidation, and fatigue at high temperatures. Chromium is being considered due to its high melting point (>1800°C), relatively low density (~7.2 g/cc), high temperature strength, and oxidation resistance. Limiting the use of chromium is its high ductile-to-brittle transition temperature. Previous efforts to reduce the ductile-to-brittle transition temperature have considered elimination of embrittling interstitals, increasing the grain size, pre-deformation and alloying. Recent computational studies have renewed interest in using alloying additions to ductilize chromium. A series of first principles calculations recently revealed elements (Ti, Zr, Hf, Nb, V) which have potential to reduce the ductile-to-brittle transition temperature when alloyed with chromium. To experimentally measure the effects of alloying and processing on the ductile-to-brittle transition temperature, chromium-vanadium alloy samples of 3 different compositions were prepared and compared to nominally pure chromium. Chromium vanadium samples were prepared from powders, hot isostatically pressed, heat treated at 1300°C and extruded at 1200°C. Elevated temperature Vickers hardness, elevated temperature tensile and elevated 3-point bend tests were performed. A diffusion study was performed using microprobe analysis to assist in the development of homogenization procedures for the alloys. Fracture surface analysis of bend and tensile specimens was used to determine the mode of fracture in bend and tensile specimens. Elevated temperature tensile tests determined a relationship between temperature and ductility in 100%Cr and 25%Cr-75%V alloys. Results from elevated temperature Vickers hardness suggest alloying with vanadium increases the strength by a factor of two. Premature failure in elevated temperature 3-point bend specimens and elevated temperature tensile tests made it difficult to quantify the effect of vanadium in affecting the ductility of chromium. Electron microscopy observations indicate that mechanical damage, likely caused by extrusion, is responsible for initiating the premature failures. Despite this complication, evidence of micro- and macro-scale ductile fracture mechanisms on the fracture surfaces of the Cr-V alloys indicate that the addition of vanadium indeed improves the ductility of chromium. Title: Processing effects on the ductility of chromium-vanadium alloys Author: Murdock, Hailey M. The next generation of high temperature structural alloys must exhibit exceptional resistance to fracture, creep, oxidation, and fatigue at high temperatures. Chromium is being considered due to its high melting point (>1800°C), relatively low density (~7.2 g/cc), high temperature strength, and oxidation resistance. Limiting the use of chromium is its high ductile-to-brittle transition temperature. Previous efforts to reduce the ductile-to-brittle transition temperature have considered elimination of embrittling interstitals, increasing the grain size, pre-deformation and alloying. Recent computational studies have renewed interest in using alloying additions to ductilize chromium. A series of first principles calculations recently revealed elements (Ti, Zr, Hf, Nb, V) which have potential to reduce the ductile-to-brittle transition temperature when alloyed with chromium. To experimentally measure the effects of alloying and processing on the ductile-to-brittle transition temperature, chromium-vanadium alloy samples of 3 different compositions were prepared and compared to nominally pure chromium. Chromium vanadium samples were prepared from powders, hot isostatically pressed, heat treated at 1300°C and extruded at 1200°C. Elevated temperature Vickers hardness, elevated temperature tensile and elevated 3-point bend tests were performed. A diffusion study was performed using microprobe analysis to assist in the development of homogenization procedures for the alloys. Fracture surface analysis of bend and tensile specimens was used to determine the mode of fracture in bend and tensile specimens. Elevated temperature tensile tests determined a relationship between temperature and ductility in 100%Cr and 25%Cr-75%V alloys. Results from elevated temperature Vickers hardness suggest alloying with vanadium increases the strength by a factor of two. Premature failure in elevated temperature 3-point bend specimens and elevated temperature tensile tests made it difficult to quantify the effect of vanadium in affecting the ductility of chromium. Electron microscopy observations indicate that mechanical damage, likely caused by extrusion, is responsible for initiating the premature failures. Despite this complication, evidence of micro- and macro-scale ductile fracture mechanisms on the fracture surfaces of the Cr-V alloys indicate that the addition of vanadium indeed improves the ductility of chromium. Close

• 46. [Article] Interaction and behavior of the redside shiner (Richardsonius balteatus) and the steelhead trout (Salmo gairdneri) in western Oregon : the influence of water temperature

  Water temperature influenced interactions between redside shiners and juvenile steelhead trout (≥1+) in the field and the laboratory. Distribution of the two species within various habitats was determined ...

  Citation × Citation Citation Abstract Copy Title: Interaction and behavior of the redside shiner (Richardsonius balteatus) and the steelhead trout (Salmo gairdneri) in western Oregon : the influence of water temperature Author: Reeves, Gordon H. Water temperature influenced interactions between redside shiners and juvenile steelhead trout (≥1+) in the field and the laboratory. Distribution of the two species within various habitats was determined in three streams with different water temperature regimes. The range of habitats occupied by trout in allopatry at cool temperatures and at intermediate temperatures in sympatry was similar but habitats occupied by shiners in allopatry at warm temperatures and in sympatry at intermediate temperatures differed. Shiners at warm temperatures in allopatry inhabited areas of intermediate depth and high velocity, similar to those inhabited by trout in the other streams. In the presence of trout at intermediate temperatures, shiners were found in deep, slow water. Water temperature and the presence of the other species influenced production, activity, and distribution of both trout and shiners in laboratory streams. Trout dominated at cool temperatures (12-15°C) and shiners prevailed at warm temperatures (19-22°C). The redside shiner exhibited two basic social organizations, loose aggregations and defense of an area. The type of organization observed varied with water temperature, abundance of food, and presence or absence of juvenile steelhead trout. The behavioral repertoire of the redside shiner was diverse. Size of the individual and proprietorship of an area were important in determining outcomes of interactions. Intensity of individual encounters varied with conditions in the laboratory streams. Plasticity of its social behavior appears to contribute to the ecological success of the redside shiner. Title: Interaction and behavior of the redside shiner (Richardsonius balteatus) and the steelhead trout (Salmo gairdneri) in western Oregon : the influence of water temperature Author: Reeves, Gordon H. Water temperature influenced interactions between redside shiners and juvenile steelhead trout (≥1+) in the field and the laboratory. Distribution of the two species within various habitats was determined in three streams with different water temperature regimes. The range of habitats occupied by trout in allopatry at cool temperatures and at intermediate temperatures in sympatry was similar but habitats occupied by shiners in allopatry at warm temperatures and in sympatry at intermediate temperatures differed. Shiners at warm temperatures in allopatry inhabited areas of intermediate depth and high velocity, similar to those inhabited by trout in the other streams. In the presence of trout at intermediate temperatures, shiners were found in deep, slow water. Water temperature and the presence of the other species influenced production, activity, and distribution of both trout and shiners in laboratory streams. Trout dominated at cool temperatures (12-15°C) and shiners prevailed at warm temperatures (19-22°C). The redside shiner exhibited two basic social organizations, loose aggregations and defense of an area. The type of organization observed varied with water temperature, abundance of food, and presence or absence of juvenile steelhead trout. The behavioral repertoire of the redside shiner was diverse. Size of the individual and proprietorship of an area were important in determining outcomes of interactions. Intensity of individual encounters varied with conditions in the laboratory streams. Plasticity of its social behavior appears to contribute to the ecological success of the redside shiner. Close

• 47. [Article] Amplification and dampening of soil respiration by changes in temperature variability

  NEWS COVERAGE: A news release based on this journal publication, which is written for a lay audience and has been approved by an author of the study, is available online: http://bit.ly/lyWhTB

  Citation × Citation Citation Abstract Copy Title: Amplification and dampening of soil respiration by changes in temperature variability Author: Loescher, H. W., Thomann, E., Sierra, C. A., Harmon, M. E., Perakis, S. S. NEWS COVERAGE: A news release based on this journal publication, which is written for a lay audience and has been approved by an author of the study, is available online: http://bit.ly/lyWhTB Title: Amplification and dampening of soil respiration by changes in temperature variability Author: Loescher, H. W., Thomann, E., Sierra, C. A., Harmon, M. E., Perakis, S. S. NEWS COVERAGE: A news release based on this journal publication, which is written for a lay audience and has been approved by an author of the study, is available online: http://bit.ly/lyWhTB Close

• 48. [Article] The effects of elevated temperature and stress on immune function in juvenile chinook salmon (Oncorhynchus tshawytscha)

  Stress, including extreme or rapidly changing temperatures, are known to have deleterious effects on fish health and physiology. This thesis examines the combined effects of elevated acclimation temperature ...

  Citation × Citation Citation Abstract Copy Title: The effects of elevated temperature and stress on immune function in juvenile chinook salmon (Oncorhynchus tshawytscha) Author: Harrahy, Laura Nicole Martini Stress, including extreme or rapidly changing temperatures, are known to have deleterious effects on fish health and physiology. This thesis examines the combined effects of elevated acclimation temperature and acute handling stress on the number of antibody producing cells, plasma lysozyme concentrations, and the number of pronephric leukocytes in juvenile chinook salmon (Oncorhynchus tshawytscha). An additional goal of this thesis was to explore the effects of a temperature fluctuation, as a potential instigator of thermal shock, on innate immunity in wild fall chinook salmon of the Columbia River, specifically to determine if there are effects on plasma lysozyme concentrations and on the frequencies of lymphocytes, neutrophils, and thrombocytes in circulation. Finally, based on results found in an experiment involving elevated acclimation temperature, the relationship between the number of antibody producing cells and fish body weight was examined. Plasma lysozyme concentrations and the number of pronephric leukocytes were both affected by acclimation to 21°C compared to 13°C. While a positive relationship was found between temperature and lysozyme, an inverse relationship was found between temperature and the number of pronephric leukocytes. Plasma lysozyme concentrations, the number of pronephric leukocytes, and the number of antibody producing cells did not respond to the stressor, and the combination of elevated temperature and stress did not have an additive effect on any of the physiological or immunological variables studied. Differences between controls and temperature-treated fish were not detected among individual time points throughout a temperature fluctuation experiment, despite overall responses in plasma lysozyme concentrations and the frequencies of circulating lymphocytes. The frequencies of circulating neutrophils and thrombocytes did not respond to the thermal stressor. Finally, a significant positive relationship was detected between the number of antibody producing cells (assessed by a hemolytic plaque assay) and body weight among non-stressed fish acclimated to 21°C and 13°C. Regardless of acclimation temperature, these results emphasize the importance of the standardization of fish size for immunological experiments. Results from this thesis suggest that some components of innate immunity are affected by elevated acclimation temperatures and that the adaptive immune system is affected by acclimation temperature differently in small and large fish. Title: The effects of elevated temperature and stress on immune function in juvenile chinook salmon (Oncorhynchus tshawytscha) Author: Harrahy, Laura Nicole Martini Stress, including extreme or rapidly changing temperatures, are known to have deleterious effects on fish health and physiology. This thesis examines the combined effects of elevated acclimation temperature and acute handling stress on the number of antibody producing cells, plasma lysozyme concentrations, and the number of pronephric leukocytes in juvenile chinook salmon (Oncorhynchus tshawytscha). An additional goal of this thesis was to explore the effects of a temperature fluctuation, as a potential instigator of thermal shock, on innate immunity in wild fall chinook salmon of the Columbia River, specifically to determine if there are effects on plasma lysozyme concentrations and on the frequencies of lymphocytes, neutrophils, and thrombocytes in circulation. Finally, based on results found in an experiment involving elevated acclimation temperature, the relationship between the number of antibody producing cells and fish body weight was examined. Plasma lysozyme concentrations and the number of pronephric leukocytes were both affected by acclimation to 21°C compared to 13°C. While a positive relationship was found between temperature and lysozyme, an inverse relationship was found between temperature and the number of pronephric leukocytes. Plasma lysozyme concentrations, the number of pronephric leukocytes, and the number of antibody producing cells did not respond to the stressor, and the combination of elevated temperature and stress did not have an additive effect on any of the physiological or immunological variables studied. Differences between controls and temperature-treated fish were not detected among individual time points throughout a temperature fluctuation experiment, despite overall responses in plasma lysozyme concentrations and the frequencies of circulating lymphocytes. The frequencies of circulating neutrophils and thrombocytes did not respond to the thermal stressor. Finally, a significant positive relationship was detected between the number of antibody producing cells (assessed by a hemolytic plaque assay) and body weight among non-stressed fish acclimated to 21°C and 13°C. Regardless of acclimation temperature, these results emphasize the importance of the standardization of fish size for immunological experiments. Results from this thesis suggest that some components of innate immunity are affected by elevated acclimation temperatures and that the adaptive immune system is affected by acclimation temperature differently in small and large fish. Close

• 49. [Article] Repeat temperature measurements in borehole GC-1, northwestern Utah: towards isolating a climate-change signal borehole temperature profiles

  Copyrighted by American Geophysical Union

  Citation × Citation Citation Abstract Copy Title: Repeat temperature measurements in borehole GC-1, northwestern Utah: towards isolating a climate-change signal borehole temperature profiles Author: Chapman, David S., Harris, Robert N. Copyrighted by American Geophysical Union Title: Repeat temperature measurements in borehole GC-1, northwestern Utah: towards isolating a climate-change signal borehole temperature profiles Author: Chapman, David S., Harris, Robert N. Copyrighted by American Geophysical Union Close

• 50. [Article] Design of an apparatus with controlled rates of temperature change for use in cold tolerance tests of conifers

  An apparatus was designed to permit freezing tests of needles and other tissue parts from coniferous trees under controlled rates of temperature change with time. The design is based on the principle of ...

  Citation × Citation Citation Abstract Copy Title: Design of an apparatus with controlled rates of temperature change for use in cold tolerance tests of conifers Author: Wessell, William James An apparatus was designed to permit freezing tests of needles and other tissue parts from coniferous trees under controlled rates of temperature change with time. The design is based on the principle of a balanced system of refrigeration demand and heat input to achieve a steady temperature state. The apparatus permits the operator to decrease temperatures from 0°C to -40°C at rates of 1, 2, 3, or 4°C per hour, to hold temperatures at the desired freezing level from 1 to 24 hours, and to increase to 0°C at rates of 1, 2, 3, or 4°C per hour. Temperatures achieved within the sample tubes are accurate to within ± 0. 9°C of the expected temperature. Title: Design of an apparatus with controlled rates of temperature change for use in cold tolerance tests of conifers Author: Wessell, William James An apparatus was designed to permit freezing tests of needles and other tissue parts from coniferous trees under controlled rates of temperature change with time. The design is based on the principle of a balanced system of refrigeration demand and heat input to achieve a steady temperature state. The apparatus permits the operator to decrease temperatures from 0°C to -40°C at rates of 1, 2, 3, or 4°C per hour, to hold temperatures at the desired freezing level from 1 to 24 hours, and to increase to 0°C at rates of 1, 2, 3, or 4°C per hour. Temperatures achieved within the sample tubes are accurate to within ± 0. 9°C of the expected temperature. Close

• 51. [Article] Bridging environmental physiology and community ecology : temperature effects at the community level

  Most climate change predictions focus on the response of individual species to changing local conditions and ignore species interactions, largely due to the lack of a sound theoretical foundation for how ...

  Citation × Citation Citation Abstract Copy Title: Bridging environmental physiology and community ecology : temperature effects at the community level Author: Iles, Alison C. Most climate change predictions focus on the response of individual species to changing local conditions and ignore species interactions, largely due to the lack of a sound theoretical foundation for how interactions are expected to change with climate and how to incorporate them into climate change models. Much of the variability in species interaction strengths may be governed by fundamental constraints on physiological rates, possibly providing a framework for including species interactions into climate change models. Metabolic rates, ingestion rates and many other physiological rates are relatively predictable from body size and body temperature due to constraints imposed by the physical and chemical laws that govern fluid dynamics and the kinetics of biochemical reaction times. My dissertation assesses the usefulness of this framework by exploring the community-level consequences of physiological constraints. In Chapter 2, I incorporated temperature and body size scaling into the biological rate parameters of a series of realistically structured trophic network models. The relative magnitude of the temperature scaling parameters affecting consumer energetic costs (metabolic rates) and energetic gains (ingestion rates) determined how consumer energetic efficiency changed with temperature. I systematically changed consumer energetic efficiency and examined the sensitivity of network stability and species persistence to various temperatures. I found that a species' probability of extinction depended primarily on the effects of organismal physiology (body size and energetic efficiency with respect to temperature) and secondarily on the effects of local food web structure (trophic level and consumer generality). This suggests that physiology is highly influential on the structure and dynamics of ecological communities. If consumer energetic efficiency declined as temperature increased, that is, species did best at lower temperatures, then the simulated networks had greater stability at lower temperatures. The opposite scenario resulted in greater stability at higher temperatures. Thus, much of the community-level response depends on what species energetic efficiencies at the organismal-level really are, which formed the research question for Chapter 3: How does consumer energetic efficiency change with temperature? Existing evidence is scarce but suggestive of decreasing consumer energetic efficiency with increasing temperature. I tested this hypothesis on seven rocky intertidal invertebrate species by measuring the relative temperature scaling of their metabolic and ingestion rates as well as consumer interaction strength under lab conditions. Energetic efficiencies of these rocky intertidal invertebrates declined and species interaction strengths tended to increase with temperature. Thus, in the rocky intertidal, the mechanistic effect of temperature would be to lower community stability at higher temperatures. Chapter 4 tests if the mechanistic effects of temperature on ingestion rates and species interaction strengths seen in the lab are apparent under field conditions. Bruce Menge and I related bio-mimetic estimates of body temperatures to estimates of per capita mussel ingestion rates and species interaction strengths by the ochre sea star Pisaster ochraceus, a keystone predator of the rocky intertidal. We found a strong, positive effect of body temperature on both per capita ingestion rates and interaction strengths. However, the effects of season and the unique way in which P. ochraceus regulates body temperatures were also apparent, leaving room for adaptation and acclimation to partially compensate for the mechanistic constraint of body temperature. Community structure of the rocky intertidal is associated with environmental forcing due to upwelling, which delivers cold, nutrient rich water to the nearshore environment. As upwelling is driven by large-scale atmospheric pressure gradients, climate change has the potential to affect a wide range of significant ecological processes through changes in water temperature. In Chapter 5, my coauthors and I identified long-term trends in the phenology of upwelling events that are consistent with climate change predictions: upwelling events are becoming stronger and longer. As expected, longer upwelling events were related to lower average water temperatures in the rocky intertidal. Furthermore, recruitment rates of barnacles and mussels were associated with the phenology of upwelling events. Thus climate change is altering the mode and the tempo of environmental forcing in nearshore ecosystems, with ramifications for community structure and function. Ongoing, long-term changes in environmental forcing in rocky intertidal ecosystems provide an opportunity to understand how temperature shapes community structure and the ramifications of climate change. My dissertation research demonstrates that the effect of temperature on organismal performance is an important force structuring ecological communities and has potential as a tractable framework for predicting the community level effects of climate change. Title: Bridging environmental physiology and community ecology : temperature effects at the community level Author: Iles, Alison C. Most climate change predictions focus on the response of individual species to changing local conditions and ignore species interactions, largely due to the lack of a sound theoretical foundation for how interactions are expected to change with climate and how to incorporate them into climate change models. Much of the variability in species interaction strengths may be governed by fundamental constraints on physiological rates, possibly providing a framework for including species interactions into climate change models. Metabolic rates, ingestion rates and many other physiological rates are relatively predictable from body size and body temperature due to constraints imposed by the physical and chemical laws that govern fluid dynamics and the kinetics of biochemical reaction times. My dissertation assesses the usefulness of this framework by exploring the community-level consequences of physiological constraints. In Chapter 2, I incorporated temperature and body size scaling into the biological rate parameters of a series of realistically structured trophic network models. The relative magnitude of the temperature scaling parameters affecting consumer energetic costs (metabolic rates) and energetic gains (ingestion rates) determined how consumer energetic efficiency changed with temperature. I systematically changed consumer energetic efficiency and examined the sensitivity of network stability and species persistence to various temperatures. I found that a species' probability of extinction depended primarily on the effects of organismal physiology (body size and energetic efficiency with respect to temperature) and secondarily on the effects of local food web structure (trophic level and consumer generality). This suggests that physiology is highly influential on the structure and dynamics of ecological communities. If consumer energetic efficiency declined as temperature increased, that is, species did best at lower temperatures, then the simulated networks had greater stability at lower temperatures. The opposite scenario resulted in greater stability at higher temperatures. Thus, much of the community-level response depends on what species energetic efficiencies at the organismal-level really are, which formed the research question for Chapter 3: How does consumer energetic efficiency change with temperature? Existing evidence is scarce but suggestive of decreasing consumer energetic efficiency with increasing temperature. I tested this hypothesis on seven rocky intertidal invertebrate species by measuring the relative temperature scaling of their metabolic and ingestion rates as well as consumer interaction strength under lab conditions. Energetic efficiencies of these rocky intertidal invertebrates declined and species interaction strengths tended to increase with temperature. Thus, in the rocky intertidal, the mechanistic effect of temperature would be to lower community stability at higher temperatures. Chapter 4 tests if the mechanistic effects of temperature on ingestion rates and species interaction strengths seen in the lab are apparent under field conditions. Bruce Menge and I related bio-mimetic estimates of body temperatures to estimates of per capita mussel ingestion rates and species interaction strengths by the ochre sea star Pisaster ochraceus, a keystone predator of the rocky intertidal. We found a strong, positive effect of body temperature on both per capita ingestion rates and interaction strengths. However, the effects of season and the unique way in which P. ochraceus regulates body temperatures were also apparent, leaving room for adaptation and acclimation to partially compensate for the mechanistic constraint of body temperature. Community structure of the rocky intertidal is associated with environmental forcing due to upwelling, which delivers cold, nutrient rich water to the nearshore environment. As upwelling is driven by large-scale atmospheric pressure gradients, climate change has the potential to affect a wide range of significant ecological processes through changes in water temperature. In Chapter 5, my coauthors and I identified long-term trends in the phenology of upwelling events that are consistent with climate change predictions: upwelling events are becoming stronger and longer. As expected, longer upwelling events were related to lower average water temperatures in the rocky intertidal. Furthermore, recruitment rates of barnacles and mussels were associated with the phenology of upwelling events. Thus climate change is altering the mode and the tempo of environmental forcing in nearshore ecosystems, with ramifications for community structure and function. Ongoing, long-term changes in environmental forcing in rocky intertidal ecosystems provide an opportunity to understand how temperature shapes community structure and the ramifications of climate change. My dissertation research demonstrates that the effect of temperature on organismal performance is an important force structuring ecological communities and has potential as a tractable framework for predicting the community level effects of climate change. Close

• 52. [Article] Selection and performance evaluation of a test method to assess thermal cracking resistance of asphalt-aggregate mixtures

  Thermal distress in asphalt concrete pavements is a widespread problem around the world. Thermal cracking can be divided into two modes of distress: low temperature cracking and thermal fatigue cracking. ...

  Citation × Citation Citation Abstract Copy Title: Selection and performance evaluation of a test method to assess thermal cracking resistance of asphalt-aggregate mixtures Author: Jung, Duhwoe Thermal distress in asphalt concrete pavements is a widespread problem around the world. Thermal cracking can be divided into two modes of distress: low temperature cracking and thermal fatigue cracking. Low temperature cracking results from extremely cold temperatures; thermal fatigue cracking results from daily temperature cycles. Low temperature cracking is attributed to tensile stresses induced in the asphalt concrete pavement as the temperature drops to an extremely low temperature. If the pavement is cooled, tensile stresses develop as a result of the pavement's tendency to contract. The friction between the pavement and the base layer resists the contraction. If the tensile stress equals the strength of the mixture at that temperature, a micro-crack develops at the surface of the pavement. Under repeated temperature cycles, the crack penetrates the full depth and across the asphalt concrete layer. The thermal stress restrained specimen test (TSRST) was identified as an accelerated laboratory test to evaluate the thermal cracking resistance of asphalt concrete mixtures. The TSRST system developed at OSU includes a load system, data control/acquisition system and software, temperature control system, and specimen alignment stand. The overall system is controlled by a personal computer. A TSRST is conducted by cooling an asphalt concrete specimen at a specified rate while monitoring the specimen at constant length. A typical thermally-induced stress curve is divided into two parts: relaxation and non-relaxation. The temperature at which the curve is divided into two parts is termed the transition temperature. The temperature at fracture is termed the fracture temperature and the maximum stress is the fracture strength. An extensive number of TSRSTs over a wide range of conditions were performed to investigate the thermal cracking resistance of asphalt concrete mixtures. The TSRST results provided a very strong indication of low temperature cracking resistance for all mixtures considered. A ranking of mixtures for low temperature cracking resistance based on the TSRST fracture temperature was in excellent agreement with a ranking based on the physical properties of the asphalt cements. It is highly recommended that the TSRST be used in mix evaluation to identify low temperature cracking resistance of asphalt concrete mixtures. The TSRST showed very promising results regarding the effect of all variables which are currently considered to affect the low temperature cracking of mixtures. The variables considered to have significant affect on the low temperature cracking resistance of mixtures in this study include asphalt type, aggregate type, degree of aging, cooling rate, and stress relaxation. Title: Selection and performance evaluation of a test method to assess thermal cracking resistance of asphalt-aggregate mixtures Author: Jung, Duhwoe Thermal distress in asphalt concrete pavements is a widespread problem around the world. Thermal cracking can be divided into two modes of distress: low temperature cracking and thermal fatigue cracking. Low temperature cracking results from extremely cold temperatures; thermal fatigue cracking results from daily temperature cycles. Low temperature cracking is attributed to tensile stresses induced in the asphalt concrete pavement as the temperature drops to an extremely low temperature. If the pavement is cooled, tensile stresses develop as a result of the pavement's tendency to contract. The friction between the pavement and the base layer resists the contraction. If the tensile stress equals the strength of the mixture at that temperature, a micro-crack develops at the surface of the pavement. Under repeated temperature cycles, the crack penetrates the full depth and across the asphalt concrete layer. The thermal stress restrained specimen test (TSRST) was identified as an accelerated laboratory test to evaluate the thermal cracking resistance of asphalt concrete mixtures. The TSRST system developed at OSU includes a load system, data control/acquisition system and software, temperature control system, and specimen alignment stand. The overall system is controlled by a personal computer. A TSRST is conducted by cooling an asphalt concrete specimen at a specified rate while monitoring the specimen at constant length. A typical thermally-induced stress curve is divided into two parts: relaxation and non-relaxation. The temperature at which the curve is divided into two parts is termed the transition temperature. The temperature at fracture is termed the fracture temperature and the maximum stress is the fracture strength. An extensive number of TSRSTs over a wide range of conditions were performed to investigate the thermal cracking resistance of asphalt concrete mixtures. The TSRST results provided a very strong indication of low temperature cracking resistance for all mixtures considered. A ranking of mixtures for low temperature cracking resistance based on the TSRST fracture temperature was in excellent agreement with a ranking based on the physical properties of the asphalt cements. It is highly recommended that the TSRST be used in mix evaluation to identify low temperature cracking resistance of asphalt concrete mixtures. The TSRST showed very promising results regarding the effect of all variables which are currently considered to affect the low temperature cracking of mixtures. The variables considered to have significant affect on the low temperature cracking resistance of mixtures in this study include asphalt type, aggregate type, degree of aging, cooling rate, and stress relaxation. Close

• 53. [Article] Development of a binary mixture gas composition instrument for use in a confined high temperature environment

  With recent advancements in material science, industrial operations are being conducted at higher and higher temperatures. This is apparent in the nuclear industry where a division of the field is working ...

  Citation × Citation Citation Abstract Copy Title: Development of a binary mixture gas composition instrument for use in a confined high temperature environment Author: Cadell, Seth R. With recent advancements in material science, industrial operations are being conducted at higher and higher temperatures. This is apparent in the nuclear industry where a division of the field is working to develop the High Temperature Gas Reactor and the Very High Temperature Gas Reactor concurrently. Both of these facilities will have outlet gas temperatures that are at significantly higher temperatures than the typical water cooled reactor. These increased temperatures provide improved efficiency for the production of hydrogen, provide direct heating for oil refineries, or more efficient electricity generation. As high temperature operations are being developed, instruments capable of measuring the operating parameters must be developed concurrently. Within the gas reactor community there is a need to measure the impurities within the primary coolant. Current devices will not survive the temperature and radiation environments of a nuclear reactor. An instrument is needed to measure the impurities within the coolant while living inside the reactor, where this instrument would measure the amount of the impurity within the coolant. There are many industrial applications that need to measure the ratio of two components, whether it be the amount of particulate in air that is typical to pneumatic pumping, or the liquid to gas ratio in natural gas as it flows through a pipeline. All of the measurements in these applications can be met using a capacitance sensor. Current capacitance sensors are built to operate at ambient temperatures with only one company producing a product that will handle a temperature of up to 400 °C. This maximum operating temperature is much too low to measure the gas characteristics in the High Temperature Gas Reactor. If this measurement technique were to be improved to operate at the expected temperatures, the coolant within the primary loop could be monitored for water leaks in the steam generator, carbon dust buildup entrained in the flow, or used to measure the purity of the coolant itself. This work details the efforts conducted to develop such an instrument. While the concept of designing a capacitance sensor to measure a gas mixture is not unique, the application of using a capacitance sensor within a nuclear reactor is a new application. This application requires the development of an instrument that will survive a high temperature nuclear reactor environment and operate at a sensitivity not found in current applications. To prove this technique, instrument prototypes were built and tested in confined environments and at high temperatures. This work discusses the proof of concept testing and outlines an application in the High Temperature Test Facility to increase the operational understanding of the instrument. This work is the first step toward the ultimate outcome of this work, which is to provide a new tool to the gas reactor community allowing real-time measurements of coolant properties within the core. Title: Development of a binary mixture gas composition instrument for use in a confined high temperature environment Author: Cadell, Seth R. With recent advancements in material science, industrial operations are being conducted at higher and higher temperatures. This is apparent in the nuclear industry where a division of the field is working to develop the High Temperature Gas Reactor and the Very High Temperature Gas Reactor concurrently. Both of these facilities will have outlet gas temperatures that are at significantly higher temperatures than the typical water cooled reactor. These increased temperatures provide improved efficiency for the production of hydrogen, provide direct heating for oil refineries, or more efficient electricity generation. As high temperature operations are being developed, instruments capable of measuring the operating parameters must be developed concurrently. Within the gas reactor community there is a need to measure the impurities within the primary coolant. Current devices will not survive the temperature and radiation environments of a nuclear reactor. An instrument is needed to measure the impurities within the coolant while living inside the reactor, where this instrument would measure the amount of the impurity within the coolant. There are many industrial applications that need to measure the ratio of two components, whether it be the amount of particulate in air that is typical to pneumatic pumping, or the liquid to gas ratio in natural gas as it flows through a pipeline. All of the measurements in these applications can be met using a capacitance sensor. Current capacitance sensors are built to operate at ambient temperatures with only one company producing a product that will handle a temperature of up to 400 °C. This maximum operating temperature is much too low to measure the gas characteristics in the High Temperature Gas Reactor. If this measurement technique were to be improved to operate at the expected temperatures, the coolant within the primary loop could be monitored for water leaks in the steam generator, carbon dust buildup entrained in the flow, or used to measure the purity of the coolant itself. This work details the efforts conducted to develop such an instrument. While the concept of designing a capacitance sensor to measure a gas mixture is not unique, the application of using a capacitance sensor within a nuclear reactor is a new application. This application requires the development of an instrument that will survive a high temperature nuclear reactor environment and operate at a sensitivity not found in current applications. To prove this technique, instrument prototypes were built and tested in confined environments and at high temperatures. This work discusses the proof of concept testing and outlines an application in the High Temperature Test Facility to increase the operational understanding of the instrument. This work is the first step toward the ultimate outcome of this work, which is to provide a new tool to the gas reactor community allowing real-time measurements of coolant properties within the core. Close

• 54. [Article] High Mobility Group Protein 1 (HMGB1) And Its Role As A Global Transcription Regulator In Response To Temperature Fluctuations In The Annual Killifish Austrofundulus limnaeus

  As a study organism, annual killifish (Austrofundulus limnaeus) provide a well suited study system for examining the effects of environmental temperature fluctuations at the cellular level. A. limnaeus ...

  Citation × Citation Citation Abstract Copy Title: High Mobility Group Protein 1 (HMGB1) And Its Role As A Global Transcription Regulator In Response To Temperature Fluctuations In The Annual Killifish Austrofundulus limnaeus Author: Alla, Victoria Martin Year: 2011 As a study organism, annual killifish (Austrofundulus limnaeus) provide a well suited study system for examining the effects of environmental temperature fluctuations at the cellular level. A. limnaeus persist in the harsh high desert climate of the Maracaibo Basin, Venezuela where they live in small, ephemeral freshwater pools. Temperatures in these waters can vary as much as 20 degrees C daily and reach maximums of over 40 degrees C due to the semi-arid climate. Previous cDNA microarray studies on killifish revealed the mRNA pattern for High Mobility Group Protein 1 (HMGB1) to be strongly affected by temperature perturbations. Specifically, peaks in hmgb1 transcript abundance were negatively correlated with temperature during temperature cycling, and experienced over a 10 fold difference in expression in response to the temperature cycle. Using the same temperature cycling experimental setup, this study's aim was three-fold: (1) to characterize the total amount of HMGB1 protein in adult male killifish livers, (2) to describe the subcellular localization of the HMGB1 protein in adult male killifish livers and (3) to sequence the 5' upstream region of the hmgb1 gene to identify possible stress responsive elements. We detected no significant difference in total HMGB1 protein levels as a consequence of temperature cycling. The data for subcellular localization of HGMB1 protein do not support a strong change in subcellular localization of the protein in response to temperature cycling; most of the HMGB1 protein is found in the cytoplasmic compartment in liver tissue. Although overall patterns of subcellular localization did not change significantly, we found a significant difference between nuclear HMGB1 protein levels in temperature cycled fish versus control (constant temperature) fish. This could suggest a muting of the natural translocation of HMGB1 into the nucleus observed in control fish at around 9:00 at night. Finally, the upstream region of the hgmb1 gene does reveal a number of putative stress responsive transcription factor binding sites. Title: High Mobility Group Protein 1 (HMGB1) And Its Role As A Global Transcription Regulator In Response To Temperature Fluctuations In The Annual Killifish Austrofundulus limnaeus Author: Alla, Victoria Martin Year: 2011 As a study organism, annual killifish (Austrofundulus limnaeus) provide a well suited study system for examining the effects of environmental temperature fluctuations at the cellular level. A. limnaeus persist in the harsh high desert climate of the Maracaibo Basin, Venezuela where they live in small, ephemeral freshwater pools. Temperatures in these waters can vary as much as 20 degrees C daily and reach maximums of over 40 degrees C due to the semi-arid climate. Previous cDNA microarray studies on killifish revealed the mRNA pattern for High Mobility Group Protein 1 (HMGB1) to be strongly affected by temperature perturbations. Specifically, peaks in hmgb1 transcript abundance were negatively correlated with temperature during temperature cycling, and experienced over a 10 fold difference in expression in response to the temperature cycle. Using the same temperature cycling experimental setup, this study's aim was three-fold: (1) to characterize the total amount of HMGB1 protein in adult male killifish livers, (2) to describe the subcellular localization of the HMGB1 protein in adult male killifish livers and (3) to sequence the 5' upstream region of the hmgb1 gene to identify possible stress responsive elements. We detected no significant difference in total HMGB1 protein levels as a consequence of temperature cycling. The data for subcellular localization of HGMB1 protein do not support a strong change in subcellular localization of the protein in response to temperature cycling; most of the HMGB1 protein is found in the cytoplasmic compartment in liver tissue. Although overall patterns of subcellular localization did not change significantly, we found a significant difference between nuclear HMGB1 protein levels in temperature cycled fish versus control (constant temperature) fish. This could suggest a muting of the natural translocation of HMGB1 into the nucleus observed in control fish at around 9:00 at night. Finally, the upstream region of the hgmb1 gene does reveal a number of putative stress responsive transcription factor binding sites. Close

• 55. [Article] Borehole temperatures and tree rings: Seasonality and estimates of extratropical Northern Hemispheric warming

  Copyrighted by American Geophysical Union.

  Citation × Citation Citation Abstract Copy Title: Borehole temperatures and tree rings: Seasonality and estimates of extratropical Northern Hemispheric warming Author: Chapman, David S., Harris, Robert N. Copyrighted by American Geophysical Union. Title: Borehole temperatures and tree rings: Seasonality and estimates of extratropical Northern Hemispheric warming Author: Chapman, David S., Harris, Robert N. Copyrighted by American Geophysical Union. Close

• 56. [Article] Effect of short-term decrease in water temperature on body temperature and involvement of testosterone in steelhead and rainbow trout, Oncorhynchus mykiss

  To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier ...

  Citation × Citation Citation Abstract Copy Title: Effect of short-term decrease in water temperature on body temperature and involvement of testosterone in steelhead and rainbow trout, Oncorhynchus mykiss Author: Schreck, Carl B., Noakes, David L.G., Yada, Takashi, Matsuda, Hiroyuki, Miura, Go, Munakata, Arimune To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier and can be found at: http://www.elsevier.com/. Title: Effect of short-term decrease in water temperature on body temperature and involvement of testosterone in steelhead and rainbow trout, Oncorhynchus mykiss Author: Schreck, Carl B., Noakes, David L.G., Yada, Takashi, Matsuda, Hiroyuki, Miura, Go, Munakata, Arimune To the best of our knowledge, one or more authors of this paper were federal employees when contributing to this work. This is the publisher’s final pdf. The published article is copyrighted by Elsevier and can be found at: http://www.elsevier.com/. Close

• 57. [Article] Determination of Surface Fluxes from the Surface Radiative Temperature

  This study examines the bulk aerodynamic method for estimating surface fluxes of heat and moisture using the surface radiative temperature. The surface radiative temperature is often the only available ...

  Citation × Citation Citation Abstract Copy Title: Determination of Surface Fluxes from the Surface Radiative Temperature Author: Sun, Jielun, Mahrt, L. This study examines the bulk aerodynamic method for estimating surface fluxes of heat and moisture using the surface radiative temperature. The surface radiative temperature is often the only available surface temperature from field measurements. Models typically predict heat fluxes from the surface radiative temperature computed from the surface energy balance. In this study, the corresponding radiometric exchange coefficient and radiometric roughness height are computed from tower- and low-level aircraft data taken during four different field programs. The data analysis shows that the radiometric exchange coefficient does not increase with increasing instability. This is because the radiometric exchange coefficient must compensate for the large vertical temperature difference resulting from use of the surface radiative temperature. The data analysis and scaling arguments indicate that the radiometric exchange coefficient for heat in the bulk aerodynamic formulation is closely related to θ*/Δθ for both stable and unstable conditions, where Δθ is the difference between the surface radiative temperature and the air temperature and θ* is the negative of the heat flux divided by the surface friction velocity. Application of Monin–Obukhov similarity theory with surface radiative temperature also reduces to a relatively circular internal relationship between the radiometric roughness height and θ*/Δθ. This roughness height is flow dependent and not systematically related to the roughness height for momentum. As an additional complication, the observed radiometric exchange coefficient for heat depends on the relationship between the measured surface radiative temperature and the microscale distribution of surface radiative temperature in the footprint of the heat flux measurement. Analogous problems affect the prediction of the moisture flux based on the saturation vapor pressure at the surface radiative temperature. Title: Determination of Surface Fluxes from the Surface Radiative Temperature Author: Sun, Jielun, Mahrt, L. This study examines the bulk aerodynamic method for estimating surface fluxes of heat and moisture using the surface radiative temperature. The surface radiative temperature is often the only available surface temperature from field measurements. Models typically predict heat fluxes from the surface radiative temperature computed from the surface energy balance. In this study, the corresponding radiometric exchange coefficient and radiometric roughness height are computed from tower- and low-level aircraft data taken during four different field programs. The data analysis shows that the radiometric exchange coefficient does not increase with increasing instability. This is because the radiometric exchange coefficient must compensate for the large vertical temperature difference resulting from use of the surface radiative temperature. The data analysis and scaling arguments indicate that the radiometric exchange coefficient for heat in the bulk aerodynamic formulation is closely related to θ*/Δθ for both stable and unstable conditions, where Δθ is the difference between the surface radiative temperature and the air temperature and θ* is the negative of the heat flux divided by the surface friction velocity. Application of Monin–Obukhov similarity theory with surface radiative temperature also reduces to a relatively circular internal relationship between the radiometric roughness height and θ*/Δθ. This roughness height is flow dependent and not systematically related to the roughness height for momentum. As an additional complication, the observed radiometric exchange coefficient for heat depends on the relationship between the measured surface radiative temperature and the microscale distribution of surface radiative temperature in the footprint of the heat flux measurement. Analogous problems affect the prediction of the moisture flux based on the saturation vapor pressure at the surface radiative temperature. Close

• 58. [Article] Long-Term Sea Surface Temperature Variability along the U.S. East Coast

  Sea surface temperature variations along the entire U.S. East Coast from 1875 to 2007 are characterized using a collection of historical observations from lighthouses and lightships combined with recent ...

  Citation × Citation Citation Abstract Copy Title: Long-Term Sea Surface Temperature Variability along the U.S. East Coast Author: Shearman, R. Kipp, Lentz, Steven J. Sea surface temperature variations along the entire U.S. East Coast from 1875 to 2007 are characterized using a collection of historical observations from lighthouses and lightships combined with recent buoy and shore-based measurements. Long-term coastal temperature trends are warming in the Gulf of Maine [1.0° ± 0.3°C (100 yr)⁻¹] and Middle Atlantic Bight [0.7° ± 0.3°C (100 yr)⁻¹], whereas trends are weakly cooling or not significant in the South Atlantic Bight [−0.1° ± 0.3°C (100 yr)⁻¹] and off Florida [−0.3° ± 0.2°C (100 yr)⁻¹]. Over the last century, temperatures along the northeastern U.S. coast have warmed at a rate 1.8–2.5 times the regional atmospheric temperature trend but are comparable to warming rates for the Arctic and Labrador, the source of coastal ocean waters north of Cape Hatteras (36°N). South of Cape Hatteras, coastal ocean temperature trends match the regional atmospheric temperature trend. The observations and a simple model show that along-shelf transport, associated with the mean coastal current system running from Labrador to Cape Hatteras, is the mechanism controlling long-term temperature changes for this region and not the local air–sea exchange of heat. Title: Long-Term Sea Surface Temperature Variability along the U.S. East Coast Author: Shearman, R. Kipp, Lentz, Steven J. Sea surface temperature variations along the entire U.S. East Coast from 1875 to 2007 are characterized using a collection of historical observations from lighthouses and lightships combined with recent buoy and shore-based measurements. Long-term coastal temperature trends are warming in the Gulf of Maine [1.0° ± 0.3°C (100 yr)⁻¹] and Middle Atlantic Bight [0.7° ± 0.3°C (100 yr)⁻¹], whereas trends are weakly cooling or not significant in the South Atlantic Bight [−0.1° ± 0.3°C (100 yr)⁻¹] and off Florida [−0.3° ± 0.2°C (100 yr)⁻¹]. Over the last century, temperatures along the northeastern U.S. coast have warmed at a rate 1.8–2.5 times the regional atmospheric temperature trend but are comparable to warming rates for the Arctic and Labrador, the source of coastal ocean waters north of Cape Hatteras (36°N). South of Cape Hatteras, coastal ocean temperature trends match the regional atmospheric temperature trend. The observations and a simple model show that along-shelf transport, associated with the mean coastal current system running from Labrador to Cape Hatteras, is the mechanism controlling long-term temperature changes for this region and not the local air–sea exchange of heat. Close

• 59. [Article] Thermoperiods and soil temperatures as they affect growth and dormancy of Douglas-fir seedlings of different geographic origin

  The effects of a range of thermoperiods and soil temperatures upon growth of Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) seedlings were studied. The seeds, of varieties glauca and menziesii, came ...

  Citation × Citation Citation Abstract Copy Title: Thermoperiods and soil temperatures as they affect growth and dormancy of Douglas-fir seedlings of different geographic origin Author: Lavender, Denis P., Oregon State University. Forest Research Laboratory, Overton, W. Scott The effects of a range of thermoperiods and soil temperatures upon growth of Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) seedlings were studied. The seeds, of varieties glauca and menziesii, came from eight widely separated areas. Plants from both varieties made maximum growth with soil and air temperatures between 18 and 24 C during the 20 weeks of the study. Little requirement for diurnal fluctuation in temperature was evident. Low soil temperatures greatly reduced growth and hastened dormancy of plants grown under all the thermoperiods tested. The effects of a range of thermoperiods and soil temperatures upon the initiation of dormancy in var. menziesii and var. glauca seedlings grown under a 9-hour daily photoperiod also were investigated. Low air temperatures generally postponed initiation of dormancy of var. menziesii seedlings, but warm days and cool nights were most effective in postponing dormancy of var. glauca plants. Soil temperatures had no consistent effect upon the initiation of dormancy under the 9-hour photoperiod. Title: Thermoperiods and soil temperatures as they affect growth and dormancy of Douglas-fir seedlings of different geographic origin Author: Lavender, Denis P., Oregon State University. Forest Research Laboratory, Overton, W. Scott The effects of a range of thermoperiods and soil temperatures upon growth of Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) seedlings were studied. The seeds, of varieties glauca and menziesii, came from eight widely separated areas. Plants from both varieties made maximum growth with soil and air temperatures between 18 and 24 C during the 20 weeks of the study. Little requirement for diurnal fluctuation in temperature was evident. Low soil temperatures greatly reduced growth and hastened dormancy of plants grown under all the thermoperiods tested. The effects of a range of thermoperiods and soil temperatures upon the initiation of dormancy in var. menziesii and var. glauca seedlings grown under a 9-hour daily photoperiod also were investigated. Low air temperatures generally postponed initiation of dormancy of var. menziesii seedlings, but warm days and cool nights were most effective in postponing dormancy of var. glauca plants. Soil temperatures had no consistent effect upon the initiation of dormancy under the 9-hour photoperiod. Close

• 60. [Article] Variation in air and soil temperatures in forest communities on the H. J. Andrews Experimental Forest, 1970-1972

  Best copy available.

  Citation × Citation Citation Abstract Copy Title: Variation in air and soil temperatures in forest communities on the H. J. Andrews Experimental Forest, 1970-1972 Author: Zobel, Donald B., McKee, Arthur, Hawk, Glenn M., U.S. International Biological Program. Coniferous Forest Biome, Dyrness, C. T., University of Washington Best copy available. Title: Variation in air and soil temperatures in forest communities on the H. J. Andrews Experimental Forest, 1970-1972 Author: Zobel, Donald B., McKee, Arthur, Hawk, Glenn M., U.S. International Biological Program. Coniferous Forest Biome, Dyrness, C. T., University of Washington Best copy available. Close

• 61. [Article] Resistance of three freshwater fishes to fluctuating thermal environments

  The resistance to elevated temperatures of three species of freshwater fishes, Oncorhynchus kisutch, Rhinichthys osculus nubilus, and Cottus perplexus was studied. Rock Creek and Greasy Creek, Benton ...

  Citation × Citation Citation Abstract Copy Title: Resistance of three freshwater fishes to fluctuating thermal environments Author: DeHart, Douglas Alan The resistance to elevated temperatures of three species of freshwater fishes, Oncorhynchus kisutch, Rhinichthys osculus nubilus, and Cottus perplexus was studied. Rock Creek and Greasy Creek, Benton County, Oregon, were surveyed to evaluate the nature of thermal stress encountered in the small cold water stream environment. Resistance to constant temperature was determined experimentally by measuring time to death at fixed levels. R. osculus and C. perplexus were found to be more resistant to elevated temperatures than O. kisutch. For fish acclimated to 20° C the incipient lethal level was found to be 25° C for C. perplexus, and 29.5° C for R. osculus. An apparatus was constructed to simulate the diel temperature regime observed in the study streams. The resistance of the three species to dielly fluctuating temperature was explored. The portion of the time temperature curve above the incipient lethal level was determined to be the critical region in relation to thermal resistance. Evidence was found for accumulation of thermal effects over periods of several days. Median resistance of O. kisutch exposed to 6 hours over their incipient lethal temperature per diel cycle with a diel maximum of 27° C was 1.5 cycles. A method of predicting resistance to cyclic exposures to elevated temperature was developed. Implications of the nature of thermal resistance in the temperature regime in small streams are discussed. Title: Resistance of three freshwater fishes to fluctuating thermal environments Author: DeHart, Douglas Alan The resistance to elevated temperatures of three species of freshwater fishes, Oncorhynchus kisutch, Rhinichthys osculus nubilus, and Cottus perplexus was studied. Rock Creek and Greasy Creek, Benton County, Oregon, were surveyed to evaluate the nature of thermal stress encountered in the small cold water stream environment. Resistance to constant temperature was determined experimentally by measuring time to death at fixed levels. R. osculus and C. perplexus were found to be more resistant to elevated temperatures than O. kisutch. For fish acclimated to 20° C the incipient lethal level was found to be 25° C for C. perplexus, and 29.5° C for R. osculus. An apparatus was constructed to simulate the diel temperature regime observed in the study streams. The resistance of the three species to dielly fluctuating temperature was explored. The portion of the time temperature curve above the incipient lethal level was determined to be the critical region in relation to thermal resistance. Evidence was found for accumulation of thermal effects over periods of several days. Median resistance of O. kisutch exposed to 6 hours over their incipient lethal temperature per diel cycle with a diel maximum of 27° C was 1.5 cycles. A method of predicting resistance to cyclic exposures to elevated temperature was developed. Implications of the nature of thermal resistance in the temperature regime in small streams are discussed. Close

• 62. [Article] Effect of high temperature drying on bending and shear strengths of western hemlock

  The advantages of high-temperature drying are faster drying, reduced inventory, reduced energy requirements, and reduced equilibrium moisture content. However the disadvantages are higher initial costs ...

  Citation × Citation Citation Abstract Copy Title: Effect of high temperature drying on bending and shear strengths of western hemlock Author: Thiam, Massamba The advantages of high-temperature drying are faster drying, reduced inventory, reduced energy requirements, and reduced equilibrium moisture content. However the disadvantages are higher initial costs of the kiln, greater power needs, knot dropout, and reduction in some strength properties. The latter was the subject of this study. Three hundred pieces of No.2 and Better nominal 42 by 145 mm (nominal 2 by 6 inches) by 2400 mm western hemlock were kiln-dried at high (116°C dry bulb and 90°C wet bulb) and conventional (82°C dry bulb and 66°C wet bulb) temperatures to a 15 % moisture content. Drying times at the high temperature condition were 50 % less than at the conventional temperature. The lower value of moisture content at equilibrium observed for the wood dried at high temperature was not statistically different from that of the wood dried at conventional temperature. High temperature drying had no significant effect on mean modulus of elasticity or modulus of rupture. However, an increase in temperature resulted in a significant decrease of shear strength. Values determined by static bending and shear parallel to the grain tests are reported. Title: Effect of high temperature drying on bending and shear strengths of western hemlock Author: Thiam, Massamba The advantages of high-temperature drying are faster drying, reduced inventory, reduced energy requirements, and reduced equilibrium moisture content. However the disadvantages are higher initial costs of the kiln, greater power needs, knot dropout, and reduction in some strength properties. The latter was the subject of this study. Three hundred pieces of No.2 and Better nominal 42 by 145 mm (nominal 2 by 6 inches) by 2400 mm western hemlock were kiln-dried at high (116°C dry bulb and 90°C wet bulb) and conventional (82°C dry bulb and 66°C wet bulb) temperatures to a 15 % moisture content. Drying times at the high temperature condition were 50 % less than at the conventional temperature. The lower value of moisture content at equilibrium observed for the wood dried at high temperature was not statistically different from that of the wood dried at conventional temperature. High temperature drying had no significant effect on mean modulus of elasticity or modulus of rupture. However, an increase in temperature resulted in a significant decrease of shear strength. Values determined by static bending and shear parallel to the grain tests are reported. Close

• 63. [Article] Distributed temperature sensing with neodymium-doped optical fiber

  Polymer electrolyte membrane (PEM) fuel cells are being studied for use as high efficiency power plants in alternative fuel vehicles. To maintain high efficiency the operating temperatures of the membranes ...

  Citation × Citation Citation Abstract Copy Title: Distributed temperature sensing with neodymium-doped optical fiber Author: Lounsbury, Jimson S. Polymer electrolyte membrane (PEM) fuel cells are being studied for use as high efficiency power plants in alternative fuel vehicles. To maintain high efficiency the operating temperatures of the membranes in these fuel cells must be closely monitored and controlled. However, the environment inside of the fuel cell is not favorable for traditional temperature sensing, so a new optical-fiber-based, distributed temperature sensor was proposed to address this need. This thesis investigates the properties of neodymium-doped optical fiber for use as a distributed temperature sensor for PEM fuel cells. The optical absorption spectrum was measured to identify the energy band structure and determine upconversion excitation schemes. The temperature coefficient of the Nd³⁺-doped silica fiber fluorescence decay time was measured for several bands of emission. Finally, two-photon upconversion was attempted from the lower excited states of Nd:YAG and Nd:silica. Title: Distributed temperature sensing with neodymium-doped optical fiber Author: Lounsbury, Jimson S. Polymer electrolyte membrane (PEM) fuel cells are being studied for use as high efficiency power plants in alternative fuel vehicles. To maintain high efficiency the operating temperatures of the membranes in these fuel cells must be closely monitored and controlled. However, the environment inside of the fuel cell is not favorable for traditional temperature sensing, so a new optical-fiber-based, distributed temperature sensor was proposed to address this need. This thesis investigates the properties of neodymium-doped optical fiber for use as a distributed temperature sensor for PEM fuel cells. The optical absorption spectrum was measured to identify the energy band structure and determine upconversion excitation schemes. The temperature coefficient of the Nd³⁺-doped silica fiber fluorescence decay time was measured for several bands of emission. Finally, two-photon upconversion was attempted from the lower excited states of Nd:YAG and Nd:silica. Close

• 64. [Article] Genetic framework for flowering-time regulation by ambient temperature-responsive miRNAs in Arabidopsis

  Flowering is the primary trait affected by ambient temperature changes. Plant microRNAs (miRNAs) are small non-coding RNAs playing an important regulatory role in plant development. In this study, to elucidate ...

  Citation × Citation Citation Abstract Copy Title: Genetic framework for flowering-time regulation by ambient temperature-responsive miRNAs in Arabidopsis Author: Kim, Wanhui, Lee, Jeong Hwan, Lee, Hanna, Carrington, James C., Fitzgerald, Heather, Ahn, Ji Hoon, Yoo, Seung Kwan, Yoo, Seong Jeon Flowering is the primary trait affected by ambient temperature changes. Plant microRNAs (miRNAs) are small non-coding RNAs playing an important regulatory role in plant development. In this study, to elucidate the mechanism of flowering-time regulation by small RNAs, we identified six ambient temperature-responsive miRNAs (miR156, miR163, miR169, miR172, miR398 and miR399) in Arabidopsis via miRNA microarray and northern hybridization analyses. We also determined the expression profile of 120 unique miRNA loci in response to ambient temperature changes by miRNA northern hybridization analysis. The expression of the ambient temperature-responsive miRNAs and their target genes was largely anticorrelated at two different temperatures (16 and 23 C). Interestingly, a lesion in short vegetative phase (SVP), a key regulator within the thermosensory pathway, caused alteration in the expression of miR172 and a subset of its target genes, providing a link between a thermosensory pathway gene and miR172. The miR172- overexpressing plants showed a temperatureindependent early flowering phenotype, suggesting that modulation of miR172 expression leads to temperature insensitivity. Taken together, our results suggest a genetic framework for flowering-time regulation by ambient temperature-responsive miRNAs under non-stress temperature conditions. Title: Genetic framework for flowering-time regulation by ambient temperature-responsive miRNAs in Arabidopsis Author: Kim, Wanhui, Lee, Jeong Hwan, Lee, Hanna, Carrington, James C., Fitzgerald, Heather, Ahn, Ji Hoon, Yoo, Seung Kwan, Yoo, Seong Jeon Flowering is the primary trait affected by ambient temperature changes. Plant microRNAs (miRNAs) are small non-coding RNAs playing an important regulatory role in plant development. In this study, to elucidate the mechanism of flowering-time regulation by small RNAs, we identified six ambient temperature-responsive miRNAs (miR156, miR163, miR169, miR172, miR398 and miR399) in Arabidopsis via miRNA microarray and northern hybridization analyses. We also determined the expression profile of 120 unique miRNA loci in response to ambient temperature changes by miRNA northern hybridization analysis. The expression of the ambient temperature-responsive miRNAs and their target genes was largely anticorrelated at two different temperatures (16 and 23 C). Interestingly, a lesion in short vegetative phase (SVP), a key regulator within the thermosensory pathway, caused alteration in the expression of miR172 and a subset of its target genes, providing a link between a thermosensory pathway gene and miR172. The miR172- overexpressing plants showed a temperatureindependent early flowering phenotype, suggesting that modulation of miR172 expression leads to temperature insensitivity. Taken together, our results suggest a genetic framework for flowering-time regulation by ambient temperature-responsive miRNAs under non-stress temperature conditions. Close

• 65. [Article] Modeling a heat regenerator-reactor with temperature dependent gas properties

  This thesis examines the transient response of a packed bed heat regenerator when heated from an initial uniform bed temperature. Very large (1700 K) temperature differences were studied as well as the ...

  Citation × Citation Citation Abstract Copy Title: Modeling a heat regenerator-reactor with temperature dependent gas properties Author: Kulkarni, Milind S. This thesis examines the transient response of a packed bed heat regenerator when heated from an initial uniform bed temperature. Very large (1700 K) temperature differences were studied as well as the effect of simultaneous chemical reaction in the gas phase. First the effects of temperature on physical and transport properties were studied in detail in the absence of a reaction. Models with compressible flow were compared with conventional models with constant properties and incompressible flow. Several measures of the regenerator's response to a step change in inlet gas temperature were calculated to characterize the spread of the temperature front. Variances of the spatial derivative of the gas temperature profile and the time derivative of the product gas temperature were used to evaluate thermal efficiency. The effects of an exothermic homogeneous gas phase reaction in the regenerator process were also studied. Several simple kinetic schemes and inlet conditions were simulated and the profiles of reaction rate and conversion as well as temperature were analyzed. Title: Modeling a heat regenerator-reactor with temperature dependent gas properties Author: Kulkarni, Milind S. This thesis examines the transient response of a packed bed heat regenerator when heated from an initial uniform bed temperature. Very large (1700 K) temperature differences were studied as well as the effect of simultaneous chemical reaction in the gas phase. First the effects of temperature on physical and transport properties were studied in detail in the absence of a reaction. Models with compressible flow were compared with conventional models with constant properties and incompressible flow. Several measures of the regenerator's response to a step change in inlet gas temperature were calculated to characterize the spread of the temperature front. Variances of the spatial derivative of the gas temperature profile and the time derivative of the product gas temperature were used to evaluate thermal efficiency. The effects of an exothermic homogeneous gas phase reaction in the regenerator process were also studied. Several simple kinetic schemes and inlet conditions were simulated and the profiles of reaction rate and conversion as well as temperature were analyzed. Close

• 66. [Article] Variation of Surface Air Temperature in Complex Terrain

  Data from three micronetworks with eddy correlation data and three additional micronetworks without eddy correlation data are analyzed to study the spatial variability of surface air temperature in complex ...

  Citation × Citation Citation Abstract Copy Title: Variation of Surface Air Temperature in Complex Terrain Author: Mahrt, L. Data from three micronetworks with eddy correlation data and three additional micronetworks without eddy correlation data are analyzed to study the spatial variability of surface air temperature in complex terrain. A simple similarity relationship is constructed to relate the spatial variation of air temperature along the slope to the thermal forcing and mixing. Mixing is not included in present empirical formulations of the surface air temperature distribution in complex terrain. The development of surface temperature gradients along the slope, resulting from surface heating or cooling, is bounded by a maximum (or saturated) value, where a further increase of temperature gradients is restricted by redistribution of heat by thermally driven slope circulations. Although much of the spatial variation of the surface air temperature is governed by complex three-dimensionality and surface vegetation, a relatively simple relationship is able to account for much of the diurnal and day-to-day variation of the spatial distribution of air temperature. This relationship requires information on the surface heat flux and friction velocity over a reference surface. Required generalizations of the relationship are outlined before it can be applied to an arbitrary site. Title: Variation of Surface Air Temperature in Complex Terrain Author: Mahrt, L. Data from three micronetworks with eddy correlation data and three additional micronetworks without eddy correlation data are analyzed to study the spatial variability of surface air temperature in complex terrain. A simple similarity relationship is constructed to relate the spatial variation of air temperature along the slope to the thermal forcing and mixing. Mixing is not included in present empirical formulations of the surface air temperature distribution in complex terrain. The development of surface temperature gradients along the slope, resulting from surface heating or cooling, is bounded by a maximum (or saturated) value, where a further increase of temperature gradients is restricted by redistribution of heat by thermally driven slope circulations. Although much of the spatial variation of the surface air temperature is governed by complex three-dimensionality and surface vegetation, a relatively simple relationship is able to account for much of the diurnal and day-to-day variation of the spatial distribution of air temperature. This relationship requires information on the surface heat flux and friction velocity over a reference surface. Required generalizations of the relationship are outlined before it can be applied to an arbitrary site. Close

• 67. [Article] A second forecast of temperature conditions in Brownlee Reservoir and in the Snake River below Brownlee Dam

  A graph is presented which shows the average annual temperature depth profile which has been computed and estimated for the Brownlee Reservoir. Forecast computations and estimations are for a median river ...

  Citation × Citation Citation Abstract Copy Title: A second forecast of temperature conditions in Brownlee Reservoir and in the Snake River below Brownlee Dam Author: Oregon State College. School of Science, Burt, Wayne V., U.S. Fish and Wildlife Service A graph is presented which shows the average annual temperature depth profile which has been computed and estimated for the Brownlee Reservoir. Forecast computations and estimations are for a median river flow year. The graph also contains forecasts of the annual temperature cycle for the Snake River below Brownlee Dam. Title: A second forecast of temperature conditions in Brownlee Reservoir and in the Snake River below Brownlee Dam Author: Oregon State College. School of Science, Burt, Wayne V., U.S. Fish and Wildlife Service A graph is presented which shows the average annual temperature depth profile which has been computed and estimated for the Brownlee Reservoir. Forecast computations and estimations are for a median river flow year. The graph also contains forecasts of the annual temperature cycle for the Snake River below Brownlee Dam. Close

• 68. [Article] The thermal regulation, microclimate, and distribution of the mountain beaver, Aplodontia rufa pacifica Merriam

  An investigation was undertaken to determine the role that temperature might play in limiting the distribution of the mountain beaver, Aplodontia rufa. A field study was carried on from August, 1965, through ...

  Citation × Citation Citation Abstract Copy Title: The thermal regulation, microclimate, and distribution of the mountain beaver, Aplodontia rufa pacifica Merriam Author: Johnson, Sheldon Robert An investigation was undertaken to determine the role that temperature might play in limiting the distribution of the mountain beaver, Aplodontia rufa. A field study was carried on from August, 1965, through August, 1966, in the coast mountains of Benton County, Oregon, and consisted of measuring the annual temperature cycle of the burrows in conjunction with air temperatures taken at a height of six cm above the soil surface. A laboratory study was conducted to determine the effects of ambient temperature on body temperature, metabolic rate, thermal conductance, insensible water loss, and heart rate. The burrow system was characterized by a cool and stable microclimate. The temperature above the soil showed a maximum annual fluctuation of 40.5°C, the temperature within the burrows varied 18.3°C, with a weekly variation in burrow temperature of not more than 4°C. Annual range in mean burrow temperature was from 2° to 14°C. The mean body temperature of Aplodontia, over an ambient temperature range of from 4° to 290°C was 37.60°C. Free-living animals had a mean body temperature of 38.0°C. Hyperthermia began at ambient temperatures above 29°C and a lethal body temperature of approximately 42°C was reached after a two hour exposure to temperatures between 32° and 35°C. Aplodontia lacked a thermoneutral zone and minimal metabolic rates were recorded at high ambient temperatures when the animals were hyperthermic. Under conditions of heat stress, mean metabolicrateswere 65 percent of the values predicted by Kleiber's equation. These animals were lethargic, their respiration rates decreased to as low as 18 per minute with minimal heart rates between 60 and 100 beats per minute. The mean minimal recorded heart rates, based on body weight, were 38 percent of that predicted. Aplodontia had a minimal thermal conductance of 0.195 cal/g/hr/°C which could only be increased by a factor of 1.84. Winter animals had an effective insulation L. 23 times that of summer animals. This raised the lower critical temperature of summer animals by 4°C (19° to 23°C). Aplodontia required a six degree thermal gradient to dissipate its minimal heat production. Insensible water loss could only be increased by a factor of 2.3 over the ambient temperature range of 12° to 31.5°C. At the latter ambient temperature, evaporative heat loss accounted for only 22 percent of Aplodontia's total heat loss. The results of this investigation indicated that high environmental temperatures may act as an important limiting factor in the distribution of the mountain beaver which lacks adequate mechanisms to avoid heat stress. Title: The thermal regulation, microclimate, and distribution of the mountain beaver, Aplodontia rufa pacifica Merriam Author: Johnson, Sheldon Robert An investigation was undertaken to determine the role that temperature might play in limiting the distribution of the mountain beaver, Aplodontia rufa. A field study was carried on from August, 1965, through August, 1966, in the coast mountains of Benton County, Oregon, and consisted of measuring the annual temperature cycle of the burrows in conjunction with air temperatures taken at a height of six cm above the soil surface. A laboratory study was conducted to determine the effects of ambient temperature on body temperature, metabolic rate, thermal conductance, insensible water loss, and heart rate. The burrow system was characterized by a cool and stable microclimate. The temperature above the soil showed a maximum annual fluctuation of 40.5°C, the temperature within the burrows varied 18.3°C, with a weekly variation in burrow temperature of not more than 4°C. Annual range in mean burrow temperature was from 2° to 14°C. The mean body temperature of Aplodontia, over an ambient temperature range of from 4° to 290°C was 37.60°C. Free-living animals had a mean body temperature of 38.0°C. Hyperthermia began at ambient temperatures above 29°C and a lethal body temperature of approximately 42°C was reached after a two hour exposure to temperatures between 32° and 35°C. Aplodontia lacked a thermoneutral zone and minimal metabolic rates were recorded at high ambient temperatures when the animals were hyperthermic. Under conditions of heat stress, mean metabolicrateswere 65 percent of the values predicted by Kleiber's equation. These animals were lethargic, their respiration rates decreased to as low as 18 per minute with minimal heart rates between 60 and 100 beats per minute. The mean minimal recorded heart rates, based on body weight, were 38 percent of that predicted. Aplodontia had a minimal thermal conductance of 0.195 cal/g/hr/°C which could only be increased by a factor of 1.84. Winter animals had an effective insulation L. 23 times that of summer animals. This raised the lower critical temperature of summer animals by 4°C (19° to 23°C). Aplodontia required a six degree thermal gradient to dissipate its minimal heat production. Insensible water loss could only be increased by a factor of 2.3 over the ambient temperature range of 12° to 31.5°C. At the latter ambient temperature, evaporative heat loss accounted for only 22 percent of Aplodontia's total heat loss. The results of this investigation indicated that high environmental temperatures may act as an important limiting factor in the distribution of the mountain beaver which lacks adequate mechanisms to avoid heat stress. Close

• 69. [Article] Developmental anatomy of Phaseolus vulgaris L. as influenced by temperature

  Bush snap beans (Phaseolus vulgaris L.) cvs 'G5O' (Gallatin 50) and 'OSU58' (Oregon 58) were used for anatomical and morphological studies of their responses to three levels of temperature. The plants ...

  Citation × Citation Citation Abstract Copy Title: Developmental anatomy of Phaseolus vulgaris L. as influenced by temperature Author: Wivutvongvana, Manee Bush snap beans (Phaseolus vulgaris L.) cvs 'G5O' (Gallatin 50) and 'OSU58' (Oregon 58) were used for anatomical and morphological studies of their responses to three levels of temperature. The plants were grown in a controlled chamber under a 16-hour photoperiod at 60°/50°, 70°/60° and 80°/70°F (day/night temperature), respectively. The leaf primordia were initiated in spiral phyllotaxy. They were oriented perpendicular to their particular stipule primordia. Decussate phyllotaxy or a mixture between decussate and spiral phyllotaxy within the same plant was observed under stress condition. Low temperature decreased the number of leaf primordia per plant and delayed the initiation. Initiation of the axillary bud primordia was delayed by low temperature when compared with medium and high temperatures. The axillary bud of the uppermost leaf was the first triad primordium of the plant. It was observed at seven to nine days after planting at medium or high temperature, and at 17 and 14 days at low temperature in 'G5O' and 'OSU58', respectively. The initiation of the triad primordia of the terminal raceme of the main shoot and the primordium of the uppermost leaf of the lateral branches were also delayed by low temperature. The initiation in 'G50' was more affected by low temperature than'OSU58'. The development of the primordia was delayed by low temperature in both cultivars with the development in 'G50' being more affected than in 'OSU58'. This delay was observed in the primordium of the uppermost leaf and the first primordium of the terminal raceme of the main shoot. The opening of flowers followed the sequence of floral initiation and development. Regardless of temperature, the first flower to open was the triad of the uppermost leaf. The first triad of the terminal raceme also opened with the first group, or in some cases, with the second group. The second group of opened flowers was of the non-leaf and the one-leaf branches. The third group was the upper triad of the terminal raceme, the two-leaf branch and the branches of the first node. The time required for opening of flowers of the second and the third group was longer than the first one. Overlapping of the two later groups was observed in 'OSU58' at high and low temperatures. Seed germination and growth of seedlings were markedly delayed by low temperature. The number of nodes was decreased. The time requirement for the first flower to open was significantly lengthened as well as the duration of flowering. The pattern of flowering was changed. Concentrated flowering within a short period was observed at medium and high temperatures, whereas uniform flowering within a long period was seen at low temperature. Different responses were observed in the number of opened flowers per plant and the percentage of pod set as a function of temperature, The highest number of opened flowers in 'G50' was observed at medium temperature, whereas highest percentage of pod set was obtained at low temperature. 'OSU58' showed reversed responses from 'G50'. High temperature decreased the percentage of pod set in both cultivars. Title: Developmental anatomy of Phaseolus vulgaris L. as influenced by temperature Author: Wivutvongvana, Manee Bush snap beans (Phaseolus vulgaris L.) cvs 'G5O' (Gallatin 50) and 'OSU58' (Oregon 58) were used for anatomical and morphological studies of their responses to three levels of temperature. The plants were grown in a controlled chamber under a 16-hour photoperiod at 60°/50°, 70°/60° and 80°/70°F (day/night temperature), respectively. The leaf primordia were initiated in spiral phyllotaxy. They were oriented perpendicular to their particular stipule primordia. Decussate phyllotaxy or a mixture between decussate and spiral phyllotaxy within the same plant was observed under stress condition. Low temperature decreased the number of leaf primordia per plant and delayed the initiation. Initiation of the axillary bud primordia was delayed by low temperature when compared with medium and high temperatures. The axillary bud of the uppermost leaf was the first triad primordium of the plant. It was observed at seven to nine days after planting at medium or high temperature, and at 17 and 14 days at low temperature in 'G5O' and 'OSU58', respectively. The initiation of the triad primordia of the terminal raceme of the main shoot and the primordium of the uppermost leaf of the lateral branches were also delayed by low temperature. The initiation in 'G50' was more affected by low temperature than'OSU58'. The development of the primordia was delayed by low temperature in both cultivars with the development in 'G50' being more affected than in 'OSU58'. This delay was observed in the primordium of the uppermost leaf and the first primordium of the terminal raceme of the main shoot. The opening of flowers followed the sequence of floral initiation and development. Regardless of temperature, the first flower to open was the triad of the uppermost leaf. The first triad of the terminal raceme also opened with the first group, or in some cases, with the second group. The second group of opened flowers was of the non-leaf and the one-leaf branches. The third group was the upper triad of the terminal raceme, the two-leaf branch and the branches of the first node. The time required for opening of flowers of the second and the third group was longer than the first one. Overlapping of the two later groups was observed in 'OSU58' at high and low temperatures. Seed germination and growth of seedlings were markedly delayed by low temperature. The number of nodes was decreased. The time requirement for the first flower to open was significantly lengthened as well as the duration of flowering. The pattern of flowering was changed. Concentrated flowering within a short period was observed at medium and high temperatures, whereas uniform flowering within a long period was seen at low temperature. Different responses were observed in the number of opened flowers per plant and the percentage of pod set as a function of temperature, The highest number of opened flowers in 'G50' was observed at medium temperature, whereas highest percentage of pod set was obtained at low temperature. 'OSU58' showed reversed responses from 'G50'. High temperature decreased the percentage of pod set in both cultivars. Close

• 70. [Article] The influence of climate change and restoration on stream temperature

  Water temperature is an essential property of a stream. Temperature regulates physical and biochemical processes in aquatic habitats. Various factors related to climatic conditions, landscape characteristics, ...

  Citation × Citation Citation Abstract Copy Title: The influence of climate change and restoration on stream temperature Author: Diabat, Mousa Water temperature is an essential property of a stream. Temperature regulates physical and biochemical processes in aquatic habitats. Various factors related to climatic conditions, landscape characteristics, and channel structure directly influence stream temperature. Numerous studies indicate that increased average air temperature during the past century has led to stream warming across the world. The trend of stream warming was also present in spring-fed watersheds, where summer flow has decreased. In addition, anthropogenic practices that alter the natural landscape and channel structure, such as forest management, agriculture, and mining contributed to stream warming. For example, deforested and unshaded stream reaches or dredged channels were warmer than shaded reaches and meandering streams. Stream temperatures in North American lotic habitats are of a specific concern due to their significant economic, cultural, and ecological value. With climate projections indicating that air temperature will only continue to rise throughout the 21st century, cold- or cool-water organisms, especially fishes, will be affected. Therefore, there is a strong need to better understand the impacts of changing climate, riparian landscape, and channel structure on a stream's heat budget. This may assist in restoring the historic thermal regime in impacted sites and mitigating the impacts of future climate change. This study looks into the relative influences of the different factors on a stream's heat budget with three manuscripts: one on stream temperature response to diel timing of air warming, one on stream temperature response to changes in air temperature, flow, and riparian vegetation, and one on stream temperature response to air warming and channel reconstruction. I used the software Heat Source version 8.05 to simulate stream temperature for all three analyses along the Middle Fork John Day River, Oregon USA. Two of the manuscripts were applied to an upper 37 km section of the Middle Fork John Day River (presented in chapter 2 and 3), where the third manuscript was applied to a 1.5-km section. The sensitivity analysis of stream temperature response to diel timing of air warming (Chapter 2: Diel Timing of Warmer Air under Climate Change Affects Magnitude, Timing, and Duration of Stream Temperature Change) was based on scenarios representing uniform air warming over the diel period, daytime warming, and nighttime warming. Uniform warming of air temperature is a simple representation of increases in the average daily or monthly temperatures generated by the 'delta method'. The delta method relies on adding a constant value to the air temperature time-series data. This constant value is the difference (delta) between base case average air temperatures and the projected one. Scenarios of daytime or nighttime warming represent conditions under which most of the warming of the air occurs during the daytime or the nighttime, respectively. I simulated the stream temperature response to warmer air conditions of +2 °C and +4 °C in daily average for all three cases of air warming conditions. The three cases of different diel distributions of air warming generated 7-day average daily maximum stream temperature (7DADM) increases of approximately +1.8 °C ± 0.1 °C at the downstream end of the study section relative to the base case. In most parts of the reach, the three distributions of air warming generated different ranges of stream temperatures, different 7DADM values, different durations of stream temperature changes, and different average daily temperatures. Changes of stream temperature were out of phase with imposed changes of air temperature. Therefore, nighttime warming of air temperatures would cause the greatest increase in maximum daily stream temperature, which typically occurs during the daytime. The sensitivity analysis of the relative influences of changes in air temperature, stream flow, and riparian vegetation on stream temperature (Chapter 3: Assessing Stream Temperature Response to Cumulative Influence of Changing Air Temperature, Flow, and Riparian Vegetation). This study summarized stream temperature simulation in 36 scenarios representing possible manifestations of 21st century climate conditions and land management strategies. In addition to existing conditions (base case) of flow, air temperature, and riparian vegetation, scenarios consisted of: two air temperature increases of 2 °C and 4 °C, two stream flow variations of +30% and -30%, three spatially uniform riparian vegetation conditions that create averages of effective shade 7%, 34%, and 79%, in addition to 14% for base case conditions. Results suggest that variation in riparian vegetation was the dominant factor influencing stream temperature because it regulates incoming shortwave radiation, the largest heat input to the stream, while variation in stream flow has a negligible influence. Results indicated that increasing the effective shade along the study section, particularly in the currently unshaded sections, could mitigate the influence of increasing air temperature, and would reduce stream temperature maxima below current values even under future climate conditions of warmer air. With the small influence it had, increasing stream flow reduced the 7DADM under low shade conditions. However, increasing stream flow showed counterintuitive results as it contributed to increasing stream temperature maxima when the stream was heavily shaded. The applied study examined the stream temperature response to restoration practices and their potential to mitigate the influence of warmer air conditions (Chapter 4: Estimating Stream Temperature Response to Restoring Channel and Riparian Vegetation and the Potential to Mitigate Warmer Air Conditions). This study focused on a 1.5 km section along the upper part of the Middle Fork John Day River that was modified due to past anthropogenic activities of mining for gold and timber harvest. Currently, the riparian vegetation of the study site is mostly shrubs and stands of short trees. Restoration designs call for the restoration of both the channel structure and replanting the riparian vegetation. Simulation results showed that the 7DADM was higher in the restored channel than the existing channel with both conditions of low and high effective shade conditions. However, a combined restoration practice of channel reconstruction and medium effective shade conditions reduced stream temperature maxima more than restoring riparian vegetation alone. In addition, results showed that restoring riparian vegetation was sufficient to mitigate the influence of warmer air on stream temperature, while restoring the channel alone is not. Heat budget analysis showed that heat accumulation during the daytime increased in the restored channel, which was longer, narrower, and deeper than the existing channel. It is important to emphasize that stream temperature is one of many goals that restoration activities aim to improve. Furthermore, differences in 7DADM among the different scenarios of restoration are negligible. Such small differences could hardly be measure. While this study examined a short section of 1.5 km, longer stream sections may increase the differences in 7DADM. Primary conclusions of this study are: 1) daily maxima of stream temperature will increase in response to increased air temperature regardless of the distribution of air warming during the diel cycle; 2) nighttime air warming caused a greater increase in stream temperature maximum than daytime warming; 3) riparian vegetation was the dominant factor on stream's heat budget, more than air temperature or stream flow; 4) restoring riparian vegetation mitigated the influence of warmer air; 5) restoring channel structure alone was not sufficient to lower temperature maxima; and 6) restoration project was most successful in improving degraded stream temperature when combined with channel reconstruction and improved riparian shade. Title: The influence of climate change and restoration on stream temperature Author: Diabat, Mousa Water temperature is an essential property of a stream. Temperature regulates physical and biochemical processes in aquatic habitats. Various factors related to climatic conditions, landscape characteristics, and channel structure directly influence stream temperature. Numerous studies indicate that increased average air temperature during the past century has led to stream warming across the world. The trend of stream warming was also present in spring-fed watersheds, where summer flow has decreased. In addition, anthropogenic practices that alter the natural landscape and channel structure, such as forest management, agriculture, and mining contributed to stream warming. For example, deforested and unshaded stream reaches or dredged channels were warmer than shaded reaches and meandering streams. Stream temperatures in North American lotic habitats are of a specific concern due to their significant economic, cultural, and ecological value. With climate projections indicating that air temperature will only continue to rise throughout the 21st century, cold- or cool-water organisms, especially fishes, will be affected. Therefore, there is a strong need to better understand the impacts of changing climate, riparian landscape, and channel structure on a stream's heat budget. This may assist in restoring the historic thermal regime in impacted sites and mitigating the impacts of future climate change. This study looks into the relative influences of the different factors on a stream's heat budget with three manuscripts: one on stream temperature response to diel timing of air warming, one on stream temperature response to changes in air temperature, flow, and riparian vegetation, and one on stream temperature response to air warming and channel reconstruction. I used the software Heat Source version 8.05 to simulate stream temperature for all three analyses along the Middle Fork John Day River, Oregon USA. Two of the manuscripts were applied to an upper 37 km section of the Middle Fork John Day River (presented in chapter 2 and 3), where the third manuscript was applied to a 1.5-km section. The sensitivity analysis of stream temperature response to diel timing of air warming (Chapter 2: Diel Timing of Warmer Air under Climate Change Affects Magnitude, Timing, and Duration of Stream Temperature Change) was based on scenarios representing uniform air warming over the diel period, daytime warming, and nighttime warming. Uniform warming of air temperature is a simple representation of increases in the average daily or monthly temperatures generated by the 'delta method'. The delta method relies on adding a constant value to the air temperature time-series data. This constant value is the difference (delta) between base case average air temperatures and the projected one. Scenarios of daytime or nighttime warming represent conditions under which most of the warming of the air occurs during the daytime or the nighttime, respectively. I simulated the stream temperature response to warmer air conditions of +2 °C and +4 °C in daily average for all three cases of air warming conditions. The three cases of different diel distributions of air warming generated 7-day average daily maximum stream temperature (7DADM) increases of approximately +1.8 °C ± 0.1 °C at the downstream end of the study section relative to the base case. In most parts of the reach, the three distributions of air warming generated different ranges of stream temperatures, different 7DADM values, different durations of stream temperature changes, and different average daily temperatures. Changes of stream temperature were out of phase with imposed changes of air temperature. Therefore, nighttime warming of air temperatures would cause the greatest increase in maximum daily stream temperature, which typically occurs during the daytime. The sensitivity analysis of the relative influences of changes in air temperature, stream flow, and riparian vegetation on stream temperature (Chapter 3: Assessing Stream Temperature Response to Cumulative Influence of Changing Air Temperature, Flow, and Riparian Vegetation). This study summarized stream temperature simulation in 36 scenarios representing possible manifestations of 21st century climate conditions and land management strategies. In addition to existing conditions (base case) of flow, air temperature, and riparian vegetation, scenarios consisted of: two air temperature increases of 2 °C and 4 °C, two stream flow variations of +30% and -30%, three spatially uniform riparian vegetation conditions that create averages of effective shade 7%, 34%, and 79%, in addition to 14% for base case conditions. Results suggest that variation in riparian vegetation was the dominant factor influencing stream temperature because it regulates incoming shortwave radiation, the largest heat input to the stream, while variation in stream flow has a negligible influence. Results indicated that increasing the effective shade along the study section, particularly in the currently unshaded sections, could mitigate the influence of increasing air temperature, and would reduce stream temperature maxima below current values even under future climate conditions of warmer air. With the small influence it had, increasing stream flow reduced the 7DADM under low shade conditions. However, increasing stream flow showed counterintuitive results as it contributed to increasing stream temperature maxima when the stream was heavily shaded. The applied study examined the stream temperature response to restoration practices and their potential to mitigate the influence of warmer air conditions (Chapter 4: Estimating Stream Temperature Response to Restoring Channel and Riparian Vegetation and the Potential to Mitigate Warmer Air Conditions). This study focused on a 1.5 km section along the upper part of the Middle Fork John Day River that was modified due to past anthropogenic activities of mining for gold and timber harvest. Currently, the riparian vegetation of the study site is mostly shrubs and stands of short trees. Restoration designs call for the restoration of both the channel structure and replanting the riparian vegetation. Simulation results showed that the 7DADM was higher in the restored channel than the existing channel with both conditions of low and high effective shade conditions. However, a combined restoration practice of channel reconstruction and medium effective shade conditions reduced stream temperature maxima more than restoring riparian vegetation alone. In addition, results showed that restoring riparian vegetation was sufficient to mitigate the influence of warmer air on stream temperature, while restoring the channel alone is not. Heat budget analysis showed that heat accumulation during the daytime increased in the restored channel, which was longer, narrower, and deeper than the existing channel. It is important to emphasize that stream temperature is one of many goals that restoration activities aim to improve. Furthermore, differences in 7DADM among the different scenarios of restoration are negligible. Such small differences could hardly be measure. While this study examined a short section of 1.5 km, longer stream sections may increase the differences in 7DADM. Primary conclusions of this study are: 1) daily maxima of stream temperature will increase in response to increased air temperature regardless of the distribution of air warming during the diel cycle; 2) nighttime air warming caused a greater increase in stream temperature maximum than daytime warming; 3) riparian vegetation was the dominant factor on stream's heat budget, more than air temperature or stream flow; 4) restoring riparian vegetation mitigated the influence of warmer air; 5) restoring channel structure alone was not sufficient to lower temperature maxima; and 6) restoration project was most successful in improving degraded stream temperature when combined with channel reconstruction and improved riparian shade. Close

• 71. [Article] The influence of environmental and physical factors on the thermal patterns of headwater streams

  A case study was performed in 2000 and 2001 to characterize the thermal pattern of four morphologically similar eastern Oregon streams and to identify the physical and environmental factors that expressed ...

  Citation × Citation Citation Abstract Copy Title: The influence of environmental and physical factors on the thermal patterns of headwater streams Author: Carr, Craig A. A case study was performed in 2000 and 2001 to characterize the thermal pattern of four morphologically similar eastern Oregon streams and to identify the physical and environmental factors that expressed significant and functionally viable relationships with stream temperature (daily maximum, daily minimum and daily rate of heating). Stream and environmental attributes were measured at various locations along each stream to provide a data set comprised of variables representing daily stream temperatures (minimum, maximum and rates of heating), daily air temperatures (minimum and maximum), shade, elevation, elevation change and length. Data from the 20 hottest days were analyzed using analysis of variance and regression-based path analysis. With the exception of those reaches that were influenced by groundwater or subsurface flow, downstream reaches consistently experienced increases in the daily maximum stream temperature. The most significant parameter with respect to daily maximum stream temperature appeared to be reach elevation; expressed through reach location in the watershed. Maximum air temperature also positively influenced maximum stream temperature however, only on streams that expressed significant variation in maximum air temperature. The dominant influence of groundwater on maximum stream temperature was also apparent. Significant reach level variation in daily minimum stream temperatures was not observed in this study, however most streams did record increases in the downstream direction. Daily minimum air temperature was consistent across all streams in expressing the most significant relationship with daily minimum stream temperature. With the exception of groundwater influenced reaches, all streams exhibited obvious downstream increases in the daily rate of stream heating. Daily minimum air temperature consistently exhibited a significant negative association with the rate of heating and a relationship was also implied between reach elevation, maximum stream temperature and minimum stream temperature and this stream temperature response. Groundwater and subsurface flow, when present, also appeared to influence the daily rate of stream heating. Resource management activities should have little impact on the parameters found, on these streams, to be associated with stream temperature. Location in the watershed and climatic influence through both minimum and maximum air temperatures emerged as the dominant factors with respect to stream thermal patterns. Title: The influence of environmental and physical factors on the thermal patterns of headwater streams Author: Carr, Craig A. A case study was performed in 2000 and 2001 to characterize the thermal pattern of four morphologically similar eastern Oregon streams and to identify the physical and environmental factors that expressed significant and functionally viable relationships with stream temperature (daily maximum, daily minimum and daily rate of heating). Stream and environmental attributes were measured at various locations along each stream to provide a data set comprised of variables representing daily stream temperatures (minimum, maximum and rates of heating), daily air temperatures (minimum and maximum), shade, elevation, elevation change and length. Data from the 20 hottest days were analyzed using analysis of variance and regression-based path analysis. With the exception of those reaches that were influenced by groundwater or subsurface flow, downstream reaches consistently experienced increases in the daily maximum stream temperature. The most significant parameter with respect to daily maximum stream temperature appeared to be reach elevation; expressed through reach location in the watershed. Maximum air temperature also positively influenced maximum stream temperature however, only on streams that expressed significant variation in maximum air temperature. The dominant influence of groundwater on maximum stream temperature was also apparent. Significant reach level variation in daily minimum stream temperatures was not observed in this study, however most streams did record increases in the downstream direction. Daily minimum air temperature was consistent across all streams in expressing the most significant relationship with daily minimum stream temperature. With the exception of groundwater influenced reaches, all streams exhibited obvious downstream increases in the daily rate of stream heating. Daily minimum air temperature consistently exhibited a significant negative association with the rate of heating and a relationship was also implied between reach elevation, maximum stream temperature and minimum stream temperature and this stream temperature response. Groundwater and subsurface flow, when present, also appeared to influence the daily rate of stream heating. Resource management activities should have little impact on the parameters found, on these streams, to be associated with stream temperature. Location in the watershed and climatic influence through both minimum and maximum air temperatures emerged as the dominant factors with respect to stream thermal patterns. Close

• 72. [Article] The influence of contemporary forest harvesting on summer stream temperatures in headwater streams of Hinkle Creek, Oregon

  Stream temperature is a water quality parameter that directly influences the quality of aquatic habitat, particularly for cold-water species such as Pacific salmonids. Forest harvesting adjacent to a stream ...

  Citation × Citation Citation Abstract Copy Title: The influence of contemporary forest harvesting on summer stream temperatures in headwater streams of Hinkle Creek, Oregon Author: Kibler, Kelly Maren Stream temperature is a water quality parameter that directly influences the quality of aquatic habitat, particularly for cold-water species such as Pacific salmonids. Forest harvesting adjacent to a stream can increase the amount of solar radiation the stream receives, which can elevate stream temperatures and impair aquatic habitat. Oregon Forest Practice Rules mandate that forest operators leave Riparian Management Areas (RMAs) adjacent to streams in order to minimize the water quality impacts from forest harvesting. However, RMAs that contain overstory merchantable conifers are not required for small non-fish-bearing streams in Oregon, thus there is potential for increases in stream temperature to occur in headwater streams after harvesting. There is concern that increases in stream temperatures and changes to onsite processes in non-fish-bearing, headwater streams may propagate downstream and impair habitat in fish-bearing streams. The objectives of the following work are to assess the effects of contemporary forest management practices on stream temperatures of small non-fish-bearing headwater streams and to develop new knowledge regarding the physical processes that control reach-level stream temperature patterns. Summer stream temperatures were measured for five years in six headwater streams in the Hinkle Creek basin in southern Oregon. After four years, four of the streams were harvested and vegetated RMAs were not left between the streams and harvest units. The watersheds of the two remaining streams were not disturbed. Post-harvest stream temperatures were monitored for one year in all six streams. Each harvested stream was paired with one unharvested stream and regression relationships for maximum, minimum and mean daily stream temperatures were developed. Changes to temperatures of harvested streams were detected by comparing the mean pre-harvest regression relationship to the mean post-harvest relationship. Change detection analyses that considered the mean response among all four harvested streams indicated that maximum daily stream temperatures did not increase after harvesting, but that minimum and mean daily temperatures decreased significantly after harvesting. Additionally, diel stream temperature fluctuations were significantly greater one year after harvesting. Pre- and post-harvest surveys of canopy closure in the harvested and unharvested streams were completed in order to compare levels of stream shading before and after harvest. The post-harvest survey quantified canopy closure from remaining overstory vegetation as well as from logging slash that partially covered the harvested streams. The surveys indicated that mean overstory canopy closure in the harvested streams decreased by 84% as a result of the harvest, but as the logging slash provided considerable cover, total canopy closure decreased by only 20%. It is possible that the logging slash effectively attenuated solar radiation and prevented extreme temperature increases in the harvested streams. However, it is likely that streamflow increased after harvesting and that the increased streamflow also prevented increases to maximum temperatures and contributed to lower minimum and mean stream temperatures. Title: The influence of contemporary forest harvesting on summer stream temperatures in headwater streams of Hinkle Creek, Oregon Author: Kibler, Kelly Maren Stream temperature is a water quality parameter that directly influences the quality of aquatic habitat, particularly for cold-water species such as Pacific salmonids. Forest harvesting adjacent to a stream can increase the amount of solar radiation the stream receives, which can elevate stream temperatures and impair aquatic habitat. Oregon Forest Practice Rules mandate that forest operators leave Riparian Management Areas (RMAs) adjacent to streams in order to minimize the water quality impacts from forest harvesting. However, RMAs that contain overstory merchantable conifers are not required for small non-fish-bearing streams in Oregon, thus there is potential for increases in stream temperature to occur in headwater streams after harvesting. There is concern that increases in stream temperatures and changes to onsite processes in non-fish-bearing, headwater streams may propagate downstream and impair habitat in fish-bearing streams. The objectives of the following work are to assess the effects of contemporary forest management practices on stream temperatures of small non-fish-bearing headwater streams and to develop new knowledge regarding the physical processes that control reach-level stream temperature patterns. Summer stream temperatures were measured for five years in six headwater streams in the Hinkle Creek basin in southern Oregon. After four years, four of the streams were harvested and vegetated RMAs were not left between the streams and harvest units. The watersheds of the two remaining streams were not disturbed. Post-harvest stream temperatures were monitored for one year in all six streams. Each harvested stream was paired with one unharvested stream and regression relationships for maximum, minimum and mean daily stream temperatures were developed. Changes to temperatures of harvested streams were detected by comparing the mean pre-harvest regression relationship to the mean post-harvest relationship. Change detection analyses that considered the mean response among all four harvested streams indicated that maximum daily stream temperatures did not increase after harvesting, but that minimum and mean daily temperatures decreased significantly after harvesting. Additionally, diel stream temperature fluctuations were significantly greater one year after harvesting. Pre- and post-harvest surveys of canopy closure in the harvested and unharvested streams were completed in order to compare levels of stream shading before and after harvest. The post-harvest survey quantified canopy closure from remaining overstory vegetation as well as from logging slash that partially covered the harvested streams. The surveys indicated that mean overstory canopy closure in the harvested streams decreased by 84% as a result of the harvest, but as the logging slash provided considerable cover, total canopy closure decreased by only 20%. It is possible that the logging slash effectively attenuated solar radiation and prevented extreme temperature increases in the harvested streams. However, it is likely that streamflow increased after harvesting and that the increased streamflow also prevented increases to maximum temperatures and contributed to lower minimum and mean stream temperatures. Close

• 73. [Article] Soil organic carbon response to six years of warming : assessing the impacts of altered diurnal temperature range

  There is a growing consensus that anthropogenic warming will impact soil organic matter (SOM). Globally, soil contains 2-3 times more carbon (C) than plants, and like plants, temperature induced change ...

  Citation × Citation Citation Abstract Copy Title: Soil organic carbon response to six years of warming : assessing the impacts of altered diurnal temperature range Author: Murphey, Virginia L. W. There is a growing consensus that anthropogenic warming will impact soil organic matter (SOM). Globally, soil contains 2-3 times more carbon (C) than plants, and like plants, temperature induced change of SOM could have significant climate repercussions. Although, the majority of warming experiments have increased day and night temperatures equally, there is evidence of greater increase in global minimum temperatures compared to midday maxima, resulting in an altered mean diurnal temperature range (DTR). Here, intact grassland mesocosms (Terracosm facility, Corvallis OR) were used to assess soil organic C (SOC) changes resulting from altered DTR over a six year period. We assessed the response of SOC to a mean temperature increase of 3.5°C with three temperature treatments: symmetric (SYM) warming of +3.5°C, asymmetric (ASYM) warming of +5°C/ +2°C at minimum and maximum daily temperature, respectively, and control treatments that were kept at ambient (AMB) temperatures. After six years of warming SOC was surprisingly unaltered by increased temperature and was more strongly influenced by plant dynamics than expected. The strongest temperature response was from soil respiration (reported as In-situ cumulative soil C mineralization) with at least 33% higher cumulative C mineralization in warming treatments. In agreement with the soil respiration response, light fraction C (<1.8g/cm³) was depleted in warming treatments (8-10% less C than AMB) at shallow depths. However, laboratory cumulative soil C mineralization, a measure of most easily degraded SOC, had a lack of response to temperature, and actually had trends for greater C in warming treatments. This response was further validated by increased soil water dissolved organic C (DOC) concentration in warming treatments. An increase in these measures suggested that plants were more influential than temperature for highly labile SOC. Aggregates, an important part of SOC allocation and sequestration, had a differential response to SYM and ASYM treatments but this was likely more directly caused by root dynamics than temperature treatment. Due to varying responses of SOC indicators, C budgets were used to assess total ecosystem C balance. We found that under AMB conditions soil was an atmospheric C sink and under both SYM and ASYM conditions soil was an atmospheric C source, with ASYM having a higher source potential than SYM. Overall, SOC responded to both temperature increase via soil respiration and differentially to temperature treatments based on plant response. We expect that a reduced diurnal temperature range could affect soil C differently than mean temperature increase, if plant differences are sustained. Title: Soil organic carbon response to six years of warming : assessing the impacts of altered diurnal temperature range Author: Murphey, Virginia L. W. There is a growing consensus that anthropogenic warming will impact soil organic matter (SOM). Globally, soil contains 2-3 times more carbon (C) than plants, and like plants, temperature induced change of SOM could have significant climate repercussions. Although, the majority of warming experiments have increased day and night temperatures equally, there is evidence of greater increase in global minimum temperatures compared to midday maxima, resulting in an altered mean diurnal temperature range (DTR). Here, intact grassland mesocosms (Terracosm facility, Corvallis OR) were used to assess soil organic C (SOC) changes resulting from altered DTR over a six year period. We assessed the response of SOC to a mean temperature increase of 3.5°C with three temperature treatments: symmetric (SYM) warming of +3.5°C, asymmetric (ASYM) warming of +5°C/ +2°C at minimum and maximum daily temperature, respectively, and control treatments that were kept at ambient (AMB) temperatures. After six years of warming SOC was surprisingly unaltered by increased temperature and was more strongly influenced by plant dynamics than expected. The strongest temperature response was from soil respiration (reported as In-situ cumulative soil C mineralization) with at least 33% higher cumulative C mineralization in warming treatments. In agreement with the soil respiration response, light fraction C (<1.8g/cm³) was depleted in warming treatments (8-10% less C than AMB) at shallow depths. However, laboratory cumulative soil C mineralization, a measure of most easily degraded SOC, had a lack of response to temperature, and actually had trends for greater C in warming treatments. This response was further validated by increased soil water dissolved organic C (DOC) concentration in warming treatments. An increase in these measures suggested that plants were more influential than temperature for highly labile SOC. Aggregates, an important part of SOC allocation and sequestration, had a differential response to SYM and ASYM treatments but this was likely more directly caused by root dynamics than temperature treatment. Due to varying responses of SOC indicators, C budgets were used to assess total ecosystem C balance. We found that under AMB conditions soil was an atmospheric C sink and under both SYM and ASYM conditions soil was an atmospheric C source, with ASYM having a higher source potential than SYM. Overall, SOC responded to both temperature increase via soil respiration and differentially to temperature treatments based on plant response. We expect that a reduced diurnal temperature range could affect soil C differently than mean temperature increase, if plant differences are sustained. Close

• 74. [Article] Temperature and the bioenergetics of Cichlasoma bimaculatum

  One means of evaluating the temperature requirements of an animal is to determine changes temperature causes in the uses and losses of energy and materials in the food the animal consumes. To develop energy ...

  Citation × Citation Citation Abstract Copy Title: Temperature and the bioenergetics of Cichlasoma bimaculatum Author: Sethi, Hari Singh One means of evaluating the temperature requirements of an animal is to determine changes temperature causes in the uses and losses of energy and materials in the food the animal consumes. To develop energy budgets for cichlids (Cichlasoma bimaculatum) at different temperatures (20, 24, 28, 32 and 36 C) data were obtained on food intake, growth (total, fat, and protein), fecal losses, maintenance requirements, and other uses and losses of energy and materials including specific dynamic action, activity, and nitrogen excretion. Starvation experiments were conducted to provide information on the metabolic cost of existence and on adjustments in body composition in the absence of food. Energy expenditure during starvation, estimated from heat of combustion data, was found to increase linearly with temperature over 4, 13 and 20 days of starvation. The caloric cost of existence per fish per day was greatest during the first four days at all temperatures and decreased as starvation was prolonged to 20 days. Caloric losses, and dry weight losses showed essentially the same thing. Protein catabolism increased regularly with temperature and decreased slightly with duration of starvation. Fat catabolism did not vary significantly with temperature but decreased markedly as starvation was prolonged. Food intake, growth, and food conversion efficiency varied greatly with changes in temperature. Cichlids were fed ad libitum on small aquatic worms of the genus Tubifex. For food consumption as well as growth, the optimum temperature dropped from 32 to 28 to 24 C as the experimental period was extended from 5 to 12 to 19 days. Optimum growth in dry weight and calories occurred at the same temperatures. Growth of cichlids through time at 20 and 28 C was nearly linear; at 24 C the curve was exponential. At 32 and 36 C, the growth curves rose and then declined. When the fish were held separately during the experiment, food conversion efficiency of cichlids was highest at 20 C and decreased with increasing temperature. Efficiencies decreased with duration of the experiment. When fish were held in groups during the experiment, efficiency was low at both high and low temperatures. The guts of the cichlids were found to contain food up to 30 hours after an ad libitum meal at all temperatures. They were reasonably empty after 36 hours. Thus, no significant correlation was found between temperature and the length of time necessary for the guts to empty. Food material not absorbed was measured by wet combustion. Percentages of absorption of unrestricted rations were found to be 83, 84, 88, 85 and 69 at 20, 24, 28, 32 and 36 C. Percentages of food absorption were much higher on the restricted ration than on the unrestricted ration. Absorption appears to have been optimal at 28 C. Specific dynamic action (SDA) was estimated at different temperatures by taking the difference between oxygen consumption of unfed and fed cichlids at the same levels of activity. SDA represented 22, 20, 19, 33 and 33 percent of the food consumed at 20, 24, 28, 32 and 36 C, when the fish were swimming at 4 cm/second. SDA was generally complete within 36 hours after feeding. Graphs showing energy and material intake, utilization, loss, and scope for growth at each temperature during different experimental periods were developed both in terms of calories per fish per day and calories per gram of fish per day. The evidence suggests that the optimum temperature for growth of this cichlid is near 24 C. Title: Temperature and the bioenergetics of Cichlasoma bimaculatum Author: Sethi, Hari Singh One means of evaluating the temperature requirements of an animal is to determine changes temperature causes in the uses and losses of energy and materials in the food the animal consumes. To develop energy budgets for cichlids (Cichlasoma bimaculatum) at different temperatures (20, 24, 28, 32 and 36 C) data were obtained on food intake, growth (total, fat, and protein), fecal losses, maintenance requirements, and other uses and losses of energy and materials including specific dynamic action, activity, and nitrogen excretion. Starvation experiments were conducted to provide information on the metabolic cost of existence and on adjustments in body composition in the absence of food. Energy expenditure during starvation, estimated from heat of combustion data, was found to increase linearly with temperature over 4, 13 and 20 days of starvation. The caloric cost of existence per fish per day was greatest during the first four days at all temperatures and decreased as starvation was prolonged to 20 days. Caloric losses, and dry weight losses showed essentially the same thing. Protein catabolism increased regularly with temperature and decreased slightly with duration of starvation. Fat catabolism did not vary significantly with temperature but decreased markedly as starvation was prolonged. Food intake, growth, and food conversion efficiency varied greatly with changes in temperature. Cichlids were fed ad libitum on small aquatic worms of the genus Tubifex. For food consumption as well as growth, the optimum temperature dropped from 32 to 28 to 24 C as the experimental period was extended from 5 to 12 to 19 days. Optimum growth in dry weight and calories occurred at the same temperatures. Growth of cichlids through time at 20 and 28 C was nearly linear; at 24 C the curve was exponential. At 32 and 36 C, the growth curves rose and then declined. When the fish were held separately during the experiment, food conversion efficiency of cichlids was highest at 20 C and decreased with increasing temperature. Efficiencies decreased with duration of the experiment. When fish were held in groups during the experiment, efficiency was low at both high and low temperatures. The guts of the cichlids were found to contain food up to 30 hours after an ad libitum meal at all temperatures. They were reasonably empty after 36 hours. Thus, no significant correlation was found between temperature and the length of time necessary for the guts to empty. Food material not absorbed was measured by wet combustion. Percentages of absorption of unrestricted rations were found to be 83, 84, 88, 85 and 69 at 20, 24, 28, 32 and 36 C. Percentages of food absorption were much higher on the restricted ration than on the unrestricted ration. Absorption appears to have been optimal at 28 C. Specific dynamic action (SDA) was estimated at different temperatures by taking the difference between oxygen consumption of unfed and fed cichlids at the same levels of activity. SDA represented 22, 20, 19, 33 and 33 percent of the food consumed at 20, 24, 28, 32 and 36 C, when the fish were swimming at 4 cm/second. SDA was generally complete within 36 hours after feeding. Graphs showing energy and material intake, utilization, loss, and scope for growth at each temperature during different experimental periods were developed both in terms of calories per fish per day and calories per gram of fish per day. The evidence suggests that the optimum temperature for growth of this cichlid is near 24 C. Close

• 75. [Article] Thermal ecology of the garter snakes Thamnophis sirtalis concinnus (Hallowell) and Thamnophis ordinoides (Baird & Girard)

  In recent years, studies dealing with temperature regulation, temperature sensitivity, and physiological responses to temperature in lizards and other reptiles have increased tremendously. It is notable ...

  Citation × Citation Citation Abstract Copy Title: Thermal ecology of the garter snakes Thamnophis sirtalis concinnus (Hallowell) and Thamnophis ordinoides (Baird & Girard) Author: Stewart, Glenn R. In recent years, studies dealing with temperature regulation, temperature sensitivity, and physiological responses to temperature in lizards and other reptiles have increased tremendously. It is notable that snakes have been largely ignored in such studies. This no doubt is due to their less direct relationship to ancestral endotherms. However, problems in the ecology of snakes themselves may be elucidated by studies of this kind. The present study deals with two species of garter snakes ( Thamnophis sirtalis concinnus and Thamnophis ordinoides) which are abundant in Oregon's Willamette Valley. The species sirtalis is the most wide ranging snake in the United States. It is commonly found near permanent water, though occasionally it is encountered in rather dry situations. In contrast to sirtalis, the monotypic species ordinoides is a strictly terrestrial northern Pacific Coast form, which typically is associated with areas of dense vegetation. T. s. concinnus is often seen basking on mild days of the coldest winter months (November-February) while T. ordinoides rarely emerges during these months. The distinct differences in habitat preference and winter behavior exhibited by these snakes suggest differences in thermal preferences and critical levels. To examine this possibility, and the responses of the snakes to thermal acclimation, comparative data on the following variables have been sought: 1) Body temperature of snakes in the field and its relationship to environmental temperatures; 2) body temperature of snakes in a thermal gradient box; 3) critical thermal maximum and minimum; 4) metabolic rate; 5) the effect of thermal acclimation on items two, three, and four. While more investigations are needed to confirm and clarify the results of this study, some tentative conclusions may be stated here: 1) T. s. concinnus and T. ordinoides are diurnal, heliothermic snakes which consistently maintain body temperatures higher than the air and substrate temperatures. 2) T. s. concinnus is more tolerant of seasonally extreme temperatures than T. ordinoides. 3) T. s, concinnus prefers slightly higher body temperatures than T. ordinoides. 4) If temperature tolerances and preferred temperatures are heritable characteristics developed in the phylogeny of the species, these differences probably are primarily related to the difference in distribution of each species as a whole, and secondarily to differences in habitat preference and habit which have resulted from competetive interactions with other species. 5) There are sexual differences in the preferred temperatures of both species, the most significant of which is the relatively high preferred temperature of pregnant females. 6) Initially, the preferred temperatures of both species are inversely related to acclimation temperature. Later, they may be directly related to acclimation temperature. 7) The critical thermal maxima and minima are similar in both species and are directly related to acclimation temperature. However, reacclimation affects the original response differently in the two species. 8) Both species exhibit typical metabolic rate responses to thermal acclimation. 9) Since metabolic rate responses are the same in both species, the greater cold tolerance of T. s. concinnus cannot be attributed to a greater ability to compensate for low temperature. Title: Thermal ecology of the garter snakes Thamnophis sirtalis concinnus (Hallowell) and Thamnophis ordinoides (Baird & Girard) Author: Stewart, Glenn R. In recent years, studies dealing with temperature regulation, temperature sensitivity, and physiological responses to temperature in lizards and other reptiles have increased tremendously. It is notable that snakes have been largely ignored in such studies. This no doubt is due to their less direct relationship to ancestral endotherms. However, problems in the ecology of snakes themselves may be elucidated by studies of this kind. The present study deals with two species of garter snakes ( Thamnophis sirtalis concinnus and Thamnophis ordinoides) which are abundant in Oregon's Willamette Valley. The species sirtalis is the most wide ranging snake in the United States. It is commonly found near permanent water, though occasionally it is encountered in rather dry situations. In contrast to sirtalis, the monotypic species ordinoides is a strictly terrestrial northern Pacific Coast form, which typically is associated with areas of dense vegetation. T. s. concinnus is often seen basking on mild days of the coldest winter months (November-February) while T. ordinoides rarely emerges during these months. The distinct differences in habitat preference and winter behavior exhibited by these snakes suggest differences in thermal preferences and critical levels. To examine this possibility, and the responses of the snakes to thermal acclimation, comparative data on the following variables have been sought: 1) Body temperature of snakes in the field and its relationship to environmental temperatures; 2) body temperature of snakes in a thermal gradient box; 3) critical thermal maximum and minimum; 4) metabolic rate; 5) the effect of thermal acclimation on items two, three, and four. While more investigations are needed to confirm and clarify the results of this study, some tentative conclusions may be stated here: 1) T. s. concinnus and T. ordinoides are diurnal, heliothermic snakes which consistently maintain body temperatures higher than the air and substrate temperatures. 2) T. s. concinnus is more tolerant of seasonally extreme temperatures than T. ordinoides. 3) T. s, concinnus prefers slightly higher body temperatures than T. ordinoides. 4) If temperature tolerances and preferred temperatures are heritable characteristics developed in the phylogeny of the species, these differences probably are primarily related to the difference in distribution of each species as a whole, and secondarily to differences in habitat preference and habit which have resulted from competetive interactions with other species. 5) There are sexual differences in the preferred temperatures of both species, the most significant of which is the relatively high preferred temperature of pregnant females. 6) Initially, the preferred temperatures of both species are inversely related to acclimation temperature. Later, they may be directly related to acclimation temperature. 7) The critical thermal maxima and minima are similar in both species and are directly related to acclimation temperature. However, reacclimation affects the original response differently in the two species. 8) Both species exhibit typical metabolic rate responses to thermal acclimation. 9) Since metabolic rate responses are the same in both species, the greater cold tolerance of T. s. concinnus cannot be attributed to a greater ability to compensate for low temperature. Close

• 76. [Article] Stream Temperature Management Strategies for the Central Umpqua Basin

  Abstract -- This report provides a technical framework to develop a temperature management plan with specific information and examples for the Central Umpqua Basin. Sections include basic stream heating ...

  Citation × Citation Citation Abstract Copy Title: Stream Temperature Management Strategies for the Central Umpqua Basin Abstract -- This report provides a technical framework to develop a temperature management plan with specific information and examples for the Central Umpqua Basin. Sections include basic stream heating concepts, general management considerations, temperature management, and extensive appendices. Title: Stream Temperature Management Strategies for the Central Umpqua Basin Abstract -- This report provides a technical framework to develop a temperature management plan with specific information and examples for the Central Umpqua Basin. Sections include basic stream heating concepts, general management considerations, temperature management, and extensive appendices. Close

• 77. [Article] Salmonberry River Temperature Monitoring-STEP Project

  Abstract -- Results of a STEP project in which volunteers monitor summer temperatures in the Salmonberry River and tributaries. The project began collecting temperatures in 1994. Project history, protocol, ...

  Citation × Citation Citation Abstract Copy Title: Salmonberry River Temperature Monitoring-STEP Project Abstract -- Results of a STEP project in which volunteers monitor summer temperatures in the Salmonberry River and tributaries. The project began collecting temperatures in 1994. Project history, protocol, and results are summarized in pdf documents. Title: Salmonberry River Temperature Monitoring-STEP Project Abstract -- Results of a STEP project in which volunteers monitor summer temperatures in the Salmonberry River and tributaries. The project began collecting temperatures in 1994. Project history, protocol, and results are summarized in pdf documents. Close

• 78. [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 Close

• 79. [Article] Snow and the ground temperature record of climate change

  Copyrighted by American Geophysical Union

  Citation × Citation Citation Abstract Copy Title: Snow and the ground temperature record of climate change Author: Bartlett, Marshall G., Chapman, David S., Harris, Robert N. Copyrighted by American Geophysical Union Title: Snow and the ground temperature record of climate change Author: Bartlett, Marshall G., Chapman, David S., Harris, Robert N. Copyrighted by American Geophysical Union Close

• 80. [Article] Relationships between Marine Stratus Cloud Optical Depth and Temperature: Inferences from AVHRR Observations

  Studies using International Satellite Cloud Climatology Project (ISCCP) data have reported decreases in cloud optical depth with increasing temperature, thereby suggesting a positive feedback in cloud ...

  Citation × Citation Citation Abstract Copy Title: Relationships between Marine Stratus Cloud Optical Depth and Temperature: Inferences from AVHRR Observations Author: Coakley, James A., Jr., Chang, Fu-Lung Studies using International Satellite Cloud Climatology Project (ISCCP) data have reported decreases in cloud optical depth with increasing temperature, thereby suggesting a positive feedback in cloud optical depth as climate warms. The negative cloud optical depth and temperature relationships are questioned because ISCCP employs threshold assumptions to identify cloudy pixels that have included partly cloudy pixels. This study applies the spatial coherence technique to one month of Advanced Very High Resolution Radiometer (AVHRR) data over the Pacific Ocean to differentiate overcast pixels from the partly cloudy pixels and to reexamine the cloud optical depth–temperature relationships. For low-level marine stratus clouds studied here, retrievals from partly cloudy pixels showed 30%–50% smaller optical depths, 1°–4°C higher cloud temperatures, and slightly larger droplet effective radii, when they were compared to retrievals from the overcast pixels. Despite these biases, retrievals for the overcast and partly cloudy pixels show similar negative cloud optical depth–temperature relationships and their magnitudes agree with the ISCCP results for the midlatitude and subtropical regions. There were slightly negative droplet effective radius–temperature relationships, and considerable positive cloud liquid water content–temperature relationships indicated by aircraft measurements. However, cloud thickness decreases appear to be the main reason why cloud optical depth decreases with increasing temperature. Overall, cloud thickness thinning may explain why similar negative cloud optical depth–temperature relationships are found in both overcast and partly cloudy pixels. In addition, comparing the cloud-top temperature to the air temperature at 740 hPa indicates that cloud-top height generally rises with warming. This suggests that the cloud thinning is mainly due to the ascending of cloud base. The results presented in this study are confined to the midlatitude and subtropical Pacific and may not be applicable to the Tropics or other regions Title: Relationships between Marine Stratus Cloud Optical Depth and Temperature: Inferences from AVHRR Observations Author: Coakley, James A., Jr., Chang, Fu-Lung Studies using International Satellite Cloud Climatology Project (ISCCP) data have reported decreases in cloud optical depth with increasing temperature, thereby suggesting a positive feedback in cloud optical depth as climate warms. The negative cloud optical depth and temperature relationships are questioned because ISCCP employs threshold assumptions to identify cloudy pixels that have included partly cloudy pixels. This study applies the spatial coherence technique to one month of Advanced Very High Resolution Radiometer (AVHRR) data over the Pacific Ocean to differentiate overcast pixels from the partly cloudy pixels and to reexamine the cloud optical depth–temperature relationships. For low-level marine stratus clouds studied here, retrievals from partly cloudy pixels showed 30%–50% smaller optical depths, 1°–4°C higher cloud temperatures, and slightly larger droplet effective radii, when they were compared to retrievals from the overcast pixels. Despite these biases, retrievals for the overcast and partly cloudy pixels show similar negative cloud optical depth–temperature relationships and their magnitudes agree with the ISCCP results for the midlatitude and subtropical regions. There were slightly negative droplet effective radius–temperature relationships, and considerable positive cloud liquid water content–temperature relationships indicated by aircraft measurements. However, cloud thickness decreases appear to be the main reason why cloud optical depth decreases with increasing temperature. Overall, cloud thickness thinning may explain why similar negative cloud optical depth–temperature relationships are found in both overcast and partly cloudy pixels. In addition, comparing the cloud-top temperature to the air temperature at 740 hPa indicates that cloud-top height generally rises with warming. This suggests that the cloud thinning is mainly due to the ascending of cloud base. The results presented in this study are confined to the midlatitude and subtropical Pacific and may not be applicable to the Tropics or other regions Close

• 81. [Article] Toward predicting community-level effects of climate: relative temperature scaling of metabolic and ingestion rates

  This is the publisher’s final pdf. The published article is copyrighted by the Ecological Society of America and can be found at: http://www.esajournals.org/loi/ecol. Supplemental Material can be found ...

  Citation × Citation Citation Abstract Copy Title: Toward predicting community-level effects of climate: relative temperature scaling of metabolic and ingestion rates Author: Iles, Alison C. This is the publisher’s final pdf. The published article is copyrighted by the Ecological Society of America and can be found at: http://www.esajournals.org/loi/ecol. Supplemental Material can be found at: http://www.esapubs.org/archive/ecol/E095/231/ Title: Toward predicting community-level effects of climate: relative temperature scaling of metabolic and ingestion rates Author: Iles, Alison C. This is the publisher’s final pdf. The published article is copyrighted by the Ecological Society of America and can be found at: http://www.esajournals.org/loi/ecol. Supplemental Material can be found at: http://www.esapubs.org/archive/ecol/E095/231/ Close

• 82. [Article] Effects of soil temperature on the root growth of Marshall strawberry plants

  Citation × Citation Citation Abstract Copy Title: Effects of soil temperature on the root growth of Marshall strawberry plants Author: Mellenthin, Walter M., 1920- Title: Effects of soil temperature on the root growth of Marshall strawberry plants Author: Mellenthin, Walter M., 1920- Close

• 83. [Article] Behavioral responses of Atlantic cod to sea temperature changes

  This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by John Wiley & Sons Ltd. The published article can be found at: http://onlinelibrary.wiley.com/jo...

  Citation × Citation Citation Abstract Copy Title: Behavioral responses of Atlantic cod to sea temperature changes Author: Freitas, Carla, Ciannelli, Lorenzo, Olsen, Esben Moland, Moland, Even, Knutsen, Halvor This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by John Wiley & Sons Ltd. The published article can be found at: http://onlinelibrary.wiley.com/journal/10.1002/%28ISSN%292045-7758 Title: Behavioral responses of Atlantic cod to sea temperature changes Author: Freitas, Carla, Ciannelli, Lorenzo, Olsen, Esben Moland, Moland, Even, Knutsen, Halvor This is the publisher’s final pdf. The published article is copyrighted by the author(s) and published by John Wiley & Sons Ltd. The published article can be found at: http://onlinelibrary.wiley.com/journal/10.1002/%28ISSN%292045-7758 Close

• 84. [Article] ArismendiIvanFisheriesWildlifeCanAirTemperature.pdf

  Citation × Citation Citation Abstract Copy Title: ArismendiIvanFisheriesWildlifeCanAirTemperature.pdf Author: Arismendi, Ivan, Johnson, Sherri L., Safeeq, Mohammad, Dunham, Jason B. Title: ArismendiIvanFisheriesWildlifeCanAirTemperature.pdf Author: Arismendi, Ivan, Johnson, Sherri L., Safeeq, Mohammad, Dunham, Jason B. Close

• 85. [Article] ArismendiIvanFisheriesWildlifeCanAirTemperature_SupplementaryData.pdf

  Citation × Citation Citation Abstract Copy Title: ArismendiIvanFisheriesWildlifeCanAirTemperature_SupplementaryData.pdf Author: Arismendi, Ivan, Johnson, Sherri L., Safeeq, Mohammad, Dunham, Jason B. Title: ArismendiIvanFisheriesWildlifeCanAirTemperature_SupplementaryData.pdf Author: Arismendi, Ivan, Johnson, Sherri L., Safeeq, Mohammad, Dunham, Jason B. Close

• 86. [Article] Oceanic vertical temperature measurements across the water-sediment interface at selected stations west of Oregon

  Citation × Citation Citation Abstract Copy Title: Oceanic vertical temperature measurements across the water-sediment interface at selected stations west of Oregon Author: Mesecar, Roderick S. Title: Oceanic vertical temperature measurements across the water-sediment interface at selected stations west of Oregon Author: Mesecar, Roderick S. Close

• 87. [Article] Growth rate and phosphorus uptake of wheat (Triticum aestivum VILL., Host) as a function of soil water suction and soil temperature

  The effect of soil temperature and soil water suction on the rate of phosphorus uptake and growth rate of wheat (Triticum aestivum VILL. , Host) was studied. Plants were grown in perlite slabs separated ...

  Citation × Citation Citation Abstract Copy Title: Growth rate and phosphorus uptake of wheat (Triticum aestivum VILL., Host) as a function of soil water suction and soil temperature Author: Fazilat, Mohammad The effect of soil temperature and soil water suction on the rate of phosphorus uptake and growth rate of wheat (Triticum aestivum VILL. , Host) was studied. Plants were grown in perlite slabs separated from an osmotic solution by a semi-permeable membrane. Measurements were made at temperatures of 10.0, 18.3, 23.9, 32.2, and 35.0°C, and soil water suctions of 0.35 and 2.5 bars. Five week old wheat seedlings were exposed to these conditions. The dry weight of shoots and roots was determined at two day intervals. Plant material extracted was analyzed for phosphorus concentration. The color intensity was measured on a Bausch and Lomb spectronic 20 spectrophotometer of 420 millimicrons. In general, a constant growth rate, which was approached exponentially during the experimental period was found in all treatment combinations. Growth rate for both shoots and roots was slow at low root temperatures and had a maximum rate at a root temperature of 24.0°C. High soil water suction was a limiting factor in growth rate. Phosphorus concentration of shoots and roots was found to approach a constant value during the experimental period according to the equation y = a+be[superscript]-0.07t[superscript]3/2 where y is the phosphorus concentration, t is the time in days, and a and b are constants. Over the entire range of soil temperatures considered the phosphorus concentration of the shoots increased linearlly with the root temperature, but the phosphorus concentration of the roots slightly decreased by increasing soil temperature and did not increase until the root temperature was about 32.0°C. There was no evidence of much variation in percent of total phosphorus uptake transported to the shoot in the experiments. Trans location of phosphorus from roots to shoots did not appear to be a limiting factor for phosphorus uptake at the low root temperature. It was suggested that the low rates of phosphorus uptake at the low root temperatures resulted from the low level of metabolic activity. Title: Growth rate and phosphorus uptake of wheat (Triticum aestivum VILL., Host) as a function of soil water suction and soil temperature Author: Fazilat, Mohammad The effect of soil temperature and soil water suction on the rate of phosphorus uptake and growth rate of wheat (Triticum aestivum VILL. , Host) was studied. Plants were grown in perlite slabs separated from an osmotic solution by a semi-permeable membrane. Measurements were made at temperatures of 10.0, 18.3, 23.9, 32.2, and 35.0°C, and soil water suctions of 0.35 and 2.5 bars. Five week old wheat seedlings were exposed to these conditions. The dry weight of shoots and roots was determined at two day intervals. Plant material extracted was analyzed for phosphorus concentration. The color intensity was measured on a Bausch and Lomb spectronic 20 spectrophotometer of 420 millimicrons. In general, a constant growth rate, which was approached exponentially during the experimental period was found in all treatment combinations. Growth rate for both shoots and roots was slow at low root temperatures and had a maximum rate at a root temperature of 24.0°C. High soil water suction was a limiting factor in growth rate. Phosphorus concentration of shoots and roots was found to approach a constant value during the experimental period according to the equation y = a+be[superscript]-0.07t[superscript]3/2 where y is the phosphorus concentration, t is the time in days, and a and b are constants. Over the entire range of soil temperatures considered the phosphorus concentration of the shoots increased linearlly with the root temperature, but the phosphorus concentration of the roots slightly decreased by increasing soil temperature and did not increase until the root temperature was about 32.0°C. There was no evidence of much variation in percent of total phosphorus uptake transported to the shoot in the experiments. Trans location of phosphorus from roots to shoots did not appear to be a limiting factor for phosphorus uptake at the low root temperature. It was suggested that the low rates of phosphorus uptake at the low root temperatures resulted from the low level of metabolic activity. Close

• 88. [Article] The microbial stability of refrigerated intermediate moisture foods

  The lag phase, the specific growth rate, the minimum a [subscript w] required for growth and the temperature characteristic of Fsendomonas fluorescens, Brochothrix thermosphacta, Salmonella typhlmurium, ...

  Citation × Citation Citation Abstract Copy Title: The microbial stability of refrigerated intermediate moisture foods Author: Li, Ken-yuon The lag phase, the specific growth rate, the minimum a [subscript w] required for growth and the temperature characteristic of Fsendomonas fluorescens, Brochothrix thermosphacta, Salmonella typhlmurium, Streptococcus faecalis and, Staphylococcus aureus have been studied in liquid model media under controlled temperature and a [subscript w] conditions. The results show that the lag phase increases and the specific growth rates decreases when the temperature is lowered or the a [subscript w] is reduced. The minimum a [subscript w] required for growth increases when the incubation temperature is lowered. At refrigeration temperature the minimum a [subscript w] for growth of mesophiles is higher than that of psychrotrophs. The temperature characteristic (representing the activation energy for growth) of psychrotrophs is lower than that of mesophiles, and therefore mesophiles are more sensitive to temperature changes. All of these growth parameters depend on the a [subscript w] controlling solute. The solute effect can be traced to the ability of the solute to penetrate into the cell and can be explained by the osmoregulatory mechanism. In general, it was found that the effect of the solute on these parameters had the order glycerol<NaCl<sucrose. A comparison of three models for the effect of temperature on growth rate (linear, square-root, and Arrhenius) showed that the linear model had both the advantage of simplicity and accuracy. In general, the Arrhenius model showed the poorest fit to experimental data. A predictive method was developed to assess the microbial stability of liquid model systems exposed to fluctuating temperatures. The strategy was to predict lag time and growth rate by different regression equations, and to estimate microbial growth using an integral function of the accumulated time. A lag time predictive model was developed using a linear relationship between lag time and reciprocal growth rate. A linear equation was used to predict growth rate as a function of temperature. The model was used to predict the growth of B. thermosphacta in liquid model media with low a [subscript w] and exposed to fluctuating temperatures. The predictions were acceptable at a 95% confidence level. This method will be used in future studies to predict the microbial stability of refrigerated foods exposed to temperature abuse. Title: The microbial stability of refrigerated intermediate moisture foods Author: Li, Ken-yuon The lag phase, the specific growth rate, the minimum a [subscript w] required for growth and the temperature characteristic of Fsendomonas fluorescens, Brochothrix thermosphacta, Salmonella typhlmurium, Streptococcus faecalis and, Staphylococcus aureus have been studied in liquid model media under controlled temperature and a [subscript w] conditions. The results show that the lag phase increases and the specific growth rates decreases when the temperature is lowered or the a [subscript w] is reduced. The minimum a [subscript w] required for growth increases when the incubation temperature is lowered. At refrigeration temperature the minimum a [subscript w] for growth of mesophiles is higher than that of psychrotrophs. The temperature characteristic (representing the activation energy for growth) of psychrotrophs is lower than that of mesophiles, and therefore mesophiles are more sensitive to temperature changes. All of these growth parameters depend on the a [subscript w] controlling solute. The solute effect can be traced to the ability of the solute to penetrate into the cell and can be explained by the osmoregulatory mechanism. In general, it was found that the effect of the solute on these parameters had the order glycerol<NaCl<sucrose. A comparison of three models for the effect of temperature on growth rate (linear, square-root, and Arrhenius) showed that the linear model had both the advantage of simplicity and accuracy. In general, the Arrhenius model showed the poorest fit to experimental data. A predictive method was developed to assess the microbial stability of liquid model systems exposed to fluctuating temperatures. The strategy was to predict lag time and growth rate by different regression equations, and to estimate microbial growth using an integral function of the accumulated time. A lag time predictive model was developed using a linear relationship between lag time and reciprocal growth rate. A linear equation was used to predict growth rate as a function of temperature. The model was used to predict the growth of B. thermosphacta in liquid model media with low a [subscript w] and exposed to fluctuating temperatures. The predictions were acceptable at a 95% confidence level. This method will be used in future studies to predict the microbial stability of refrigerated foods exposed to temperature abuse. Close

• 89. [Article] Optimal Storage Temperature Design for Frozen Seafood Inventories: Application to Pacific Whiting Surimi

  Research Paper

  Citation × Citation Citation Abstract Copy Title: Optimal Storage Temperature Design for Frozen Seafood Inventories: Application to Pacific Whiting Surimi Author: Sylvia, Gilbert, Burden, Merrick, Kolbe, Edward Research Paper Title: Optimal Storage Temperature Design for Frozen Seafood Inventories: Application to Pacific Whiting Surimi Author: Sylvia, Gilbert, Burden, Merrick, Kolbe, Edward Research Paper Close

• 90. [Article] Stream temperatures : some basic considerations

  Declared out of print December 2009. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonst...

  Citation × Citation Citation Abstract Copy Title: Stream temperatures : some basic considerations Author: Moore, James A. (James Allan), 1939-, Oregon State University. Extension Service, Miner, J. Ronald Declared out of print December 2009. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonstate.edu/catalog Title: Stream temperatures : some basic considerations Author: Moore, James A. (James Allan), 1939-, Oregon State University. Extension Service, Miner, J. Ronald Declared out of print December 2009. Facts and recommendations in this publication may no longer be valid. Please look for up-to-date information in the OSU Extension Catalog: http://extension.oregonstate.edu/catalog Close

• 91. [Article] Stream Temperature Management in the Tualatin Watershed: Is it Improving Salmonid Habitat?

  The purpose of this paper is to examine the literature from scientific and governmental entities that describes the problems with elevated stream temperatures in the Tualatin basin, the actions being taken ...

  Citation × Citation Citation Abstract Copy Title: Stream Temperature Management in the Tualatin Watershed: Is it Improving Salmonid Habitat? Author: Hennings, Raymond Banks Year: 2014 The purpose of this paper is to examine the literature from scientific and governmental entities that describes the problems with elevated stream temperatures in the Tualatin basin, the actions being taken to resolve those problems, and to assess whether these actions are meeting the goal of improving salmonid habitat in the basin. Elevated stream temperatures are considered a pollutant under the US Clean Water Act (Clean Water Act 1972, as amended) because increased stream temperatures can be harmful to native aquatic biota, particularly salmonid fish species that have evolved to use cold water (IMST 2004). Title: Stream Temperature Management in the Tualatin Watershed: Is it Improving Salmonid Habitat? Author: Hennings, Raymond Banks Year: 2014 The purpose of this paper is to examine the literature from scientific and governmental entities that describes the problems with elevated stream temperatures in the Tualatin basin, the actions being taken to resolve those problems, and to assess whether these actions are meeting the goal of improving salmonid habitat in the basin. Elevated stream temperatures are considered a pollutant under the US Clean Water Act (Clean Water Act 1972, as amended) because increased stream temperatures can be harmful to native aquatic biota, particularly salmonid fish species that have evolved to use cold water (IMST 2004). Close

• 92. [Article] Stagnation point heat transfer in a relaxing gas

  Stagnation point heat transfer in a gas undergoing relaxation of its internal energy is examined by solution of the equations of motion using the two temperature approach of Wang Chang and Uhlenbeck. The ...

  Citation × Citation Citation Abstract Copy Title: Stagnation point heat transfer in a relaxing gas Author: Wilson, Robert E. (Robert Elliott) Stagnation point heat transfer in a gas undergoing relaxation of its internal energy is examined by solution of the equations of motion using the two temperature approach of Wang Chang and Uhlenbeck. The results are presented in parametric form and show that relaxation effects produce an adiabatic wall temperature above the free stream stagnation temperature, which is related to the thermal conductivity of the ''inert" mode, the dimensionless relaxation length, the ratio of the translational mode temperature to the temperature of the relaxing mode at the edge of the boundary layer, and the magnitude of the internal energy undergoing relaxation. An experiment is described whereby the thermal conductivity of the "inert" mode, which is unknown, may be determined from adiabatic wall temperature measurements. Title: Stagnation point heat transfer in a relaxing gas Author: Wilson, Robert E. (Robert Elliott) Stagnation point heat transfer in a gas undergoing relaxation of its internal energy is examined by solution of the equations of motion using the two temperature approach of Wang Chang and Uhlenbeck. The results are presented in parametric form and show that relaxation effects produce an adiabatic wall temperature above the free stream stagnation temperature, which is related to the thermal conductivity of the ''inert" mode, the dimensionless relaxation length, the ratio of the translational mode temperature to the temperature of the relaxing mode at the edge of the boundary layer, and the magnitude of the internal energy undergoing relaxation. An experiment is described whereby the thermal conductivity of the "inert" mode, which is unknown, may be determined from adiabatic wall temperature measurements. Close

• 93. [Article] Fully developed laminar natural convection in a vertical parallel plate channel with symmetric uniform wall temperature

  Described in this thesis is an investigation of the fully developed natural convection heat transfer in a vertical channel formed by two infinitely wide parallel plates maintained at a uniform wall temperature. ...

  Citation × Citation Citation Abstract Copy Title: Fully developed laminar natural convection in a vertical parallel plate channel with symmetric uniform wall temperature Author: Willie, Robert H. Described in this thesis is an investigation of the fully developed natural convection heat transfer in a vertical channel formed by two infinitely wide parallel plates maintained at a uniform wall temperature. Closed-form solutions for the velocity and temperature profiles are developed along with local and averaged Nusselt numbers. The local Nusselt number based on bulk temperature is found to be 3.77. This result is an analog corresponding to 7.60 for fully developed laminar forced convection in a parallel plate channel with uniform wall temperature boundary condition. The local Nusselt number based on the ambient temperature is deduced as a function of flowwise location. Results are compared with existing numerical and experimental data to find good agreement. Title: Fully developed laminar natural convection in a vertical parallel plate channel with symmetric uniform wall temperature Author: Willie, Robert H. Described in this thesis is an investigation of the fully developed natural convection heat transfer in a vertical channel formed by two infinitely wide parallel plates maintained at a uniform wall temperature. Closed-form solutions for the velocity and temperature profiles are developed along with local and averaged Nusselt numbers. The local Nusselt number based on bulk temperature is found to be 3.77. This result is an analog corresponding to 7.60 for fully developed laminar forced convection in a parallel plate channel with uniform wall temperature boundary condition. The local Nusselt number based on the ambient temperature is deduced as a function of flowwise location. Results are compared with existing numerical and experimental data to find good agreement. Close

• 94. [Article] Durability of room-temperature-setting and intermediate-temperature-setting resin glues cured to different degrees in Yellow Birch plywood

  This report is one of a series issued in cooperation with the Army-Navy-Civil Committee on aircraft design criteria under the supervision of the Aeronautical Board.

  Citation × Citation Citation Abstract Copy Title: Durability of room-temperature-setting and intermediate-temperature-setting resin glues cured to different degrees in Yellow Birch plywood Author: Forest Products Laboratory (U.S.), Olson, W. Z., Black, John M. This report is one of a series issued in cooperation with the Army-Navy-Civil Committee on aircraft design criteria under the supervision of the Aeronautical Board. Title: Durability of room-temperature-setting and intermediate-temperature-setting resin glues cured to different degrees in Yellow Birch plywood Author: Forest Products Laboratory (U.S.), Olson, W. Z., Black, John M. This report is one of a series issued in cooperation with the Army-Navy-Civil Committee on aircraft design criteria under the supervision of the Aeronautical Board. Close

• 95. [Article] Spatial, diel and seasonal variations in dissolved oxygen and temperature within a stratified lake

  Spatial, diel and seasonal variations in dissolved oxygen and temperature were measured in Triangle Lake, Oregon. Spatial dissolved oxygen and temperature variations measured in the stratified lake are ...

  Citation × Citation Citation Abstract Copy Title: Spatial, diel and seasonal variations in dissolved oxygen and temperature within a stratified lake Author: Smith, Stanley Allan Spatial, diel and seasonal variations in dissolved oxygen and temperature were measured in Triangle Lake, Oregon. Spatial dissolved oxygen and temperature variations measured in the stratified lake are presented to illustrate the horizontal uniformity of the lake and to demonstrate the applicability of the one dimensional assumption for sampling and theoretical modeling of temperature and dissolved oxygen. A nocturnal density overturning within the epilimnion was investigated and its significance as a mode of vertical mixing evaluated. Seasonal variations in temperature and dissolved oxygen indicated that a complete winter overturn did not occur. The effect of seasonal variations in temperature and dissolved oxygen upon the habitat of game fish within the lake is presented. Title: Spatial, diel and seasonal variations in dissolved oxygen and temperature within a stratified lake Author: Smith, Stanley Allan Spatial, diel and seasonal variations in dissolved oxygen and temperature were measured in Triangle Lake, Oregon. Spatial dissolved oxygen and temperature variations measured in the stratified lake are presented to illustrate the horizontal uniformity of the lake and to demonstrate the applicability of the one dimensional assumption for sampling and theoretical modeling of temperature and dissolved oxygen. A nocturnal density overturning within the epilimnion was investigated and its significance as a mode of vertical mixing evaluated. Seasonal variations in temperature and dissolved oxygen indicated that a complete winter overturn did not occur. The effect of seasonal variations in temperature and dissolved oxygen upon the habitat of game fish within the lake is presented. Close

• 96. [Article] High-temperature, high-pressure NMR probe for superconducting magnets

  A high-temperature, high-pressure autoclave has been adapted for use with a high-field nuclear magnetic resonance spectrometer. The autoclave has an internal pressure range of atmospheric pressure to 1.5 ...

  Citation × Citation Citation Abstract Copy Title: High-temperature, high-pressure NMR probe for superconducting magnets Author: Mullen, Corina P. A high-temperature, high-pressure autoclave has been adapted for use with a high-field nuclear magnetic resonance spectrometer. The autoclave has an internal pressure range of atmospheric pressure to 1.5 kbar and a temperature range of 273 K to 1900 K. The autoclave is usable in a high field (8 T) magnet with a room temperature, 76.4 mm bore. The autoclave was tested using assorted nuclear species with resonant frequencies ranging from 57 to 70 MHz at pressures ranging from atmospheric pressure to 1220 bar and temperatures ranging from 273 K to 448 K. Previously, the autoclave was used in conjunction with an iron magnet at temperatures to 1900 K and pressures to 1.5 kbar. Title: High-temperature, high-pressure NMR probe for superconducting magnets Author: Mullen, Corina P. A high-temperature, high-pressure autoclave has been adapted for use with a high-field nuclear magnetic resonance spectrometer. The autoclave has an internal pressure range of atmospheric pressure to 1.5 kbar and a temperature range of 273 K to 1900 K. The autoclave is usable in a high field (8 T) magnet with a room temperature, 76.4 mm bore. The autoclave was tested using assorted nuclear species with resonant frequencies ranging from 57 to 70 MHz at pressures ranging from atmospheric pressure to 1220 bar and temperatures ranging from 273 K to 448 K. Previously, the autoclave was used in conjunction with an iron magnet at temperatures to 1900 K and pressures to 1.5 kbar. Close

• 97. [Article] Impact of Isothermal Aging and Testing Temperature on Large Flip-Chip BGA Interconnect Mechanical Shock Performance

  The stability of solder interconnects in a mechanical shock environment is crucial for large body size flip-chip ball grid array (FCBGA) electronic packages. Additionally, the junction temperature increases ...

  Citation × Citation Citation Abstract Copy Title: Impact of Isothermal Aging and Testing Temperature on Large Flip-Chip BGA Interconnect Mechanical Shock Performance Author: Lee, Tae-Kyu, Chen, Zhiqiang, Guirguis, Cherif, Akinade, Kola Year: 2017 The stability of solder interconnects in a mechanical shock environment is crucial for large body size flip-chip ball grid array (FCBGA) electronic packages. Additionally, the junction temperature increases with higher electric power condition, which brings the component into an elevated temperature environment, thus introducing another consideration factor for mechanical stability of interconnection joints. Since most of the shock performance data available were produced at room temperature, the effect of elevated temperature is of interest to ensure the reliability of the device in a mechanical shock environment. To achieve a stablea interconnect pound in a dynamic shock environment, the interconnections must tolerate mechanical strain, which is induced by the shock wave input and reaches the particular component interconnect joint. In this study, large body size (52.5 x 52.5 mm(2)) FCBGA components assembled on 2.4-mm-thick boards were tested with various isothermal pre-conditions and testing conditions. With a heating element embedded in the test board, a test temperature range from room temperature to 100A degrees C was established. The effects of elevated temperature on mechanical shock performance were investigated. Failure and degradation mechanisms are identified and discussed based on the microstructure evolution and grain structure transformations. Title: Impact of Isothermal Aging and Testing Temperature on Large Flip-Chip BGA Interconnect Mechanical Shock Performance Author: Lee, Tae-Kyu, Chen, Zhiqiang, Guirguis, Cherif, Akinade, Kola Year: 2017 The stability of solder interconnects in a mechanical shock environment is crucial for large body size flip-chip ball grid array (FCBGA) electronic packages. Additionally, the junction temperature increases with higher electric power condition, which brings the component into an elevated temperature environment, thus introducing another consideration factor for mechanical stability of interconnection joints. Since most of the shock performance data available were produced at room temperature, the effect of elevated temperature is of interest to ensure the reliability of the device in a mechanical shock environment. To achieve a stablea interconnect pound in a dynamic shock environment, the interconnections must tolerate mechanical strain, which is induced by the shock wave input and reaches the particular component interconnect joint. In this study, large body size (52.5 x 52.5 mm(2)) FCBGA components assembled on 2.4-mm-thick boards were tested with various isothermal pre-conditions and testing conditions. With a heating element embedded in the test board, a test temperature range from room temperature to 100A degrees C was established. The effects of elevated temperature on mechanical shock performance were investigated. Failure and degradation mechanisms are identified and discussed based on the microstructure evolution and grain structure transformations. Close

• 98. [Article] Climate change on the Colorado Plateau of eastern Utah inferred from borehole temperatures

  copyrighted by American Geophysical Union

  Citation × Citation Citation Abstract Copy Title: Climate change on the Colorado Plateau of eastern Utah inferred from borehole temperatures Author: Chapman, David S., Harris, Robert N. copyrighted by American Geophysical Union Title: Climate change on the Colorado Plateau of eastern Utah inferred from borehole temperatures Author: Chapman, David S., Harris, Robert N. copyrighted by American Geophysical Union Close

• 99. [Article] Air Temperature Measurement Errors in Naturally Ventilated Radiation Shields

  Two sources of systematic errors are considered for estimating air temperature. The first source is ambiguity of the definition of the standardized measurement height over vegetated surfaces of varying ...

  Citation × Citation Citation Abstract Copy Title: Air Temperature Measurement Errors in Naturally Ventilated Radiation Shields Author: Nakamura, Reina, Mahrt, L. Two sources of systematic errors are considered for estimating air temperature. The first source is ambiguity of the definition of the standardized measurement height over vegetated surfaces of varying heights. Without such a standardization, evaluation of the horizontal air temperature gradient is contaminated by the vertical variation of air temperature. This error is generally small in daytime unstable conditions, but increases with increasing stability at night. In an attempt to reduce such error, the use of the zero-plane displacement height for standardizing the measurement height is proposed. The second source of systematic errors is radiative forcing on the sensor–shield systems. A series of experiments is performed over a grass field to investigate the radiatively induced error in the air temperature estimate by the Onset HOBO Pro thermistor in a naturally ventilated multiplate shield. The magnitude of this error is estimated by comparing air temperature measurements by a platinum resistance temperature detector (RTD) sensor in a mechanically aspirated shield. In contrast to the errors resulting from the first source, the radiatively induced error increases with increasing instability. An empirical model is developed for correcting the radiatively induced temperature error using information on wind speed and net or shortwave radiation. The robustness of the model is examined with independent data. Title: Air Temperature Measurement Errors in Naturally Ventilated Radiation Shields Author: Nakamura, Reina, Mahrt, L. Two sources of systematic errors are considered for estimating air temperature. The first source is ambiguity of the definition of the standardized measurement height over vegetated surfaces of varying heights. Without such a standardization, evaluation of the horizontal air temperature gradient is contaminated by the vertical variation of air temperature. This error is generally small in daytime unstable conditions, but increases with increasing stability at night. In an attempt to reduce such error, the use of the zero-plane displacement height for standardizing the measurement height is proposed. The second source of systematic errors is radiative forcing on the sensor–shield systems. A series of experiments is performed over a grass field to investigate the radiatively induced error in the air temperature estimate by the Onset HOBO Pro thermistor in a naturally ventilated multiplate shield. The magnitude of this error is estimated by comparing air temperature measurements by a platinum resistance temperature detector (RTD) sensor in a mechanically aspirated shield. In contrast to the errors resulting from the first source, the radiatively induced error increases with increasing instability. An empirical model is developed for correcting the radiatively induced temperature error using information on wind speed and net or shortwave radiation. The robustness of the model is examined with independent data. Close

• 100. [Article] Effect of Solute and Temperature on Osmotic Tolerance _Final.ppt

  Citation × Citation Citation Abstract Copy Title: Effect of Solute and Temperature on Osmotic Tolerance _Final.ppt Author: Huang, Kenneth Title: Effect of Solute and Temperature on Osmotic Tolerance _Final.ppt Author: Huang, Kenneth Close