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1

Johnson, Sherri L. "Factors influencing stream temperatures in small streams: substrate effects and a shading experiment." Canadian Journal of Fisheries and Aquatic Sciences 61, no. 6 (2004): 913–23. http://dx.doi.org/10.1139/f04-040.

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The temperature of stream water is an important control of many in-stream processes. To better understand the processes and consequences of solar energy inputs to streams, stream temperature dynamics were examined before, during, and after experimental shading of a 150-m reach of a second-order stream in the Oregon Cascade Range. Maximum water temperatures declined significantly in the shaded reach, but minimum and mean temperatures were not modified. Heat budget calculations before shading show the dominance of solar energy as an influence of stream temperature. The influence of substrate typ
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2

Kristensen, P. B., E. A. Kristensen, T. Riis, et al. "Riparian forest as a management tool for moderating future thermal conditions of lowland temperate streams." Hydrology and Earth System Sciences Discussions 10, no. 5 (2013): 6081–106. http://dx.doi.org/10.5194/hessd-10-6081-2013.

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Abstract. Predictions of the future climate infer that stream water temperatures may increase in temperate lowland areas and that streams without riparian forest will be particularly prone to elevated stream water temperature. Planting of riparian forest is a potential mitigation measure to reduce water temperatures for the benefit of stream organisms. However, no studies have yet determined the length of a forested reach required to obtain a significant temperature decrease. To investigate this we measured the temperature in five small Danish lowland streams from June 2010 to July 2011, all s
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Murphy, Robert D., John A. Hagan, Bradley P. Harris, Suresh A. Sethi, T. Scott Smeltz, and Felipe Restrepo. "Can Landsat Thermal Imagery and Environmental Data Accurately Estimate Water Temperatures in Small Streams?" Journal of Fish and Wildlife Management 12, no. 1 (2021): 12–26. http://dx.doi.org/10.3996/jfwm-20-048.

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Abstract The ability to monitor water temperature is important for assessing changes in riverine ecosystems resulting from climate warming. Direct in situ water temperature collection efforts provide point samples but are cost-prohibitive for characterizing stream temperatures across large spatial scales, especially for small, remote streams. In contrast, satellite thermal infrared imagery may provide a spatially extensive means of monitoring riverine water temperatures; however, researchers do not have a good understanding of the accuracy of these remotely sensed temperatures for small stream
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4

Bourque, C. P. A., and J. H. Pomeroy. "Effects of forest harvesting on summer stream temperatures in New Brunswick, Canada: an inter-catchment, multiple-year comparison." Hydrology and Earth System Sciences 5, no. 4 (2001): 599–614. http://dx.doi.org/10.5194/hess-5-599-2001.

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Abstract. This paper presents a pre- and post-harvest comparison of stream temperatures collected in five neighbouring streams (sub-catchments) over a period of five years (1994-1998). The aim of the study was to determine whether land cover changes from clear cutting in areas outside forest buffer zones (applied to streams >0.5 m wide) might contribute to an increase in summer mean stream temperatures in buffered streams downslope by infusion of warmed surface and sub-surface water into the streams. Specific relationships were observed in all five forest streams investigated. To assist in
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5

Joughin, Ian R., Slawek Tulaczyk, and Hermann F. Engelhardt. "Basal melt beneath Whillans Ice Stream and Ice Streams A and C, West Antarctica." Annals of Glaciology 36 (2003): 257–62. http://dx.doi.org/10.3189/172756403781816130.

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AbstractWe have used a recently derived map of the velocity of Whillans Ice Stream and Ice Streams A and C, West Antarctica, to help estimate basal melt. Ice temperature was modeled with a simple vertical advection–diffusion equation,“tuned” to match temperature profiles. We find that most of the melt occurs beneath the tributaries, where larger basal shear stresses and thicker ice favor greater melt (e.g. 10–20mm a−1). The occurrence of basal freezing is predicted beneath much of the ice plains of Ice Stream C andWhillans Ice Stream. Modeled melt rates for when Ice Stream C was active suggest
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6

Munir, Tariq, and Cherie Westbrook. "Thermal Characteristics of a Beaver Dam Analogues Equipped Spring-Fed Creek in the Canadian Rockies." Water 13, no. 7 (2021): 990. http://dx.doi.org/10.3390/w13070990.

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Beaver dam analogues (BDAs) are becoming an increasingly popular stream restoration technique. One ecological function BDAs might help restore is suitable habitat conditions for fish in streams where loss of beaver dams and channel incision has led to their decline. A critical physical characteristic for fish is stream temperature. We examined the thermal regime of a spring-fed Canadian Rocky Mountain stream in relation to different numbers of BDAs installed in series over three study periods (April–October; 2017–2019). While all BDA configurations significantly influenced stream and pond temp
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7

Stott, T., and S. Marks. "Effects of plantation forest clearfelling on stream temperatures in the Plynlimon experimental catchments, mid-Wales." Hydrology and Earth System Sciences 4, no. 1 (2000): 95–104. http://dx.doi.org/10.5194/hess-4-95-2000.

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Abstract. Hourly stream temperatures monitored over 28 months, which spanned a 3 month period of environmentally sensitive plot-scale harvesting of 20 ha. (20%) of the Nant Tanllwyth catchment (0.89 km2) on the south side of the main stream in early 1996, resulted in a 0.58°C (p< 0.001) increase in monthly mean stream temperature. Over the same 28 month experimental period, there was no significant increase in the monthly mean air temperature recorded at a nearby automatic weather station. Monthly mean temperatures are highest in July and August in the year before and the year after the cle
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8

Leach, J. A., and R. D. Moore. "Winter stream temperature in the rain-on-snow zone of the Pacific Northwest: influences of hillslope runoff and transient snow cover." Hydrology and Earth System Sciences 18, no. 2 (2014): 819–38. http://dx.doi.org/10.5194/hess-18-819-2014.

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Abstract. Stream temperature dynamics during winter are less well studied than summer thermal regimes, but the winter season thermal regime can be critical for fish growth and development in coastal catchments. The winter thermal regimes of Pacific Northwest headwater streams, which provide vital winter habitat for salmonids and their food sources, may be particularly sensitive to changes in climate because they can remain ice-free throughout the year and are often located in rain-on-snow zones. This study examined winter stream temperature patterns and controls in small headwater catchments w
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9

Leach, J. A., and R. D. Moore. "Winter stream temperature in the rain-on-snow zone of the Pacific northwest: influences of hillslope runoff and transient snow cover." Hydrology and Earth System Sciences Discussions 10, no. 10 (2013): 12951–3003. http://dx.doi.org/10.5194/hessd-10-12951-2013.

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Abstract. Stream temperature dynamics during winter are less well studied than summer thermal regimes, but the winter season thermal regime can be critical for fish growth and development in coastal catchments. The winter thermal regimes of Pacific Northwest headwater streams, which provide vital winter habitat for salmonids and their food sources, may be particularly sensitive to changes in climate because they can remain ice-free throughout the year and are often located in rain-on-snow zones. This study examined winter stream temperature patterns and controls in small headwater catchments w
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10

Mellina, Eric, R. Dan Moore, Scott G. Hinch, J. Stevenson Macdonald, and Greg Pearson. "Stream temperature responses to clearcut logging in British Columbia: the moderating influences of groundwater and headwater lakes." Canadian Journal of Fisheries and Aquatic Sciences 59, no. 12 (2002): 1886–900. http://dx.doi.org/10.1139/f02-158.

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Although the future timber supply in the northern hemisphere is expected to come from boreal and subboreal forests, little research has been conducted in these regions that examines the temperature responses of small, lake-headed streams to streamside timber harvesting. We examined the temperature patterns of two subboreal outlet streams in north-central British Columbia for 1 year before and 3 years after clearcut logging and found only modest changes (averaging 0.05–1.1°C) with respect to summer daily maximum and minimum temperatures, diurnal fluctuations, and stream cooling. A multistream c
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11

Siegel, Jared E., Aimee H. Fullerton, Alyssa M. FitzGerald, Damon Holzer, and Chris E. Jordan. "Daily stream temperature predictions for free-flowing streams in the Pacific Northwest, USA." PLOS Water 2, no. 8 (2023): e0000119. http://dx.doi.org/10.1371/journal.pwat.0000119.

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Supporting sustainable lotic ecosystems and thermal habitats requires estimates of stream temperature that are high in scope and resolution across space and time. We combined and enhanced elements of existing stream temperature models to produce a new statistical model to address this need. Contrasting with previous models that estimated coarser metrics such as monthly or seasonal stream temperature or focused on individual watersheds, we modeled daily stream temperature across the entire calendar year for a broad geographic region. This model reflects mechanistic processes using publicly avai
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12

MacDonald, Ryan J., Sarah Boon, James M. Byrne, Mike D. Robinson, and Joseph B. Rasmussen. "Potential future climate effects on mountain hydrology, stream temperature, and native salmonid life history." Canadian Journal of Fisheries and Aquatic Sciences 71, no. 2 (2014): 189–202. http://dx.doi.org/10.1139/cjfas-2013-0221.

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Native salmonids of western North America are subject to many environmental pressures, most notably the effects of introduced species and environmental degradation. To better understand how native salmonids on the eastern slopes of the Canadian Rocky Mountains may respond to future changes in climate, we applied a process-based approach to hydrologic and stream temperature modelling. This study demonstrates that stream thermal regimes in western Alberta, Canada, may only warm during the summer period, while colder thermal regimes during spring, fall, and winter could result from response to ea
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13

Fogel, Caleb B., Colin L. Nicol, Jeffrey C. Jorgensen, et al. "How riparian and floodplain restoration modify the effects of increasing temperature on adult salmon spawner abundance in the Chehalis River, WA." PLOS ONE 17, no. 6 (2022): e0268813. http://dx.doi.org/10.1371/journal.pone.0268813.

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Stream temperatures in the Pacific Northwest are projected to increase with climate change, placing additional stress on cold-water salmonids. We modeled the potential impact of increased stream temperatures on four anadromous salmonid populations in the Chehalis River Basin (spring-run and fall-run Chinook salmon Oncorhynchus tshawytscha, coho salmon O. kisutch, and steelhead O. mykiss), as well as the potential for floodplain reconnection and stream shade restoration to offset the effects of future temperature increases. In the Chehalis River Basin, peak summer stream temperatures are predic
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14

Hoess, Rebecca, Konstantina A. Generali, Johannes Kuhn, and Juergen Geist. "Impact of Fish Ponds on Stream Hydrology and Temperature Regime in the Context of Freshwater Pearl Mussel Conservation." Water 14, no. 16 (2022): 2490. http://dx.doi.org/10.3390/w14162490.

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Conservation of endangered, cold-stenothermic species, such as the freshwater pearl mussel (FPM) and its salmonid host fish, are particularly challenging in headwater streams as their last refuge areas. Understanding the impact of anthropogenic catchment features such as fish ponds on the hydrology and the temperature regime of such streams is, therefore, important. In this study, runoff in a FPM catchment with more than 150 small ponds was simulated using SWAT and compared to a scenario without ponds. Additionally, water temperature was monitored hourly along three steams over 2.5 years, at s
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15

Ice, George G., Jeff Light, and Maryanne Reiter. "Use of Natural Temperature Patterns to Identify Achievable Stream Temperature Criteria for Forest Streams." Western Journal of Applied Forestry 19, no. 4 (2004): 252–59. http://dx.doi.org/10.1093/wjaf/19.4.252.

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Abstract Almost 90% of the streams listed on the EPA's nationwide database as water-quality impaired for temperature are in the Northwest. Historic records, monitoring of streams in federal wilderness areas in Oregon, and available data for least-impaired streams in Oregon, Washington, and Idaho show that many of these streams cannot achieve state temperature criteria. Forest management often is cited as a cause for increased stream temperature above state standards. The expectation that all forested streams should be below state targets has led to unnecessary listing of streams as impaired, w
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16

Cole, Elizabeth, and Michael Newton. "Influence of streamside buffers on stream temperature response following clear-cut harvesting in western Oregon." Canadian Journal of Forest Research 43, no. 11 (2013): 993–1005. http://dx.doi.org/10.1139/cjfr-2013-0138.

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Determining the effectiveness of different riparian buffers for mitigating forest-harvesting impacts on stream temperatures continues to be of interest throughout the world. Four small, low or medium elevation streams in managed western Oregon forests were studied to determine how the arrangement and amount of streamside retention strips (buffers) in clear-cut units influenced stream temperatures. Buffers included (i) no tree, (ii) predominantly sun-sided 12 m wide partial, and (iii) two-sided (Best Management Practice, (BMP)) 15–30 m wide buffers. Harvested units alternated with uncut units a
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17

Kurylyk, B. L., K. T. B. MacQuarrie, D. Caissie, and J. M. McKenzie. "Shallow groundwater thermal sensitivity to climate change and land cover disturbances: derivation of analytical expressions and implications for stream temperature modeling." Hydrology and Earth System Sciences 19, no. 5 (2015): 2469–89. http://dx.doi.org/10.5194/hess-19-2469-2015.

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Abstract. Climate change is expected to increase stream temperatures and the projected warming may alter the spatial extent of habitat for cold-water fish and other aquatic taxa. Recent studies have proposed that stream thermal sensitivities, derived from short-term air temperature variations, can be employed to infer future stream warming due to long-term climate change. However, this approach does not consider the potential for streambed heat fluxes to increase due to gradual warming of the shallow subsurface. The temperature of shallow groundwater is particularly important for the thermal r
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18

Tronstad, Lusha, J. Joseph Giersch, Scott Hotaling, et al. "Establishing a long-term monitoring network for assessing potential climatic refugia in cold alpine streams." UW National Parks Service Research Station Annual Reports 40 (December 15, 2017): 69–78. http://dx.doi.org/10.13001/uwnpsrc.2017.5581.

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Managing landscapes to maintain climate refugia is likely the best strategy to promote persistence of temperature-sensitive species with limited dispersal capacity. Rare, cold-stenothermic taxa occupy mosaic mountain stream networks due largely to hydrological source heterogeneity. We collected environmental and biological data from alpine streams in the Teton Range, Wyoming representing runoff from snowpack (N=3), glaciers (N=4) and subterranean ice (N=4), every summer from 2015-2017. We quantified differences in habitat among the streams according to a glaciality index that included bed stab
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19

Caissie, Daniel, Nassir El-Jabi, and André St-Hilaire. "Stochastic modelling of water temperatures in a small stream using air to water relations." Canadian Journal of Civil Engineering 25, no. 2 (1998): 250–60. http://dx.doi.org/10.1139/l97-091.

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Stream water temperature is a very important parameter when assessing aquatic ecosystem dynamics. For instance, cold-water fishes such as salmon can be adversely affected by maximum summer temperatures or by those exaggerated by land-use activities such as deforestation. The present study deals with the modelling of stream water temperatures using a stochastic approach to relate air and water temperatures in Catamaran Brook, a small stream in New Brunswick where long-term multidisciplinary habitat research is being carried out. The first step in the modelling approach was to establish the long
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20

Campbell, Mel, Donna Delparte, Matthew Belt, Zhongqi Chen, Christopher C. Caudill, and Trevor Caughlin. "Diel Variation in Summer Stream Temperature in an Idaho Desert Stream and Implications for Identifying Thermal Refuges." Climate 13, no. 3 (2025): 44. https://doi.org/10.3390/cli13030044.

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Thermal refuges in streams are essential for the survival of coldwater fish species such as Redband trout (Oncorhynchus mykiss) in landscapes with stressful or lethal stream temperatures. We utilized an uncrewed aerial system (UAS) mounted with thermal and natural color sensors to conduct hourly flights over a 24 h period in the desert stream Little Jacks Creek during late summer when temperatures were near seasonal maximums and streamflow was near seasonal minimums. We used fine-resolution imagery to map stream temperatures and characterize how our thermal sensor exhibits variability across a
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21

Kohil, Ahmed, Hassan Farag, and Mona Ossman. "Mathematical modeling of a multi-stream brazed aluminum plate fin heat exchanger." Thermal Science 14, no. 1 (2010): 103–14. http://dx.doi.org/10.2298/tsci1001103k.

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The need for small size and lightweight heat exchangers in many applications has resulted in the development of many heat transfer surfaces. This type of heat exchanger is much more compact than can be practically realized with circular tubes. In this work a steady-state mathematical model that representing one of the plate fin heat exchangers enclosed in cold box of an ethylene plant has been developed. This model could evaluate the performance of the heat exchanger by predicting the outlet temperatures of the hot and cold streams when the inlet conditions are known. The model has been valida
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22

Joughin, Ian, Slawek Tulaczyk, Douglas R. MacAyeal, and Hermann Engelhardt. "Melting and freezing beneath the Ross ice streams, Antarctica." Journal of Glaciology 50, no. 168 (2004): 96–108. http://dx.doi.org/10.3189/172756504781830295.

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AbstractWe have estimated temperature gradients and melt rates at the bottom of the ice streams in West Antarctica. Measured velocities were used to include the effects of horizontal advection and strain heating in the temperature model and to determine shear heating at the bed. Our modeled temperatures agree well with measured temperatures from boreholes in regions of steady flow. We find that ice-stream tributaries and the inland ice account for about 87% of the total melt generated beneath the Ross ice streams and their catchments. Our estimates indicate that the ice plains of Whillans Ice
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23

Troia, Matthew J., Michael A. Denk, and Keith B. Gido. "Temperature-dependent performance as a driver of warm-water fish species replacement along the river continuum." Canadian Journal of Fisheries and Aquatic Sciences 73, no. 3 (2016): 394–405. http://dx.doi.org/10.1139/cjfas-2015-0094.

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Replacement of fish species by their congeners along gradients of stream size is common in warm-water streams, but the causative environmental factors driving this turnover are not fully understood. We used laboratory experiments to test for differences in temperature-dependent egg hatch success and age-0 food ration size for three congeneric cyprinids that differ in abundance along temperature–stream size gradients. Headwater species (Pimephales promelas and Pimephales notatus) had lower thermal optima and narrower thermal breadths for hatch success compared with a river mainstem species (Pim
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24

Letcher, Benjamin H., Daniel J. Hocking, Kyle O’Neil, Andrew R. Whiteley, Keith H. Nislow, and Matthew J. O’Donnell. "A hierarchical model of daily stream temperature using air-water temperature synchronization, autocorrelation, and time lags." PeerJ 4 (February 29, 2016): e1727. http://dx.doi.org/10.7717/peerj.1727.

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Water temperature is a primary driver of stream ecosystems and commonly forms the basis of stream classifications. Robust models of stream temperature are critical as the climate changes, but estimating daily stream temperature poses several important challenges. We developed a statistical model that accounts for many challenges that can make stream temperature estimation difficult. Our model identifies the yearly period when air and water temperature are synchronized, accommodates hysteresis, incorporates time lags, deals with missing data and autocorrelation and can include external drivers.
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25

Du, Xinzhong, Greg Goss, and Monireh Faramarzi. "Impacts of Hydrological Processes on Stream Temperature in a Cold Region Watershed Based on the SWAT Equilibrium Temperature Model." Water 12, no. 4 (2020): 1112. http://dx.doi.org/10.3390/w12041112.

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Variance in stream temperature from historical norms, which reflects the impacts from both hydrological and meteorological factors, is a significant indicator of the stream ecosystem health. Therefore, it is imperative to study the hydrological processes controlling stream temperature in the watershed. The impacts of hydrological processes on stream temperature in the cold region of Western Canada were investigated based on the previously developed Soil and Water Assessment Tool (SWAT) equilibrium temperature model. The model was calibrated and validated for streamflow and stream temperature b
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26

Mauger, Sue, Rebecca Shaftel, Jason C. Leppi, and Daniel J. Rinella. "Summer temperature regimes in southcentral Alaska streams: watershed drivers of variation and potential implications for Pacific salmon." Canadian Journal of Fisheries and Aquatic Sciences 74, no. 5 (2017): 702–15. http://dx.doi.org/10.1139/cjfas-2016-0076.

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Climate is changing fastest in high-latitude regions, focusing our research on understanding rates and drivers of changing temperature regimes in southcentral Alaska streams and implications for salmon populations. We collected continuous water and air temperature data during open-water periods from 2008 to 2012 in 48 nonglacial salmon streams across the Cook Inlet basin spanning a range of watershed characteristics. The most important predictors of maximum temperatures, expressed as mean July temperature, maximum weekly average temperature, and maximum weekly maximum temperature (MWMT), were
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27

Tronstad, Lusha M., J. Joseph Giersch, Scott Hotaling, et al. "Assessing thermal tolerance of vulnerable alpine stream insects as part of a long-term monitoring project in the Teton Range, Wyoming." UW National Parks Service Research Station Annual Reports 41 (December 15, 2018): 98–104. http://dx.doi.org/10.13001/uwnpsrc.2018.5661.

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Alpine streams are predicted to decline as air temperatures warm and their water sources dry. Stream temperatures are expected to increase as glaciers and permanent snowfields decrease in size. For aquatic insects that are cold-adapted and restricted to small, high elevation streams fed by glaciers or snowfields, warmer water temperatures could be lethal. Conversely, less water in streams may increase the likelihood of insects freezing during winter months. We measured the critical thermal maximum (CTMAX) – the highest non-lethal temperature an insect can survive, and supercooling temperature
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28

Ahmad, Mateen, Waseem Saeed, and Khaqan Javed. "Temperature Distribution Analysis along the Length of Floating Head Multi Stream Heat Exchanger." International Journal of Chemical Engineering and Applications 12, no. 3 (2021): 17–21. http://dx.doi.org/10.18178/ijcea.2021.12.3.790.

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Heat transfer between two streams is common and simple and well established and perfectly commercialized. Normally, the exchanger that is used for this purpose is shell and tube heat exchanger but in some industrial production unit where more than one reactant is to be preheated or pre-cooled for chemical reaction and same as post heating and post cooling required of multiple streams at same or different temperatures, Problem that is associated with such type shell and tube heat exchanger is that it can’t handle the multiple stream and for handling multiple streams we required more number of e
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29

Kurylyk, B. L., K. T. B. MacQuarrie, D. Caissie, and J. M. McKenzie. "Shallow groundwater thermal sensitivity to climate change and land cover disturbances: derivation of analytical expressions and implications for stream temperature projections." Hydrology and Earth System Sciences Discussions 11, no. 11 (2014): 12573–626. http://dx.doi.org/10.5194/hessd-11-12573-2014.

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Abstract. Climate change is expected to increase stream temperatures, and the projected warming may alter the spatial extent of habitat for coldwater fish and other aquatic taxa. Recent studies have proposed that stream thermal sensitivities, derived from short term air temperature variations, can be employed to infer future stream warming due to long term climate change. However, this approach does not consider the potential for streambed heat fluxes to increase due to gradual warming of shallow groundwater. The temperature of shallow groundwater is particularly important for the thermal regi
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30

Briggs, Martin A., Phillip Goodling, Zachary C. Johnson, et al. "Bedrock depth influences spatial patterns of summer baseflow, temperature and flow disconnection for mountainous headwater streams." Hydrology and Earth System Sciences 26, no. 15 (2022): 3989–4011. http://dx.doi.org/10.5194/hess-26-3989-2022.

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Abstract. In mountain headwater streams, the quality and resilience of summer cold-water habitat is generally regulated by stream discharge, longitudinal stream channel connectivity and groundwater exchange. These critical hydrologic processes are thought to be influenced by the stream corridor bedrock contact depth (sediment thickness), a parameter often inferred from sparse hillslope borehole information, piezometer refusal and remotely sensed data. To investigate how local bedrock depth might control summer stream temperature and channel disconnection (dewatering) patterns, we measured stre
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31

Brown, Alastair. "Stream temperature velocity." Nature Climate Change 6, no. 5 (2016): 440. http://dx.doi.org/10.1038/nclimate3015.

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32

Anderson, Paul D., David J. Larson, and Samuel S. Chan. "Riparian Buffer and Density Management Influences on Microclimate of Young Headwater Forests of Western Oregon." Forest Science 53, no. 2 (2007): 254–69. http://dx.doi.org/10.1093/forestscience/53.2.254.

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Abstract Thinning of 30- to 70-year-old Douglas-fir (Pseudotsuga menziesii [Mirb.] Franco) stands is a common silvicultural activity on federal forest lands of the Pacific Northwest, United States. Empirical relationships among riparian functions, silvicultural treatments, and different riparian buffer widths are not well documented for small headwater streams. We investigated buffer width and density management effects on riparian microclimates of headwater streams in western Oregon. Spatial variations in stand density, canopy cover, and microclimate were measured along transects extending fr
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Malard, Florian, Alain Mangin, Urs Uehlinger, and J. V. Ward. "Thermal heterogeneity in the hyporheic zone of a glacial floodplain." Canadian Journal of Fisheries and Aquatic Sciences 58, no. 7 (2001): 1319–35. http://dx.doi.org/10.1139/f01-079.

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We examined the thermal regime of surface and hyporheic waters at three kryal sites and four krenal streams within the channel network of a glacial floodplain. Temperature was continuously measured for 1 year in the surface stream and at sediment depths of 30 and 80 cm. The vertical pattern of water temperature was strongly influenced by the direction and intensity of surface water – groundwater exchanges. At sites characterized by strong downwelling of surface waters, the thermal regimes of surface and hyporheic waters were virtually identical. In contrast, inputs of groundwater substantially
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34

Abdrabboh, M., and G. A. Karim. "An Investigation of the Volatilization of Oil Sand Surfaces When Subjected to Parallel Hot Gaseous Streams." Journal of Energy Resources Technology 108, no. 4 (1986): 343–46. http://dx.doi.org/10.1115/1.3231287.

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Preshaped rectangular sand slabs were subjected to hot oxidizing streams. The rate of mass loss due to fluid volatilization at constant stream temperature was established and correlated with time by a simple analytical expression that fitted the experimental data well. The correlation parameters showed that the ultimate extent of volatilization depends uniquely on the surrounding stream temperature. The time rate of mass loss was found to be a function of Reynolds and Schmidt numbers and the temperature of the heating stream.
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Rauch, Martina, Saša Mudrinić, and Antun Galović. "Detailed Analysis of Exergy Destruction of All Basic Types of Heat Exchangers." Processes 10, no. 2 (2022): 249. http://dx.doi.org/10.3390/pr10020249.

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Dimensionless expressions of exergy destruction, normalized to ambient temperature and heat capacity of the weaker stream, for all basic types of recuperators are derived. The analytical expressions for maximum exergy destruction were calculated using the GNU Octave software for all recuperators, namely parallel-flow and counter-flow recuperators, and all forms of cross-flow heat exchangers, namely without mixing of streams, only mixing the streamlines of the weaker stream, only mixing the streamlines of the stronger stream and mixing the weaker and stronger streams. For parallel-flow and coun
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36

Mahlum, Shad K., Lisa A. Eby, Michael K. Young, Chris G. Clancy, and Mike Jakober. "Effects of wildfire on stream temperatures in the Bitterroot River Basin, Montana." International Journal of Wildland Fire 20, no. 2 (2011): 240. http://dx.doi.org/10.1071/wf09132.

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Wildfire is a common natural disturbance that can influence stream ecosystems. Of particular concern are increases in water temperature during and following fires, but studies of these phenomena are uncommon. We examined effects of wildfires in 2000 on maximum water temperature for a suite of second- to fourth-order streams with a range of burn severities in the Bitterroot River basin, Montana. Despite many sites burning at high severity, there were no apparent increases in maximum water temperature during the fires. One month after fire and in the subsequent year, increases in maximum water t
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37

Hornbach, Daniel J. "Multi-Year Monitoring of Ecosystem Metabolism in Two Branches of a Cold-Water Stream." Environments 8, no. 3 (2021): 19. http://dx.doi.org/10.3390/environments8030019.

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Climate change is likely to have large impacts on freshwater biodiversity and ecosystem function, especially in cold-water streams. Ecosystem metabolism is affected by water temperature and discharge, both of which are expected to be affected by climate change and, thus, require long-term monitoring to assess alterations in stream function. This study examined ecosystem metabolism in two branches of a trout stream in Minnesota, USA over 3 years. One branch was warmer, allowing the examination of elevated temperature on metabolism. Dissolved oxygen levels were assessed every 10 min from spring
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Michel, Adrien, Tristan Brauchli, Michael Lehning, Bettina Schaefli, and Hendrik Huwald. "Stream temperature and discharge evolution in Switzerland over the last 50 years: annual and seasonal behaviour." Hydrology and Earth System Sciences 24, no. 1 (2020): 115–42. http://dx.doi.org/10.5194/hess-24-115-2020.

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Abstract. Stream temperature and discharge are key hydrological variables for ecosystem and water resource management and are particularly sensitive to climate warming. Despite the wealth of meteorological and hydrological data, few studies have quantified observed stream temperature trends in the Alps. This study presents a detailed analysis of stream temperature and discharge in 52 catchments in Switzerland, a country covering a wide range of alpine and lowland hydrological regimes. The influence of discharge, precipitation, air temperature, and upstream lakes on stream temperatures and thei
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Nam, Sooyoun, Honggeun Lim, Byoungki Choi, Qiwen Li, Haewon Moon, and Hyung Tae Choi. "Responses of Stream Water Temperature to Water Levels in Forested Catchments of South Korea." Forests 14, no. 10 (2023): 2085. http://dx.doi.org/10.3390/f14102085.

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Event flow characteristics were evaluated based on temperature and level of stream water in 22 forested catchments (area: 13.2–281.4 ha) to investigate sustainable flood management measures. Temperature and stream water levels were during 346 rainfall events in the summer season (July–September) from 2020 to 2022. Rising stream water levels responded to falling stream water temperature between ≤100 and >100 ha forested catchments in two types of time of concentration. Stream water temperature decreased by 3.0 °C when the stream water level increased by up to 0.9 m during rainfall events. Fa
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40

Preall, Richard J., and Neil H. Ringler. "Comparison of Actual and Potential Growth Rates of Brown Trout (Salmo trutta) in Natural Streams Based on Bioenergetic Models." Canadian Journal of Fisheries and Aquatic Sciences 46, no. 6 (1989): 1067–76. http://dx.doi.org/10.1139/f89-138.

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A ratio of specific growth rate to predicted maximum growth rate was employed as an ecological growth coefficient (EGC) in identifying major determinants of growth for brown trout, Salmo trutta, in natural streams. The coefficient may be more useful than specific growth rate when comparing trout populations from streams having diverse characteristics, since it accounts for the quantitative effects of stream temperature and mean trout weight. The maximum growth rate was generated by translating Elliott's bioenergetic equations into computer models applicable to fish weighing 5–300 g and to stre
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Surfleet, Christopher, and Justin Louen. "The Influence of Hyporheic Exchange on Water Temperatures in a Headwater Stream." Water 10, no. 11 (2018): 1615. http://dx.doi.org/10.3390/w10111615.

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A headwater stream in coastal California was used to evaluate the temperature response of effective shade reduction. Spatial distribution of stream water temperatures for summer low-flow conditions (<0.006 m3 s−1) were highly correlated with net radiation and advective heat transfers from hyporheic exchange and subsequent streambed conduction. Using a heat budget model, mean maximum stream water temperatures were predicted to increase by 1.7 to 2.2 °C for 50% and 0% effective shade scenarios, respectively, at the downstream end of a 300 m treatment reach. Effects on mean maximum stream wate
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42

Kreutzweiser, David P., Scott S. Capell, and Stephen B. Holmes. "Stream temperature responses to partial-harvest logging in riparian buffers of boreal mixedwood forest watersheds." Canadian Journal of Forest Research 39, no. 3 (2009): 497–506. http://dx.doi.org/10.1139/x08-191.

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As part of a larger study to examine the operational feasibility, ecological benefits, and environmental impacts of partial-harvest logging in riparian buffers along boreal mixedwood forest streams, we determined the effects on summer stream temperatures. Three logged study reaches were compared with three reference reaches over two prelogging and two postlogging summers. Partial-harvest logging resulted in an average removal of 10%, 20%, and 28% of the basal area from riparian buffers at the three logged sites. At the two more intensively logged sites, there were small (<10%) reductions in
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Bykanov, Serhii, Babak Tetiana Babak, and Roman Stotskyi. "THERMAL INTEGRATION OF COMPRESSION REFRIGERATION UNITS IN DAIRY FACILITIES." Bulletin of the National Technical University "KhPI". Series: Chemistry, Chemical Technology and Ecology, no. 1(5) (May 15, 2021): 92–98. http://dx.doi.org/10.20998/2079-0821.2021.01.14.

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The heat integration of an ammonia compression refrigeration unit, that is used in different dairy facilities, was carried out by the pinch analysis methods. The schematic diagram of such unit with a cooling capacity of 1000 kW was taken as a basis. The main cycle temperatures, refrigerant consumption and its specific heat capacity were calculated for a given refrigerating capacity. Based on these data, a stream table was formed, that included a hot stream of a refrigerant – ammonia – and also two cold streams: water for chemical water treatment and water for technology. The hot stream of ammo
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Seyedhashemi, Hanieh, Jean-Philippe Vidal, Jacob S. Diamond, et al. "Regional, multi-decadal analysis on the Loire River basin reveals that stream temperature increases faster than air temperature." Hydrology and Earth System Sciences 26, no. 9 (2022): 2583–603. http://dx.doi.org/10.5194/hess-26-2583-2022.

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Abstract. Stream temperature appears to be increasing globally, but its rate remains poorly constrained due to a paucity of long-term data and difficulty in parsing effects of hydroclimate and landscape variability. Here, we address these issues using the physically based thermal model T-NET (Temperature-NETwork) coupled with the EROS semi-distributed hydrological model to reconstruct past daily stream temperature and streamflow at the scale of the entire Loire River basin in France (105 km2 with 52 278 reaches). Stream temperature increased for almost all reaches in all seasons (mean =+0.38 ∘
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Dzara, Jessica R., Bethany T. Neilson, and Sarah E. Null. "Quantifying thermal refugia connectivity by combining temperature modeling, distributed temperature sensing, and thermal infrared imaging." Hydrology and Earth System Sciences 23, no. 7 (2019): 2965–82. http://dx.doi.org/10.5194/hess-23-2965-2019.

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Abstract. Watershed-scale stream temperature models are often one-dimensional because they require fewer data and are more computationally efficient than two- or three-dimensional models. However, one-dimensional models assume completely mixed reaches and ignore small-scale spatial temperature variability, which may create temperature barriers or refugia for cold-water aquatic species. Fine spatial- and temporal-resolution stream temperature monitoring provides information to identify river features with increased thermal variability. We used distributed temperature sensing (DTS) to observe sm
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Gardner, Beth, Patrick J. Sullivan, and Arthur J. Lembo, Jr. "Predicting stream temperatures: geostatistical model comparison using alternative distance metrics." Canadian Journal of Fisheries and Aquatic Sciences 60, no. 3 (2003): 344–51. http://dx.doi.org/10.1139/f03-025.

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The Beaverkill Watershed in the Catskill Mountains of New York, U.S.A., shows evidence of high summer stream temperatures throughout critical trout habitat. Because habitat quality, as characterized by stream temperature, dramatically influences trout communities, it is important for biologists to identify and map these characteristics and to monitor how they change over time. Stream temperatures were recorded over time throughout the Beaverkill Watershed and were used to identify thermal refugia and areas of thermal stress. Seventy-two temperature loggers were placed throughout the watershed
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Ficklin, D. L., B. L. Barnhart, J. H. Knouft, et al. "Climate change and stream temperature projections in the Columbia River basin: habitat implications of spatial variation in hydrologic drivers." Hydrology and Earth System Sciences 18, no. 12 (2014): 4897–912. http://dx.doi.org/10.5194/hess-18-4897-2014.

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Abstract. Water temperature is a primary physical factor regulating the persistence and distribution of aquatic taxa. Considering projected increases in air temperature and changes in precipitation in the coming century, accurate assessment of suitable thermal habitats in freshwater systems is critical for predicting aquatic species' responses to changes in climate and for guiding adaptation strategies. We use a hydrologic model coupled with a stream temperature model and downscaled general circulation model outputs to explore the spatially and temporally varying changes in stream temperature
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Ficklin, D. L., B. L. Barnhart, J. H. Knouft, et al. "Climate change and stream temperature projections in the Columbia River Basin: biological implications of spatial variation in hydrologic drivers." Hydrology and Earth System Sciences Discussions 11, no. 6 (2014): 5793–829. http://dx.doi.org/10.5194/hessd-11-5793-2014.

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Abstract. Water temperature is a primary physical factor regulating the persistence and distribution of aquatic taxa. Considering projected increases in temperature and changes in precipitation in the coming century, accurate assessment of suitable thermal habitat in freshwater systems is critical for predicting aquatic species responses to changes in climate and for guiding adaptation strategies. We use a hydrologic model coupled with a stream temperature model and downscaled General Circulation Model outputs to explore the spatially and temporally varying changes in stream temperature at the
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49

Stefan, Heinz G., and Eric B. Preud'homme. "STREAM TEMPERATURE ESTIMATION FROM AIR TEMPERATURE." Journal of the American Water Resources Association 29, no. 1 (1993): 27–45. http://dx.doi.org/10.1111/j.1752-1688.1993.tb01502.x.

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Dolinsek, Ivan J., Robert L. McLaughlin, James W. A. Grant, Lisa M. O’Connor, and Thomas C. Pratt. "Do natural history data predict the movement ecology of fishes in Lake Ontario streams?" Canadian Journal of Fisheries and Aquatic Sciences 71, no. 8 (2014): 1171–85. http://dx.doi.org/10.1139/cjfas-2013-0294.

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Little is known about the movements of most stream fishes, so fisheries managers often rely on natural history data from the literature to make management decisions. Observations of over 15 000 individuals from 37 species across 3 years were used to evaluate four aspects of the reliability of literature data for predicting the movement behaviour of stream fishes: (i) water temperature when fish enter streams; (ii) reasons for moving into the streams; (iii) stream residence times of migrants; and (iv) relative use of lake and stream habitats. Comparisons of our data for arrival times in the str
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