Sensitivity of Summer Stream Temperatures to Climate Variability in the Pacific Northwest United States

Charles H Luce, USDA Forest Service, Rocky Mountain Research Station, Boise, ID, United States, Brian Staab, US Forest Service, Portland, OR, United States, Marc G Kramer, University of Florida, Soil and Water Science Department, Ft Walton Beach, FL, United States, Seth Wenger, University of Georgia, River Basin Center - Odum School of Ecology, Athens, GA, United States, Dan Isaak, USDA Forest Service, Boise, ID, United States and Callie McConnell, US Forest Service, Washington Office, United States

Contact First Author: Charles H Luce; chluce@msn.com

Previously Published Material: Recently published in a paper in Water Resources Research (Summer 2014).  No presentation has been made at a professional society meeting.

Abstract ID#: 35828

 

English Abstract:
Estimating differences in thermal response among streams to a warming climate is important for prioritizing native fish conservation efforts. While there are plentiful estimates of air temperature responses to climate change, the sensitivity of streams, particularly small headwater streams, to warming temperatures is less well understood. A substantial body of literature correlates sub-annual scale temperature variations in air and stream temperatures driven by annual cycles in solar angle; however, these may be a low-precision proxy for climate change driven changes in the stream energy balance. We analyzed summer stream temperature records from forested streams in the Pacific Northwest for interannual correlations to air temperature and standardized annual streamflow departures. A significant pattern emerged where cold streams always showed lower sensitivities to air temperature variation, while warm streams could be insensitive or sensitive depending on geological or vegetation context. A pattern where cold streams are less sensitive to direct temperature increases is important for conservation planning, although substantial questions may yet remain for secondary effects related to snow, runoff, groundwater, or vegetation changes induced by climate change.