16 Environmental Geology in the Pacific Northwest (Posters)
Saturday, 5 May 2007
8:00 AM - 6:00 PM
QUANTIFYING THE GLACIAL MELTWATER COMPONENT OF STREAMFLOW IN A NORTH CASCADE BASIN USING A DISTRIBUTED HYDROLOGY MODEL
Paper number: 16-4
Program: THEME SESSIONS
Time: 8:00 AM – 6:00 PM
Authors
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Robert J. MitchellWestern Washington University, Bellingham, WA
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Doug H. ClarkWestern Washington University, Bellingham, WA
Abstract
The model was used to simulate streamflow using the current glacial coverage and three water years (2003 through 2005) of meteorological data from the basin. The late summer glacial meltwater contribution to streamflow from these simulations ranged from 8.4% for the wettest water year, to 26.1% for the driest water year. When the glacier size was reduced buy 17%, the late summer glacial meltwater contribution lowered to 5.5% and 19.2% for the wettest and driest water years, respectively. We also created hypothetical meteorological data inputs using predicted climate changes for the Pacific Northwest. When compared to current flow conditions, these simulation results indicate that a 15.7% reduction in late summer streamflow could occur when the glacier size is reduced by 17%, suggesting that fish habitat and the use of the Middle Fork Nooksack as a water supply source may be compromised in the future.