Publication Date:
2012-04-19
Description:
Diel fluctuations can comprise a significant portion of summer discharge in small to medium catchments. The source of these signals and the manner in which they are propagated to stream gauging sites is poorly understood. In this work we analyze stream discharge from 15 subcatchments in Dry Creek, Idaho, Reynolds Creek, Idaho, and the HJ Andrews, Oregon. We identify diel signals in summer low flow, determine the lag between the diel signals and evapotranspiration demand, and identify seasonal trends in the evolution of the lag at each site. The lag between vegetation water use and streamflow response increases thorough the summer at each subcatchment, with the rate of increase a function of catchment stream length and other catchment characteristics such as geology, vegetation, and stream geomorphology. These findings support the hypothesis that variations in stream velocity are the key control on the seasonal evolution of the observed lags. Copyright © 2012 John Wiley & Sons, Ltd.
Print ISSN:
0885-6087
Electronic ISSN:
1099-1085
Topics:
Architecture, Civil Engineering, Surveying
,
Geography
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