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Discussion of "Evaluating vertical velocities between the stream and the hyporheic zone from temperature data" by Seydell, I., Wawra, B.E., and Zanke, U.C.E


Buffington, John M.; Tonina, Daniele. 2008. Discussion of "Evaluating vertical velocities between the stream and the hyporheic zone from temperature data" by Seydell, I., Wawra, B.E., and Zanke, U.C.E. In: Habersack, H.; Piégay, H.; Rinaldi, M., eds. Gravel-bed rivers 6-from process understanding to river restoration. Elsevier: 128-131.

Hyporheic exchange is principally driven by spatial variations of near-bed pressure, which can be sensitive to seasonal changes in discharge, flow depth, and watersurface profile (Tonina and Buffington, 2003, 2007). Simulations of hyporheic exchange across two-dimensional pool-riffle topography show that the strength and spatial extent of the hyporheic exchange vary with discharge.

Keywords: stream, hyporheic exchange, temperature data


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http://www.fs.fed.us/rm/pubs_other/rmrs_2008_buffington_j001.pdf

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Title: RMRS Other Publications: Discussion of "Evaluating vertical velocities between the stream and the hyporheic zone from temperature data" by Seydell, I., Wawra, B.E., and Zanke, U.C.E
Electronic Publish Date: September 25, 2008
Last Update:
September 25, 2008

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