Rocky Mountain Research Station Publications
RMRS Online Publication - Journal
Articles, External Publications, and Special Reports
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
About PDFs: For best results, do not open the PDF in your Web browser. Right-click on the PDF link to download the PDF file directly to your computer. Click here for more PDF help.
Download Article
http://www.fs.fed.us/rm/pubs_other/rmrs_2008_buffington_j001.pdf
PDF File Size: 310 K
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