Hydraulics, morphology, and energy dissipation in an alpine step-pool channel

Author:

Wilcox Andrew C.1,Wohl Ellen E.2,Comiti Francesco3,Mao Luca4

Affiliation:

1. Department of Geosciences; University of Montana; Missoula Montana USA

2. Department of Geosciences; Colorado State University; Fort Collins Colorado USA

3. Faculty of Science and Technology; Free University of Bozen-Bolzano; Bolzano Italy

4. Department of Land and Agro-Forest Environments; University of Padova; Legnaro Italy

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference99 articles.

1. The influence of roughness structure on flow resistance on steep slopes;Aberle;J. Hydraul. Res.,2003

2. Step-pool streams: Adjustment to maximum flow resistance;Abrahams;Water Resour. Res.,1995

3. Geomorphology of steepland headwaters: The transition from hillslopes to channels;Benda;J. Am. Water Resour. Assoc.,2005

4. 1 min in the life of a river: Selecting the optimal record length for the measurement of velocity in fluvial boundary layers;Buffin-Bélanger;Geomorphology,2005

5. Bunte , K. S. R. Abt K. W. Swingle J. P. Potyondy 2010 Bankfull mobile particle size and its predictions from a Shields-type approach 2nd Joint Federal Interagency Conference, Las Vegas, Nev.

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