Continental-scale relationship between bankfull width and drainage area for single-thread alluvial channels

Author:

Wilkerson Gregory V.1,Kandel Dinesh R.1,Perg Lesley A.2,Dietrich William E.3,Wilcock Peter R.4,Whiles Matt R.5

Affiliation:

1. Department of Civil and Environmental Engineering; Southern Illinois University; Carbondale Illinois USA

2. Los Angeles; California USA

3. Department of Earth and Planetary Science; University of California; Berkley California USA

4. Department of Geography and Environmental Engineering; John Hopkins University; Baltimore Maryland USA

5. Department of Zoology; Southern Illinois University; Carbondale Illinois USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Reference78 articles.

1. How do big rivers come to be different?;Ashworth;Earth-Sci. Rev,2012

2. Width of streams and rivers in response to vegetation, bank material, and other factors;Anderson;J. Am. Water Resources Assoc.,2004

3. Synthesizing U.S. river restoration efforts;Bernhardt;Science,2005

4. Changes in characteristics and function of woody debris with increasing size of streams in western Washington;Bilby;Trans. Am. Fish. Soc.,1989

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