Sediment supply versus local hydraulic controls on sediment transport and storage in a river with large sediment loads

Author:

Dean David J.1,Topping David J.1,Schmidt John C.2,Griffiths Ronald E.1,Sabol Thomas A.1

Affiliation:

1. Grand Canyon Monitoring and Research Center, Southwest Biological Science Center; U.S. Geological Survey; Flagstaff Arizona USA

2. Department of Watershed Sciences, Quinney College of Natural Resources; Utah State University; Logan Utah USA

Funder

National Park Service

Commission of Environmental Cooperation (CEC)

U.S. Geological Survey, Southwest Biological Science Center

U.S. Bureau of Reclamation

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Reference112 articles.

1. Channel narrowing by vertical accretion along the Green River near Green River, Utah;Allred;Geol. Soc. Am. Bull.,1999

2. Relationship between sediment supply and avulsion frequency in braided rivers;Ashworth;Geology,2004

3. Stream-channel response to floods, with examples from central Texas;Baker;Geol. Soc. Am. Bull.,1977

4. Large shift in source of fine sediment in the Upper Mississippi River;Belmont;Environ. Sci. Technol.,2011

5. Sediment problems of the lower Colorado River;Borland;Proc. Am. Soc. Civ. Eng. J. Hydraul. Div.,1960

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