On how spatial variations of channel width influence river profile curvature

Author:

Ferrer-Boix Carles1,Chartrand Shawn M.1,Hassan Marwan A.1,Martín-Vide Juan P.2,Parker Gary3

Affiliation:

1. Department of Geography; University of British Columbia; Vancouver British Columbia Canada

2. Department of Civil and Environmental Engineering; Technical University of Catalonia; Barcelona Spain

3. Department of Civil and Environmental Engineering, Department of Geology; University of Illinois at Urbana-Champaign; Urbana Illinois USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference45 articles.

1. Development of longitudinal profiles of alluvial channels in response to base-level lowering;Begin;Earth Surf. Processes Landforms,1981

2. Stochastic forcing of sediment routing and storage in channel networks;Benda;Water Resour. Res.,1997

3. Laboratory study of degradation and aggradation;Bhimadipaty;J. Waterw. Port Coastal Ocean Eng.,1971

4. Knickpoint recession rate and catchment area: The case of uplifted rivers in Eastern Scotland;Bishop;Earth Surf. Processes Landforms,2005

5. On the equilibrium profile of river beds;Bolla Pittaluga;J. Geophys. Res. Earth Surf.,2014

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