The problem of predicting the size distribution of sediment supplied by hillslopes to rivers

Author:

Sklar Leonard S.ORCID,Riebe Clifford S.,Marshall Jill A.,Genetti Jennifer,Leclere Shirin,Lukens Claire L.,Merces Viviane

Funder

NSF

Doris and David Dawdy Fund for Hydrologic Science

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference161 articles.

1. Using soil residence time to delineate spatial and temporal patterns of transient landscape response;Almond;J. Geophys. Res. Earth Surf.,2007

2. Changes of bedload characteristics along the Marsyandi River (central Nepal): implications for understanding hillslope sediment supply, sediment load evolution along fluvial networks, and denudation in active orogenic belts;Attal;Geol. Soc. Am. Spec. Pap.,2006

3. Impact of change in erosion rate and landscape steepness on hillslope and fluvial sediments grain size in the Feather River Basin (Sierra Nevada, California);Attal;Earth Surf. Dyn.,2015

4. Geomorphologic evidence for the late Pliocene onset of hyperaridity in the Atacama Desert;Amundson;Geol. Soc. Am. Bull.,2012

5. Hillslope soils and vegetation;Amundson;Geomorphology,2015

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