Fluvial response to changes in the magnitude and frequency of sediment supply in a 1-D model
<p>In steep headwater reaches, episodic mass movements can deliver large volumes of sediment to fluvial channels. If these inputs of sediment occur with a high frequency and magnitude, the capacity of the stream to rework the supplied material can be exceeded for a significant amount of tim...
Main Authors: | T. Müller, M. A. Hassan |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2018-11-01
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Series: | Earth Surface Dynamics |
Online Access: | https://www.earth-surf-dynam.net/6/1041/2018/esurf-6-1041-2018.pdf |
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