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...

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Bibliographic Details
Main Authors: T. Müller, M. A. Hassan
Format: Article
Language:English
Published: Copernicus Publications 2018-11-01
Series:Earth Surface Dynamics
Online Access:https://www.earth-surf-dynam.net/6/1041/2018/esurf-6-1041-2018.pdf