Articles | Volume 9, issue 2
https://doi.org/10.5194/esurf-9-333-2021
https://doi.org/10.5194/esurf-9-333-2021
Research article
 | 
21 Apr 2021
Research article |  | 21 Apr 2021

Effect of stress history on sediment transport and channel adjustment in graded gravel-bed rivers

Chenge An, Marwan A. Hassan, Carles Ferrer-Boix, and Xudong Fu

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Status: closed
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Chenge An on behalf of the Authors (28 Nov 2020)  Author's response   Manuscript 
ED: Reconsider after major revisions (08 Dec 2020) by Francois Metivier
AR by Chenge An on behalf of the Authors (13 Dec 2020)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (05 Mar 2021) by Francois Metivier
ED: Publish as is (09 Mar 2021) by Niels Hovius (Editor)
AR by Chenge An on behalf of the Authors (12 Mar 2021)  Manuscript 
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Short summary
Mountain rivers are characterized by fluctuations of water flow, including both flood and inter-flood low flow. Recently, increasing attention has been paid to how inter-flood low flow affects the sediment transport in subsequent floods. Here we present a series of flume experiments. Results show that the existence of inter-flood low flow can reduce the sediment transport at the beginning of the subsequent flood. However, such an effect is gradually erased with the increase of flow intensity.