Articles | Volume 7, issue 4
https://doi.org/10.5194/esurf-7-911-2019
https://doi.org/10.5194/esurf-7-911-2019
Research article
 | 
01 Oct 2019
Research article |  | 01 Oct 2019

How does the downstream boundary affect avulsion dynamics in a laboratory bifurcation?

Gerard Salter, Vaughan R. Voller, and Chris Paola

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Gerard Salter on behalf of the Authors (09 Aug 2019)  Author's response   Manuscript 
ED: Publish as is (27 Aug 2019) by Paola Passalacqua
ED: Publish as is (04 Sep 2019) by Niels Hovius (Editor)
AR by Gerard Salter on behalf of the Authors (05 Sep 2019)  Author's response   Manuscript 
Download
Short summary
Bifurcations are the switches that steer water and sediment in delta and multithread river networks, playing an important role in shaping the landscape. In lab experiments, we found that when the downstream branches grow through time, frequent switching in the water and sediment partitioning occurs. In contrast, once sediment freely exits the downstream boundary, long periods of time when one branch dominates occur; however, unlike our theoretical prediction, these are not permanent.