Articles | Volume 6, issue 1
https://doi.org/10.5194/esurf-6-163-2018
https://doi.org/10.5194/esurf-6-163-2018
Research article
 | 
05 Mar 2018
Research article |  | 05 Mar 2018

Topographical change caused by moderate and small floods in a gravel bed ephemeral river – a depth-averaged morphodynamic simulation approach

Eliisa S. Lotsari, Mikel Calle, Gerardo Benito, Antero Kukko, Harri Kaartinen, Juha Hyyppä, Hannu Hyyppä, and Petteri Alho

Viewed

Total article views: 3,012 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,682 1,208 122 3,012 99 87 108
  • HTML: 1,682
  • PDF: 1,208
  • XML: 122
  • Total: 3,012
  • Supplement: 99
  • BibTeX: 87
  • EndNote: 108
Views and downloads (calculated since 05 Sep 2017)
Cumulative views and downloads (calculated since 05 Sep 2017)

Viewed (geographical distribution)

Total article views: 3,012 (including HTML, PDF, and XML) Thereof 2,825 with geography defined and 187 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Apr 2024
Download
Short summary
This paper analyses the timing of topographical changes of a gravel bed ephemeral river channel during consecutive and moderate- and low-magnitude floods by applying a morphodynamic model calibrated with pre- and post-event surveys using RTK-GPS and mobile laser scanning. The channel acted as a braided river during lower flows but as a meandering river during higher flows. The channel changes can be greater during the long-lasting receding phase than during the rising phase of the floods.