Articles | Volume 6, issue 3
https://doi.org/10.5194/esurf-6-583-2018
https://doi.org/10.5194/esurf-6-583-2018
Research article
 | 
25 Jul 2018
Research article |  | 25 Jul 2018

Evidence of, and a proposed explanation for, bimodal transport states in alluvial rivers

Kieran B. J. Dunne and Douglas J. Jerolmack

Viewed

Total article views: 4,272 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,922 1,204 146 4,272 353 104 112
  • HTML: 2,922
  • PDF: 1,204
  • XML: 146
  • Total: 4,272
  • Supplement: 353
  • BibTeX: 104
  • EndNote: 112
Views and downloads (calculated since 06 Dec 2017)
Cumulative views and downloads (calculated since 06 Dec 2017)

Viewed (geographical distribution)

Total article views: 4,272 (including HTML, PDF, and XML) Thereof 4,097 with geography defined and 175 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 21 Feb 2025
Download
Short summary
What controls the size and shape of a river – its width, depth, and slope? The cross-sectional channel geometry of gravel-bedded rivers is understood to be a function of the river's fluid shear stress and the weight of the average particle on its bed; however, there is no satisfactory explanation for sand-bedded rivers. We analyze global datasets and individual river profiles and propose that accounting for riverbank cohesion could allow for an explanation for sand-bedded river channel geometry.
Share