Articles | Volume 11, issue 4
https://doi.org/10.5194/esurf-11-741-2023
https://doi.org/10.5194/esurf-11-741-2023
Research article
 | 
09 Aug 2023
Research article |  | 09 Aug 2023

Self-organization of channels and hillslopes in models of fluvial landform evolution and its potential for solving scaling issues

Stefan Hergarten and Alexa Pietrek

Viewed

Total article views: 2,095 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,559 428 108 2,095 38 44
  • HTML: 1,559
  • PDF: 428
  • XML: 108
  • Total: 2,095
  • BibTeX: 38
  • EndNote: 44
Views and downloads (calculated since 25 Jul 2022)
Cumulative views and downloads (calculated since 25 Jul 2022)

Viewed (geographical distribution)

Total article views: 2,095 (including HTML, PDF, and XML) Thereof 1,970 with geography defined and 125 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 23 Nov 2024
Download
Short summary
The transition from hillslopes to channelized flow is typically attributed to a threshold catchment size in landform evolution models. Here we propose an alternative concept directly based on topography. Using this concept, channels and hillslopes self-organize, whereby the catchment size of the channel heads varies over some range. Our numerical results suggest that this concept works better than the established idea of a strict threshold catchment size.