Articles | Volume 13, issue 6
https://doi.org/10.5194/esurf-13-1249-2025
https://doi.org/10.5194/esurf-13-1249-2025
Research article
 | 
24 Nov 2025
Research article |  | 24 Nov 2025

Rainfall and tectonic forcing lead to contrasting headwater slope evolutions

Yinbing Zhu, Patrice Rey, and Tristan Salles

Viewed

Total article views: 929 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
785 116 28 929 5 33 37
  • HTML: 785
  • PDF: 116
  • XML: 28
  • Total: 929
  • Supplement: 5
  • BibTeX: 33
  • EndNote: 37
Views and downloads (calculated since 23 Apr 2025)
Cumulative views and downloads (calculated since 23 Apr 2025)

Viewed (geographical distribution)

Total article views: 929 (including HTML, PDF, and XML) Thereof 929 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 25 Nov 2025
Download
Short summary
We use computer models to study how landscapes respond to changes in rainfall and tectonic uplift. We find that rainfall rate changes produce unique slope change reversals near the headwaters, which differ from the simpler responses caused by uplift rate changes. These reversals are more pronounced when hillslope diffusion is dominant. These findings help us understand how climate and tectonic forcing shape the landscape differently and may allow scientists to tell their effects apart in nature.
Share