Earth Surface Dynamics
Earth Surface Dynamics
ESurf
Articles | Volume 12, issue 6
Articles | Volume 12, issue 6
https://doi.org/10.5194/esurf-12-1415-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-12-1415-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 12, issue 6
Research article
 | 
13 Dec 2024
Research article |  | 13 Dec 2024

Post-fire evolution of ravel transport regimes in the Diablo Range, CA

Hayden L. Jacobson, Danica L. Roth, Gabriel Walton, Margaret Zimmer, and Kerri Johnson

Viewed

Total article views: 3,729 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,547 823 359 3,729 227 282
  • HTML: 2,547
  • PDF: 823
  • XML: 359
  • Total: 3,729
  • BibTeX: 227
  • EndNote: 282
Views and downloads (calculated since 10 Apr 2024)
Cumulative views and downloads (calculated since 10 Apr 2024)

Viewed (geographical distribution)

Total article views: 3,729 (including HTML, PDF, and XML) Thereof 3,681 with geography defined and 48 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 08 Aug 2026
Download
Short summary
Loose grains travel farther after a fire because no vegetation is left to stop them. This matters since loose grains at the base of a slope can turn into a debris flow if it rains. To find if grass growing back after a fire had different impacts on grains of different sizes on slopes of different steepness, we dropped thousands of natural grains and measured how far they went. Large grains went farther 7 months after the fire than 11 months after, and small grain movement didn’t change much.
Read more
Share