Articles | Volume 12, issue 6
https://doi.org/10.5194/esurf-12-1415-2024
https://doi.org/10.5194/esurf-12-1415-2024
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

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-2694', Emmanuel Gabet, 09 May 2024
  • RC2: 'Comment on egusphere-2023-2694', Anonymous Referee #2, 07 Jul 2024
  • EC1: 'Comment on egusphere-2023-2694', Tom Coulthard, 16 Jul 2024
  • AC1: 'Comment on egusphere-2023-2694', Hayden Jacobson, 01 Sep 2024
  • EC2: 'Comment on egusphere-2023-2694', Tom Coulthard, 04 Sep 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Hayden Jacobson on behalf of the Authors (01 Sep 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (04 Sep 2024) by Tom Coulthard
RR by Emmanuel Gabet (07 Sep 2024)
RR by Anonymous Referee #2 (24 Sep 2024)
ED: Publish subject to technical corrections (25 Sep 2024) by Tom Coulthard
ED: Publish subject to technical corrections (07 Oct 2024) by Tom Coulthard (Editor)
AR by Hayden Jacobson on behalf of the Authors (17 Oct 2024)  Manuscript 
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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.