Articles | Volume 13, issue 2
https://doi.org/10.5194/esurf-13-277-2025
https://doi.org/10.5194/esurf-13-277-2025
Research article
 | 
31 Mar 2025
Research article |  | 31 Mar 2025

Hillslope diffusion and channel steepness in landscape evolution models

David G. Litwin, Luca C. Malatesta, and Leonard S. Sklar

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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-2024-2418', Anonymous Referee #1, 13 Sep 2024
  • RC2: 'Comment on egusphere-2024-2418', Charles Shobe, 21 Sep 2024
  • AC1: 'Authors' response to reviewers', David Litwin, 28 Oct 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by David Litwin on behalf of the Authors (29 Oct 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (15 Nov 2024) by Simon Mudd
AR by David Litwin on behalf of the Authors (15 Dec 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (20 Jan 2025) by Simon Mudd
ED: Publish as is (31 Jan 2025) by Wolfgang Schwanghart (Editor)
AR by David Litwin on behalf of the Authors (04 Feb 2025)  Manuscript 
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Short summary
Channel–hillslope coupling in landscape evolution models can strongly affect channel profiles. When hillslope diffusion is applied everywhere and only topography is tracked, a new scaling predicts how detachment-limited channels steepen with hillslope diffusion. Field data support channel steepening to transport sediment but not as predicted by the scaling, highlighting the need for a critical inspection of channel–hillslope coupling approaches.
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