Articles | Volume 25, issue 3
https://doi.org/10.5194/nhess-25-1229-2025
https://doi.org/10.5194/nhess-25-1229-2025
Research article
 | 
31 Mar 2025
Research article |  | 31 Mar 2025

Topographic controls on landslide mobility: modeling hurricane-induced landslide runout and debris-flow inundation in Puerto Rico

Dianne L. Brien, Mark E. Reid, Collin Cronkite-Ratcliff, and Jonathan P. Perkins

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Reviewer comment on nhess-2024-141', Martin Mergili, 28 Oct 2024
    • AC1: 'Reply on RC1', Dianne Brien, 08 Nov 2024
  • RC2: 'Comment on nhess-2024-141', Anonymous Referee #2, 21 Nov 2024
    • AC2: 'Reply on RC2', Dianne Brien, 10 Dec 2024
  • RC3: 'Comment on nhess-2024-141', Anonymous Referee #3, 23 Nov 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (17 Dec 2024) by Margreth Keiler
AR by Dianne Brien on behalf of the Authors (06 Jan 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (20 Jan 2025) by Margreth Keiler
AR by Dianne Brien on behalf of the Authors (28 Jan 2025)
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Short summary
Landslide runout zones are the areas downslope or downstream of landslide initiation. People often live and work in these areas, leading to property damage and deaths. Landslide runout may occur on hillslopes or in channels, requiring different modeling approaches. We develop methods to identify potential runout zones and apply these methods to identify susceptible areas for three municipalities in Puerto Rico.
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