Articles | Volume 23, issue 10
https://doi.org/10.5194/nhess-23-3261-2023
https://doi.org/10.5194/nhess-23-3261-2023
Research article
 | 
18 Oct 2023
Research article |  | 18 Oct 2023

Landslide initiation thresholds in data-sparse regions: application to landslide early warning criteria in Sitka, Alaska, USA

Annette I. Patton, Lisa V. Luna, Joshua J. Roering, Aaron Jacobs, Oliver Korup, and Benjamin B. Mirus

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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-2023-25', Anonymous Referee #1, 07 Apr 2023
    • AC1: 'Reply on RC1', Annette Patton, 31 May 2023
  • RC2: 'Comment on egusphere-2023-25', Anonymous Referee #2, 18 Apr 2023
    • AC2: 'Reply on RC2', Annette Patton, 31 May 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (01 Jun 2023) by Francesco Marra
AR by Annette Patton on behalf of the Authors (03 Jun 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (07 Jun 2023) by Francesco Marra
RR by Anonymous Referee #2 (21 Jun 2023)
RR by Anonymous Referee #1 (26 Jun 2023)
ED: Publish subject to technical corrections (26 Jun 2023) by Francesco Marra
ED: Publish subject to technical corrections (19 Aug 2023) by Paolo Tarolli (Executive editor)
AR by Annette Patton on behalf of the Authors (30 Aug 2023)  Manuscript 
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Short summary
Landslide warning systems often use statistical models to predict landslides based on rainfall. They are typically trained on large datasets with many landslide occurrences, but in rural areas large datasets may not exist. In this study, we evaluate which statistical model types are best suited to predicting landslides and demonstrate that even a small landslide inventory (five storms) can be used to train useful models for landslide early warning when non-landslide events are also included.
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