Articles | Volume 22, issue 10
Nat. Hazards Earth Syst. Sci., 22, 3183–3209, 2022
https://doi.org/10.5194/nhess-22-3183-2022
Nat. Hazards Earth Syst. Sci., 22, 3183–3209, 2022
https://doi.org/10.5194/nhess-22-3183-2022
Research article
06 Oct 2022
Research article | 06 Oct 2022

Physically based modeling of co-seismic landslide, debris flow, and flood cascade

Bastian van den Bout et al.

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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 nhess-2021-292', Martin Mergili, 21 Feb 2022
    • AC1: 'Reply on RC1', Bastian van den Bout, 23 May 2022
  • RC2: 'Comment on nhess-2021-292', Tommaso Baggio, 07 Mar 2022
    • AC2: 'Reply on RC2', Bastian van den Bout, 23 May 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (25 May 2022) by Andreas Günther
AR by Bastian van den Bout on behalf of the Authors (02 Jun 2022)  Author's response    Manuscript
ED: Publish subject to technical corrections (16 Jun 2022) by Andreas Günther

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Bastian van den Bout on behalf of the Authors (06 Oct 2022)   Author's adjustment   Manuscript
EA: Adjustments approved (06 Oct 2022) by Andreas Günther
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Short summary
Natural hazards such as earthquakes, landslides, and flooding do not always occur as stand-alone events. After the 2008 Wenchuan earthquake, a co-seismic landslide blocked a stream in Hongchun. Two years later, a debris flow breached the material, blocked the Min River, and resulted in flooding of a small town. We developed a multi-process model that captures the full cascade. Despite input and process uncertainties, probability of flooding was high due to topography and trigger intensities.
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