Articles | Volume 25, issue 3
https://doi.org/10.5194/nhess-25-1037-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
Characterizing the scale of regional landslide triggering from storm hydrometeorology
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- Final revised paper (published on 10 Mar 2025)
- Preprint (discussion started on 03 Apr 2024)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Review of “Characterizing the scale of regional landslide triggering from storm hydrometeorology” by Perkins et al.,', Odin Marc, 22 Apr 2024
- AC1: 'Reply on RC1', Jonathan Perkins, 17 Jul 2024
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RC2: 'Comment on egusphere-2024-873', Ben Mirus, 14 May 2024
- AC2: 'Reply on RC2', Jonathan Perkins, 18 Jul 2024
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) (25 Jul 2024) by Olivier Dewitte
AR by Jonathan Perkins on behalf of the Authors (05 Sep 2024)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (11 Oct 2024) by Olivier Dewitte
RR by Ben Mirus (04 Nov 2024)
RR by Odin Marc (13 Nov 2024)
ED: Publish subject to technical corrections (14 Nov 2024) by Olivier Dewitte
AR by Jonathan Perkins on behalf of the Authors (12 Dec 2024)
Manuscript
The authors present an analysis of several storms induced landslide events, most relating to atmospheric rivers phenomena in California. They retrieve rainfall from a gridded gauge product (covering >10 years, 6hr resolution, 4km spatial resolution), and a leaky bucket model to constrain regolith moisture and derive a soil moisture anomaly, A*, relative to a 15 yr return event. They show that 15 yr return appear to be the minimal return time for causing extensive landsliding based on 4 well constrained cases and then show and discuss the advantage of using a soil moisture anomaly (rather than simple rainfall anomaly) to understand landsliding triggered by rainfall in California. The work is a nice progression from previous work arguing for the use of anomaly to study landslide event (Rainfall anomaly for Marc et al., 2019, or soil moisture anomaly for Saito and Matusyama 2012, but with a more complex methodology and rather preliminary data). Therefore the authors’ work goes provides first basis for simple, physically meainingful and regional scale indicators that could provide a basis for landslide hazard forecasting during storms. In terms of methodology and presentation, I had reviewed a previous version of this work and a lot of my previous concerns in terms of methodology and clarity have been addressed and this version of the draft appears very clear and well thought to me. I therefore congratulate the authors, as I think the work will be a very good contribution to Esurf !
I provide in the attached document a series of minor comments where I have identified potential improvements.
Sincerely, Odin Marc