Articles | Volume 12, issue 5
https://doi.org/10.5194/esurf-12-1027-2024
https://doi.org/10.5194/esurf-12-1027-2024
Research article
 | 
16 Sep 2024
Research article |  | 16 Sep 2024

How water, temperature, and seismicity control the preconditioning of massive rock slope failure (Hochvogel)

Johannes Leinauer, Michael Dietze, Sibylle Knapp, Riccardo Scandroglio, Maximilian Jokel, and Michael Krautblatter

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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-2024-231', Maximillian Van Wyk de Vries, 09 Mar 2024
  • CC1: 'Comment on egusphere-2024-231', Giacomo Medici, 12 Mar 2024
  • RC2: 'Comment on egusphere-2024-231', Anonymous Referee #2, 18 Mar 2024
  • AC1: 'Comment on egusphere-2024-231', Johannes Leinauer, 25 Apr 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Johannes Leinauer on behalf of the Authors (25 Apr 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (15 Jul 2024) by Robert Hilton
ED: Publish as is (15 Jul 2024) by Wolfgang Schwanghart (Editor)
AR by Johannes Leinauer on behalf of the Authors (29 Jul 2024)  Author's response   Manuscript 
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Short summary
Massive rock slope failures are a significant alpine hazard and change the Earth's surface. Therefore, we must understand what controls the preparation of such events. By correlating 4 years of slope displacements with meteorological and seismic data, we found that water from rain and snowmelt is the most important driver. Our approach is applicable to similar sites and indicates where future climatic changes, e.g. in rain intensity and frequency, may alter the preparation of slope failure.