Articles | Volume 22, issue 7
Nat. Hazards Earth Syst. Sci., 22, 2219–2237, 2022
https://doi.org/10.5194/nhess-22-2219-2022
Nat. Hazards Earth Syst. Sci., 22, 2219–2237, 2022
https://doi.org/10.5194/nhess-22-2219-2022
Research article
06 Jul 2022
Research article | 06 Jul 2022

Spatial assessment of probable recharge areas – investigating the hydrogeological controls of an active deep-seated gravitational slope deformation

Jan Pfeiffer 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-2021-388', Catherine Bertrand, 01 Mar 2022
    • AC1: 'Reply on RC1', J. Pfeiffer, 10 May 2022
  • RC2: 'Comment on nhess-2021-388', Anonymous Referee #2, 05 Apr 2022
    • AC2: 'Reply on RC2', J. Pfeiffer, 10 May 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (further review by editor and referees) (23 May 2022) by Andreas Günther
AR by J. Pfeiffer on behalf of the Authors (24 May 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (27 May 2022) by Andreas Günther
RR by Catherine Bertrand (30 May 2022)
ED: Publish as is (01 Jun 2022) by Andreas Günther
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Short summary
The activity of slow-moving deep-seated landslides is commonly governed by pore pressure variations within the shear zone. Groundwater recharge as a consequence of precipitation therefore is a process regulating the activity of landslides. In this context, we present a highly automated geo-statistical approach to spatially assess groundwater recharge controlling the velocity of a deep-seated landslide in Tyrol, Austria.
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