Articles | Volume 21, issue 10
https://doi.org/10.5194/nhess-21-2949-2021
https://doi.org/10.5194/nhess-21-2949-2021
Research article
 | 
01 Oct 2021
Research article |  | 01 Oct 2021

A climatology of sub-seasonal temporal clustering of extreme precipitation in Switzerland and its links to extreme discharge

Alexandre Tuel and Olivia Martius

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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-2021-93', Anonymous Referee #1, 28 Apr 2021
    • AC1: 'Reply on RC1', Alexandre Tuel, 06 Jul 2021
  • RC2: 'Comment on nhess-2021-93', Anonymous Referee #2, 26 May 2021
    • AC2: 'Reply on RC2', Alexandre Tuel, 06 Jul 2021
  • CC1: 'Comment on nhess-2021-93', Manuela Irene Brunner, 01 Jun 2021
    • AC3: 'Reply on CC1', Alexandre Tuel, 07 Jul 2021

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) (26 Jul 2021) by Ricardo Trigo
AR by Alexandre Tuel on behalf of the Authors (16 Aug 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (25 Aug 2021) by Ricardo Trigo
RR by Anonymous Referee #1 (10 Sep 2021)
RR by Anonymous Referee #2 (10 Sep 2021)
ED: Publish subject to minor revisions (review by editor) (10 Sep 2021) by Ricardo Trigo
AR by Alexandre Tuel on behalf of the Authors (14 Sep 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (15 Sep 2021) by Ricardo Trigo
AR by Alexandre Tuel on behalf of the Authors (15 Sep 2021)  Author's response   Manuscript 
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Short summary
Extreme river discharge may be triggered by large accumulations of precipitation over short time periods, which can result from the successive occurrence of extreme-precipitation events. We find a distinct spatiotemporal pattern in the temporal clustering behavior of precipitation extremes over Switzerland, with clustering occurring on the northern side of the Alps in winter and on their southern side in fall. Clusters tend to be followed by extreme discharge, particularly in the southern Alps.
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