Articles | Volume 29, issue 9
https://doi.org/10.5194/hess-29-2219-2025
https://doi.org/10.5194/hess-29-2219-2025
Research article
 | 
15 May 2025
Research article |  | 15 May 2025

Seasonal ice storage changes and meltwater generation at Murtèl rock glacier (Engadine, eastern Swiss Alps): estimates from measurements and energy budgets in the coarse blocky active layer

Dominik Amschwand, Seraina Tschan, Martin Scherler, Martin Hoelzle, Bernhard Krummenacher, Anna Haberkorn, Christian Kienholz, Lukas Aschwanden, and Hansueli Gubler

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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-2024-844', Anonymous Referee #1, 14 May 2024
    • AC1: 'Reply on RC1 and RC2', Dominik Amschwand, 12 Jul 2024
  • RC2: 'Comment on egusphere-2024-844', Ryan Webb, 20 May 2024
    • AC1: 'Reply on RC1 and RC2', Dominik Amschwand, 12 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) (17 Jul 2024) by Hongkai Gao
AR by Dominik Amschwand on behalf of the Authors (29 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (03 Sep 2024) by Hongkai Gao
RR by Anonymous Referee #1 (02 Oct 2024)
RR by Anonymous Referee #3 (23 Oct 2024)
ED: Publish subject to revisions (further review by editor and referees) (24 Oct 2024) by Hongkai Gao
AR by Dominik Amschwand on behalf of the Authors (18 Dec 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (29 Dec 2024) by Hongkai Gao
AR by Dominik Amschwand on behalf of the Authors (13 Jan 2025)  Author's response   Manuscript 
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Short summary
Meltwater from rock glaciers, frozen landforms of debris and ice, has gained attention in dry mountain regions. We estimated how much ice melts in Murtèl rock glacier (Swiss Alps) based on belowground heat flow measurements and observations of the rising and falling ground-ice table. We found seasonal aggradation and melt of 150–300 mm w.e. (20 %–40 % of the snowpack). The ice (largely sourced from refrozen snowmelt) melts in hot summer periods, infiltrates, and recharges groundwater.
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