Articles | Volume 18, issue 4
https://doi.org/10.5194/tc-18-2103-2024
https://doi.org/10.5194/tc-18-2103-2024
Research article
 | 
30 Apr 2024
Research article |  | 30 Apr 2024

Surface heat fluxes at coarse blocky Murtèl rock glacier (Engadine, eastern Swiss Alps)

Dominik Amschwand, Martin Scherler, Martin Hoelzle, Bernhard Krummenacher, Anna Haberkorn, Christian Kienholz, 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-2023-2109', Anonymous Referee #1, 29 Oct 2023
    • AC1: 'Reply on RC1', Dominik Amschwand, 10 Dec 2023
  • RC2: 'Comment on egusphere-2023-2109', Anonymous Referee #2, 31 Oct 2023
    • AC1: 'Reply on RC1', Dominik Amschwand, 10 Dec 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (13 Dec 2023) by Emily Collier
AR by Dominik Amschwand on behalf of the Authors (14 Jan 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (05 Feb 2024) by Emily Collier
AR by Dominik Amschwand on behalf of the Authors (14 Feb 2024)
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Short summary
Rock glaciers are coarse-debris permafrost landforms that are comparatively climate resilient. We estimate the surface energy balance of rock glacier Murtèl (Swiss Alps) based on a large surface and sub-surface sensor array. During the thaw seasons 2021 and 2022, 90 % of the net radiation was exported via turbulent heat fluxes and only 10 % was transmitted towards the ground ice table. However, early snowmelt and droughts make these permafrost landforms vulnerable to climate warming.