Articles | Volume 20, issue 9
https://doi.org/10.5194/tc-20-5365-2026
https://doi.org/10.5194/tc-20-5365-2026
Research article
 | 
21 Sep 2026
Research article |  | 21 Sep 2026

Feedbacks and timescales in the modelled transient response of debris-covered glaciers

Florian Hardmeier, James C. Ferguson, and Andreas Vieli

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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-2025-5997', Anonymous Referee #1, 14 Mar 2026
    • AC2: 'Reply on RC1', Florian Hardmeier, 04 Jun 2026
  • RC2: 'Comment on egusphere-2025-5997', Anonymous Referee #2, 26 Apr 2026
    • AC1: 'Reply on RC2', Florian Hardmeier, 04 Jun 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (09 Jun 2026) by Anna Crawford
AR by Florian Hardmeier on behalf of the Authors (21 Jul 2026)  Author's response 
EF by Katja Gänger (23 Jul 2026)  Manuscript   Author's tracked changes 
ED: Referee Nomination & Report Request started (06 Aug 2026) by Anna Crawford
RR by Anonymous Referee #1 (18 Aug 2026)
RR by Anonymous Referee #2 (22 Aug 2026)
ED: Publish subject to minor revisions (review by editor) (24 Aug 2026) by Anna Crawford
AR by Florian Hardmeier on behalf of the Authors (28 Aug 2026)  Author's response 
EF by Katja Gänger (31 Aug 2026)
EF by Katja Gänger (31 Aug 2026)  Manuscript   Author's tracked changes 
ED: Publish as is (31 Aug 2026) by Anna Crawford
AR by Florian Hardmeier on behalf of the Authors (10 Sep 2026)  Manuscript 
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Short summary
As mountain glaciers are retreating, they are becoming increasingly debris-covered. We want to better understand how these glaciers respond to a changing climate. Here, we present an improved model that simulates transport of debris within and on the glacier. We find that short-term changes have a low impact due to long response times. However, long-term warming can lead to fast collapse of the glacier tongue after a phase of thinning, where debris cover expands and thickens.
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