Articles | Volume 19, issue 9
https://doi.org/10.5194/tc-19-3655-2025
https://doi.org/10.5194/tc-19-3655-2025
Research article
 | 
10 Sep 2025
Research article |  | 10 Sep 2025

Ongoing firn warming at Eclipse Icefield, Yukon, indicates potential widespread meltwater percolation and retention in firn pack across the St. Elias Range

Ingalise Kindstedt, Dominic Winski, C. Max Stevens, Emma Skelton, Luke Copland, Karl Kreutz, Mikaila Mannello, Renée Clavette, Jacob Holmes, Mary Albert, and Scott N. Williamson

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Review of Kindstedt et. al.', Anonymous Referee #1, 12 Feb 2025
    • AC1: 'Reply on RC1', Ingalise Kindstedt, 29 Mar 2025
  • RC2: 'Comment on egusphere-2024-3807', Anonymous Referee #2, 18 Feb 2025
    • AC2: 'Reply on RC2', Ingalise Kindstedt, 29 Mar 2025
  • EC1: 'Editor's recommendation', Florent Dominé, 04 Mar 2025

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) (01 Apr 2025) by Florent Dominé
AR by Ingalise Kindstedt on behalf of the Authors (04 Apr 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (04 Apr 2025) by Florent Dominé
RR by Anonymous Referee #2 (27 Apr 2025)
RR by Anonymous Referee #1 (28 Apr 2025)
ED: Publish subject to minor revisions (review by editor) (02 May 2025) by Florent Dominé
AR by Ingalise Kindstedt on behalf of the Authors (12 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (21 May 2025) by Florent Dominé
AR by Ingalise Kindstedt on behalf of the Authors (22 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (28 May 2025) by Florent Dominé
AR by Ingalise Kindstedt on behalf of the Authors (28 May 2025)  Manuscript 
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Short summary
Atmospheric warming over mountain glaciers is leading to increased warming and melting of snow as it compresses into glacier ice. This affects both regional hydrology and climate records contained in the ice. Here we use field observations and modeling to show that surface melting and percolation at Eclipse Icefield (Yukon, Canada) are increasing with an increase in extreme melt events and that compressing snow at Eclipse is likely to continue warming even if air temperatures remain stable.
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