Articles | Volume 19, issue 10
https://doi.org/10.5194/tc-19-4835-2025
https://doi.org/10.5194/tc-19-4835-2025
Research article
 | 
21 Oct 2025
Research article |  | 21 Oct 2025

Modeling the impacts of climate trends and lake formation on the retreat of a tropical Andean glacier (1962–2020)

Tal Y. Shutkin, Bryan G. Mark, Nathan D. Stansell, Rolando Cruz Encarnación, Henry H. Brecher, Zhengyu Liu, Bidhyananda Yadav, and Forrest S. Schoessow

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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-2024-3194', Ethan Lee & Owen King (co-review team), 13 Mar 2025
    • AC1: 'Reply on RC1', Tal Shutkin, 12 May 2025
  • RC2: 'Comment on egusphere-2024-3194', Catriona Fyffe, 31 Mar 2025
    • AC2: 'Reply on RC2', Tal Shutkin, 25 May 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (18 Jun 2025) by Nicholas Barrand
AR by Tal Shutkin on behalf of the Authors (07 Aug 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (20 Aug 2025) by Nicholas Barrand
AR by Tal Shutkin on behalf of the Authors (20 Aug 2025)
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Short summary
Queshque Glacier of Peru's tropical Andes has retreated rapidly since the mid-20th century. Using a glacier model, we show that this has primarily been driven by steady warming despite the counteracting effect of recent snowfall amounts. Independently from climatic trends, we find that the formation of a new lake at the glacier's base has further accelerated ice loss. This research demonstrates the utility of empirical glacier models for interpreting past and future changes in the tropics.
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