Articles | Volume 19, issue 5
https://doi.org/10.5194/tc-19-1973-2025
https://doi.org/10.5194/tc-19-1973-2025
Research article
 | 
27 May 2025
Research article |  | 27 May 2025

Tracing ice loss from the Late Holocene to the future in eastern Nuussuaq, central western Greenland

Josep Bonsoms, Marc Oliva, Juan Ignacio López-Moreno, and Guillaume Jouvet

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Reviewer Comment on egusphere-2024-1770', Anonymous Referee #1, 13 Nov 2024
  • RC2: 'Comment on egusphere-2024-1770', Adriano Ribolini, 17 Dec 2024

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) (21 Feb 2025) by Florence Colleoni
AR by Josep Bonsoms on behalf of the Authors (26 Feb 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (03 Mar 2025) by Florence Colleoni
AR by Josep Bonsoms on behalf of the Authors (03 Mar 2025)
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Short summary
The extent to which Greenland's peripheral glaciers and ice caps current and future ice loss rates are unprecedented within the Holocene is poorly understood. This study connects the maximum ice extent of the Late Holocene with present and future glacier evolution in the Nuussuaq Peninsula (central western Greenland). By > 2050 glacier mass loss may have doubled in rate compared to the Late Holocene to the present, highlighting significant impacts of anthropogenic climate change.
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