Articles | Volume 19, issue 10
https://doi.org/10.5194/tc-19-4355-2025
https://doi.org/10.5194/tc-19-4355-2025
Research article
 | 
07 Oct 2025
Research article |  | 07 Oct 2025

Reinforced ridges in Thwaites Glacier yield insights into resolution requirements for coupled ice sheet and solid Earth models

Luc Houriez, Eric Larour, Lambert Caron, Nicole-Jeanne Schlegel, Surendra Adhikari, Erik Ivins, Tyler Pelle, Hélène Seroussi, Eric Darve, and Martin Fischer

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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-2024-4136', Anonymous Referee #1, 22 Mar 2025
    • AC1: 'Reply on RC1', Luc Houriez, 10 May 2025
  • RC2: 'Comment on egusphere-2024-4136', Jan Swierczek-Jereczek, 27 Mar 2025
    • AC2: 'Reply on RC2', Luc Houriez, 10 May 2025

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 May 2025) by Alexander Robinson
AR by Luc Houriez on behalf of the Authors (30 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (03 Jul 2025) by Alexander Robinson
AR by Luc Houriez on behalf of the Authors (11 Jul 2025)  Manuscript 
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Short summary
This work examines how interactions between the ice sheet and the Earth’s evolving surface affect the future of Thwaites Glacier in Antarctica. We find that small features in the bedrock play a major role in these interactions which can delay the glacier’s retreat by decades or even centuries. This can significantly reduce sea-level rise projections. Our study highlights resolution requirements for similar ice–earth models and the importance of bedrock mapping efforts in Antarctica.
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