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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Latest update: 07 Oct 2025
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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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