Simulating the Holocene evolution of Ryder Glacier, North Greenland
<p>The Greenland Ice Sheet's negative mass balance is driven by a sensitivity to a warming atmosphere and ocean. The fidelity of ice-sheet models in accounting for ice–ocean interaction is inherently uncertain and often constrained against recent fluctuations in the ice-sheet margin from the previou...
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| Päätekijät: | , , , , , , , , |
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| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Copernicus Publications
2025-09-01
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| Sarja: | The Cryosphere |
| Linkit: | https://tc.copernicus.org/articles/19/3631/2025/tc-19-3631-2025.pdf |
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