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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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Autores principales: J. Barnett, F. A. Holmes, J. Cuzzone, H. Åkesson, M. Morlighem, M. O'Regan, J. Nilsson, N. Kirchner, M. Jakobsson
Formato: Artigo
Lenguaje:Inglês
Publicado: Copernicus Publications 2025-09-01
Colección:The Cryosphere
Acceso en línea:https://tc.copernicus.org/articles/19/3631/2025/tc-19-3631-2025.pdf
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