Thwaites Glacier thins and retreats fastest where ice-shelf channels intersect its grounding zone
<p>Antarctic ice shelves buttress the flow of the ice sheet but are vulnerable to increased basal melting from contact with a warming ocean and increased mass loss from calving due to changing flow patterns. Channels and similar features at the bases of ice shelves have been linked to enhanced basal...
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| Autori principali: | , , , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Copernicus Publications
2024-11-01
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| Serie: | The Cryosphere |
| Accesso online: | https://tc.copernicus.org/articles/18/4971/2024/tc-18-4971-2024.pdf |
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