Spatio-temporal melt and basal channel evolution on Pine Island Glacier ice shelf from CryoSat-2
<p>Ice shelves buttress the grounded ice sheet, restraining its flow into the ocean. Mass loss from these ice shelves occurs primarily through ocean-induced basal melting, with the highest melt rates occurring in regions that host basal channels – elongated, kilometre-wide zones of relatively thin i...
में बचाया:
| मुख्य लेखकों: | , , , , , |
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| स्वरूप: | Artigo |
| भाषा: | Inglês |
| प्रकाशित: |
Copernicus Publications
2025-10-01
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| श्रृंखला: | The Cryosphere |
| ऑनलाइन पहुंच: | https://tc.copernicus.org/articles/19/4893/2025/tc-19-4893-2025.pdf |
| टैग: |
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