Impact of glacial isostatic adjustment on zones of potential grounding line persistence in the Ross Sea Embayment (Antarctica) since the Last Glacial Maximum
<p>Ice streams in the Ross Sea Embayment (West Antarctica) retreated up to 1000 km since the Last Glacial Maximum (LGM). One way that bathymetry influenced this retreat was through the presence of local bathymetric highs, or pinning points, which decreased ice flux through the grounding line a...
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| Main Authors: | S. T. Kodama, T. Pico, A. A. Robel, J. E. Christian, N. Gomez, C. Vigilia, E. Powell, J. Gagliardi, S. Tulaczyk, T. Blackburn |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-08-01
|
| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/19/2935/2025/tc-19-2935-2025.pdf |
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