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Rapid, buoyancy-driven ice-sheet retreat of hundreds of metres per day
Rates of ice-sheet grounding-line retreat can be quantified from the spacing of corrugation ridges on deglaciated regions of the seafloor1,2, providing a long-term context for the approximately 50-year satellite record of ice-sheet change3,4,5. However, the few existing examples of these landforms a...
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| Main Authors: | , , , , , , , |
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| Format: | Default Article |
| Published: |
2023
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| Subjects: | |
| Online Access: | https://hdl.handle.net/2134/22561798.v1 |
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