Interaction of marine ice-sheet instabilities in two drainage basins: simple scaling of geometry and transition time
The initiation of a marine ice-sheet instability (MISI) is generally discussed from the ocean side of the ice sheet. It has been shown that the reduction in ice-shelf buttressing and softening of the coastal ice can destabilize a marine ice sheet if the bedrock is sloping upward towards the ocean. U...
| Published in: | The Cryosphere |
|---|---|
| Main Authors: | , |
| Format: | Text |
| Language: | English |
| Published: |
2018
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/tc-9-631-2015 https://tc.copernicus.org/articles/9/631/2015/ |