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...
Gorde:
| Egile Nagusiak: | , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
Copernicus Publications
2015-04-01
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| Saila: | The Cryosphere |
| Sarrera elektronikoa: | http://www.the-cryosphere.net/9/631/2015/tc-9-631-2015.pdf |
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