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...
Main Authors: | , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
München : European Geopyhsical Union
2015
|
Subjects: | |
Online Access: | https://dx.doi.org/10.34657/1037 https://oa.tib.eu/renate/handle/123456789/684 |