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...

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Bibliographic Details
Main Authors: Feldmann, J., Levermann, A.
Format: Article in Journal/Newspaper
Language:English
Published: München : European Geopyhsical Union 2015
Subjects:
550
Online Access:https://doi.org/10.34657/1037
https://oa.tib.eu/renate/handle/123456789/684