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
Published in:The Cryosphere
Main Authors: J. Feldmann, A. Levermann
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
Online Access:https://doi.org/10.5194/tc-9-631-2015
https://doaj.org/article/24b80ddd96ce41cd82544be6b9557cae