Dynamic response of Antarctic Peninsula Ice Sheet to potential collapse of Larsen C and George VI ice shelves

Ice shelf break-up and disintegration events over the past 5 decades have led to speed-up, thinning, and retreat of upstream tributary glaciers and increases to rates of global sea-level rise. The southward progression of these episodes indicates a climatic cause and in turn suggests that the larger...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: C. Schannwell, S. Cornford, D. Pollard, N. E. Barrand
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-12-2307-2018
https://www.the-cryosphere.net/12/2307/2018/tc-12-2307-2018.pdf
https://doaj.org/article/799236950ae74fda89d511dd0e536868