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...
Published in: | The Cryosphere |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
2019
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-12-2307-2018 https://tc.copernicus.org/articles/12/2307/2018/ |