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: | Article in Journal/Newspaper |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://hdl.handle.net/1983/4332c956-538e-48ed-829e-84398490ea13 https://research-information.bris.ac.uk/en/publications/4332c956-538e-48ed-829e-84398490ea13 https://doi.org/10.5194/tc-12-2307-2018 https://research-information.bris.ac.uk/ws/files/167362284/tc_12_2307_2018.pdf http://www.scopus.com/inward/record.url?scp=85050468215&partnerID=8YFLogxK |