Evidence of marine ice-cliff instability in Pine Island Bay from iceberg-keel plough marks.

Marine ice-cliff instability (MICI) processes could accelerate future retreat of the Antarctic Ice Sheet if ice shelves that buttress grounding lines more than 800 metres below sea level are lost. The present-day grounding zones of the Pine Island and Thwaites glaciers in West Antarctica need to ret...

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Bibliographic Details
Main Authors: Wise, Matthew G, Dowdeswell, Julian A, Jakobsson, Martin, Larter, Robert D
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2017
Subjects:
Online Access:https://www.repository.cam.ac.uk/handle/1810/275729
https://doi.org/10.17863/CAM.22993