Ocean access beneath the southwest tributary of Pine Island Glacier, West Antarctica

The catchments of Pine Island Glacier and Thwaites Glacier in the Amundsen Sea Embayment are two of the largest, most rapidly changing, and potentially unstable sectors of the West Antarctic Ice Sheet. They are also neighboring outlets, separated by the topographically unconfined eastern shear margi...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Dustin M. Schroeder, Andrew M. Hilger, John D. Paden, Duncan A. Young, Hugh F. J. Corr
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2018
Subjects:
Online Access:https://doi.org/10.1017/aog.2017.45
https://doaj.org/article/7f50ce51262d47e89164a4b8944ccb95