Subglacial controls on the flow of Institute Ice Stream, West Antarctica

The Institute Ice Stream (IIS) rests on a reverse-sloping bed, extending >150 km upstream into the ~1.8 km deep Robin Subglacial Basin, placing it at the threshold of marine ice-sheet instability. Understanding IIS vulnerability has focused on the effect of grounding-line melting, which is foreca...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Martin J. Siegert, Neil Ross, Jilu Li, Dustin M. Schroeder, David Rippin, David Ashmore, Robert Bingham, Prasad Gogineni
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2016
Subjects:
Online Access:https://doi.org/10.1017/aog.2016.17
https://doaj.org/article/7dbc6844a4f7469ebca80aee109e6e60