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...
Published in: | Annals of Glaciology |
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Main Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press
2016
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Subjects: | |
Online Access: | https://doi.org/10.1017/aog.2016.17 https://doaj.org/article/7dbc6844a4f7469ebca80aee109e6e60 |