A deep subglacial embayment adjacent to the grounding line of Institute Ice Stream, West Antarctica
The Institute Ice Stream (IIS) in West Antarctica may be increasingly vulnerable to melting at the grounding line through modifications in ocean circulation. Understanding such change requires knowledge of grounding-line boundary conditions, including the topography on which it rests. Here, we discu...
Published in: | Geological Society, London, Special Publications |
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Main Authors: | , , , , , |
Other Authors: | , , |
Format: | Book Part |
Language: | unknown |
Published: |
Geological Society of London
2017
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/517226/ https://doi.org/10.1144/SP461.11 |