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 forecast...
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| Hauptverfasser: | , , , , , , , |
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| Format: | Artigo |
| Sprache: | Inglês |
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Cambridge University Press
2016-09-01
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| Schriftenreihe: | Annals of Glaciology |
| Schlagworte: | |
| Online-Zugang: | https://www.cambridge.org/core/product/identifier/S0260305516000173/type/journal_article |
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