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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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Autori principali: Martin J. Siegert, Neil Ross, Jilu Li, Dustin M. Schroeder, David Rippin, David Ashmore, Robert Bingham, Prasad Gogineni
Natura: Artigo
Lingua:Inglês
Pubblicazione: Cambridge University Press 2016-09-01
Serie:Annals of Glaciology
Soggetti:
basal hydrology
ice dynamics
radio-echo sounding
sediments
Accesso online:https://www.cambridge.org/core/product/identifier/S0260305516000173/type/journal_article
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