Modeling Ice Shelf/Ocean Interaction in Antarctica: A Review

The most rapid loss of ice from the Antarctic Ice Sheet is observed where ice streams flow into the ocean and begin to float, forming the great Antarctic ice shelves that surround much of the continent. Because these ice shelves are floating, their thinning does not greatly influence sea level. Howe...

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Bibliographic Details
Main Authors: Dinniman, Michael, Asay-Davis, Xylar, Galton-Fenzi, Benjamin, Holland, Paul, Jenkins, Adrian, Timmermann, Ralph
Format: Article in Journal/Newspaper
Language:English
Published: Rockville, MD : The Oceanography Society 2016
Subjects:
sea
550
Online Access:https://oa.tib.eu/renate/handle/123456789/10004
https://doi.org/10.34657/9042