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...
Published in: | Oceanography |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
ODU Digital Commons
2016
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Subjects: | |
Online Access: | https://digitalcommons.odu.edu/ccpo_pubs/229 https://doi.org/10.5670/oceanog.2016.106 https://digitalcommons.odu.edu/context/ccpo_pubs/article/1231/viewcontent/Dinniman2016ModelingIceShelfOceaninAntarcticaOCR.pdf |