Deglaciation and future stability of the Coats Land ice margin, Antarctica
The East Antarctic Ice Sheet discharges into the Weddell Sea via the Coats Land ice margin. We have used geophysical data to determine the changing ice-sheet configuration in this region through its last glacial advance and Holocene retreat and to identify constraints on its future stability. Method...
Published in: | The Cryosphere |
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Main Authors: | , , , , , , , , , , , , , |
Format: | Text |
Language: | English |
Published: |
2019
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-12-2383-2018 https://tc.copernicus.org/articles/12/2383/2018/ |