Rapid sea-level rise along the Antarctic margins in response to increased glacial discharge
The Antarctic shelf seas are a climatically and ecologically important region, and are at present receiving increasing amounts of freshwater from the melting of the Antarctic Ice Sheet and its fringing ice shelves1, 2, primarily around the Antarctic Peninsula and the Amundsen Sea. In response, the s...
| Main Authors: | , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
2014-10.
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| Subjects: | |
| Online Access: | Get fulltext Get fulltext |