Projecting Antarctic ice discharge using response functions from SeaRISE ice-sheet models
The largest uncertainty in projections of future sea-level change results from the potentially changing dynamical ice discharge from Antarctica. Basal ice-shelf melting induced by a warming ocean has been identified as a major cause for additional ice flow across the grounding line. Here we attempt...
| Main Authors: | , , , , , , , , , , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2014-08-01
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| Series: | Earth System Dynamics |
| Online Access: | http://www.earth-syst-dynam.net/5/271/2014/esd-5-271-2014.pdf |