Three positive feedback mechanisms for ice-sheet melting in a warming climate
Three positive feedback mechanisms that accelerate ice-sheet melting are assessed in a warming climate, using a numerical ice model driven by atmospheric climate models. The Greenland ice sheet (GrIS) is the modeling test-bed under accelerated melting conditions. The first feedback is the interactio...
| Main Authors: | , |
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| Format: | Journal Article |
| Published: |
International Glaciological Society
2011
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| Online Access: | http://hdl.handle.net/20.500.11937/35335 |