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...

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Bibliographic Details
Main Authors: Ren, D, Leslie, LM
Format: Article in Journal/Newspaper
Language:unknown
Published: 2011
Subjects:
Online Access:http://hdl.handle.net/10453/118394