Three positive feedback mechanisms for ice-sheet melting in a warming climate

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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, Diandong, Leslie, L.
Format:	Journal Article
Published:	International Glaciological Society 2011
Online Access:	http://hdl.handle.net/20.500.11937/35335

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