Greenland ice sheet response to transient climate change: Consensus between two CGCMs
Possible accelerated melting of the Greenland ice sheet in the 21st century has profound implications for sea-level rise and for climate change feedback. This study quantifies the potential melting of the Greenland ice sheet under a realistic 21st century greenhouse gas emission scenario. T...
| Main Authors: | , , |
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| Format: | Journal Article |
| Published: |
Copernicus GmbH
2008
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| Online Access: | http://meetings.copernicus.org/www.cosis.net/abstracts/EGU2008/12412/EGU2008-A-12412.pdf http://hdl.handle.net/20.500.11937/4210 |