Large and irreversible future decline of the Greenland ice sheet
<p>We have studied the evolution of the Greenland ice sheet under a range of constant climates typical of those projected for the end of the present century using a dynamical ice sheet model (Glimmer) coupled to an atmosphere general circulation model (FAMOUS–ice AGCM). The ice sheet surface mass ba...
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| Main Authors: | , , |
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| Format: | Artigo |
| Language: | Inglês |
| Published: |
Copernicus Publications
2020-12-01
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| Series: | The Cryosphere |
| Subjects: | |
| Online Access: | https://tc.copernicus.org/articles/14/4299/2020/tc-14-4299-2020.pdf |
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