The role of history and strength of the oceanic forcing in sea level projections from Antarctica with the Parallel Ice Sheet Model
<p>Mass loss from the Antarctic Ice Sheet constitutes the largest uncertainty in projections of future sea level rise. Ocean-driven melting underneath the floating ice shelves and subsequent acceleration of the inland ice streams are the major reasons for currently observed mass loss from Antarctica...
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| Autors principals: | , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Copernicus Publications
2020-09-01
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| Col·lecció: | The Cryosphere |
| Matèries: | |
| Accés en línia: | https://tc.copernicus.org/articles/14/3097/2020/tc-14-3097-2020.pdf |
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