The impact of early Holocene Arctic shelf flooding on climate in an atmosphere–ocean–sea–ice model
Glacial terminations are characterized by a strong rise in sea level related to melting ice sheets. This rise in sea level is not uniform all over the world, because regional effects (uplift and subsidence of coastal zones) are superimposed on global trends. During the early Holocene the Siberian Sh...
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| Autori principali: | , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Copernicus Publications
2013-11-01
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| Serie: | Climate of the Past |
| Accesso online: | http://www.clim-past.net/9/2651/2013/cp-9-2651-2013.pdf |
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