West Antarctic Ice Sheet retreat driven by Holocene warm water incursions

Glaciological and oceanographic observations coupled with numerical models show that warm Circumpolar Deep Water (CDW) upwelling onto the West Antarctic continental shelf causes melting of the undersides of floating ice shelves. Because these ice shelves buttress glaciers feeding into them, their oc...

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Publicado no:Nature
Main Authors: Hillenbrand, Claus-Dieter, Smith, James A., Hodell, David A., Greaves, Mervyn, Poole, Christopher R., Kender, Sev, Williams, Mark, Andersen, Thorbjørn Joest, Jernas, Patrycja E., Elderfield, Henry, Klages, Johann P., Roberts, Stephen J., Gohl, Karsten, Larter, Robert D., Kuhn, Gerhard
Formato: Artigo
Idioma:Inglês
Publicado em: 2017
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Article
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5510715/
https://ncbi.nlm.nih.gov/pubmed/28682333
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/nature22995
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