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...

Täydet tiedot

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Bibliografiset tiedot
Julkaisussa:Nature
Päätekijät: 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
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: 2017
Aiheet:
Article
Linkit: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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