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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Bibliographic Details
Published in: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
Format: Text
Language:English
Published: 2017
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5510715/
http://www.ncbi.nlm.nih.gov/pubmed/28682333
https://doi.org/10.1038/nature22995