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) incursions onto the West Antarctic continental shelf cause 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
Main Authors: C. D. Hillenbrand, J. A. Smith, D. A. Hodell, M Greaves, C. R. Poole, S Kender, Mark Williams, P. E. Jernas, H Elderfield, J. P. Klages, S. J. Roberts, K Gohl, R. D. Larter, G Kuhn
Format: Other Non-Article Part of Journal/Newspaper
Language:unknown
Published: 2017
Subjects:
Online Access:https://figshare.com/articles/journal_contribution/West_Antarctic_Ice_Sheet_retreat_driven_by_Holocene_warm_water_incursions/10216049