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...
Published in: | Nature |
---|---|
Main Authors: | , , , , , , , , , , , , , , |
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 |