Ice Stream Slowdown Will Drive Long-Term Thinning of the Ross Ice Shelf, With or Without Ocean Warming
Author:
Affiliation:
1. School of Surveying; University of Otago; Dunedin New Zealand
2. Division of Polar Earth-System Sciences; Korea Polar Research Institute; Incheon South Korea
Funder
NZARI
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017GL075794/fullpdf
Reference16 articles.
1. Variable deceleration of Whillans Ice Stream, West Antarctica;Beem;Journal of Geophysical Research: Earth Surface,2014
2. The shape of change: An EOF approach to identifying sources of transient thickness change in an ice shelf;Campbell;Annals of Glaciology,2017
3. Variability in the mass flux of the Ross ice streams, West Antarctica, over the last millennium;Catania;Journal of Glaciology,2012
4. The response of ice shelf basal melting to variations in ocean temperature;Holland;Journal of Climate,2008
5. Century-scale discharge stagnation and reactivation of the Ross ice streams, West Antarctica;Hulbe;Journal of Geophysical Research,2007
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