Ice-sheet response to oceanic forcing

The ice sheets of Greenland and Antarctica are losing ice at accelerating rates, much of which is a response to oceanic forcing, especially of the floating ice shelves. Recent observations establish a clear correspondence between the increased delivery of oceanic heat to the ice-sheet margin and inc...

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Vydané v:	Science (American Association for the Advancement of Science) Ročník 338; číslo 6111; s. 1172
Hlavní autori:	Joughin, Ian, Alley, Richard B, Holland, David M
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	United States 30.11.2012
Predmet:	Antarctic Regions Atmosphere Global Warming Greenland Ice Cover Oceans and Seas Tidal Waves Transition Temperature Antarctic Regions Greenland
ISSN:	1095-9203, 1095-9203
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