Dynamics of the last glacial maximum Antarctic ice-sheet and its response to ocean forcing

Retreat of the Last Glacial Maximum (LGM) Antarctic ice sheet is thought to have been initiated by changes in ocean heat and eustatic sea level propagated from the Northern Hemisphere (NH) as northern ice sheets melted under rising atmospheric temperatures. The extent to which spatial variability in...

Celý popis

Podrobná bibliografia

Vydané v:	Proceedings of the National Academy of Sciences - PNAS Ročník 109; číslo 40; s. 16052
Hlavní autori:	Golledge, Nicholas R, Fogwill, Christopher J, Mackintosh, Andrew N, Buckley, Kevin M
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	United States 02.10.2012
Predmet:	Antarctic Regions Computer Simulation Global Warming History, Ancient Ice Cover - chemistry Models, Theoretical Oceans and Seas Water Movements Antarctic Regions
ISSN:	1091-6490, 1091-6490
On-line prístup:	Zistit podrobnosti o prístupe
Tagy:	Pridať tag Žiadne tagy, Buďte prvý, kto otaguje tento záznam!