Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma

The geometry of Antarctic ice sheets during warm periods of the geological past is difficult to determine from geological evidence, but is important to know because such reconstructions enable a more complete understanding of how the ice-sheet system responds to changes in climate. Here we investiga...

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Vydáno v:	Climate of the past Ročník 13; číslo 7; s. 959 - 975
Hlavní autoři:	Golledge, Nicholas R., Thomas, Zoë A., Levy, Richard H., Gasson, Edward G. W., Naish, Timothy R., McKay, Robert M., Kowalewski, Douglas E., Fogwill, Christopher J.
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Katlenburg-Lindau Copernicus GmbH 27.07.2017 Copernicus Publications
Témata:	Air temperature Antarctic climate Antarctic ice sheet Atmospheric models Climate Climate change Climate models Computer simulation Flotation Geology Glaciation Global sea level Greenhouse effect Greenhouse gases Ice Ice sheet models Ice sheets Interglacial periods Natural history Ocean temperature open climate campaign Pliocene Pliocene Epoch Precipitation Regional climates Regional variations Sea level Simulation Southern Hemisphere Temperature Topography (geology) Antarctica Prydz Bay
ISSN:	1814-9332, 1814-9324, 1814-9332
On-line přístup:	Získat plný text
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Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma

Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma