Net effect of ice-sheet–atmosphere interactions reduces simulated transient Miocene Antarctic ice-sheet variability

Benthic δ18O levels vary strongly during the warmer-than-modern early and mid-Miocene (23 to 14 Myr ago), suggesting a dynamic Antarctic ice sheet (AIS). So far, however, realistic simulations of the Miocene AIS have been limited to equilibrium states under different CO2 levels and orbital settings....

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Vydané v:	The cryosphere Ročník 16; číslo 4; s. 1315 - 1332
Hlavní autori:	Stap, Lennert B., Berends, Constantijn J., Scherrenberg, Meike D. W., van de Wal, Roderik S. W., Gasson, Edward G. W.
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Katlenburg-Lindau Copernicus GmbH 11.04.2022 European Geosciences Union Copernicus Publications
Predmet:	Albedo Antarctic ice sheet Approximation Atmosphere Bedrock Benthos Carbon dioxide Climate Climate models Cycles Environmental Sciences Equilibrium Experiments Feedback General circulation models Glaciation Ice Ice sheet models Ice sheets Ice shelves Ice volume Interpolation Miocene Negative feedback Ocean temperature Precipitation (Meteorology) Sheet modelling Simulation Topography Variability Water temperature
ISSN:	1994-0424, 1994-0416, 1994-0424, 1994-0416
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