Deglacial evolution of regional Antarctic climate and Southern Ocean conditions in transient climate simulations

Constraining Antarctica's climate evolution since the end of the Last Glacial Maximum (∼18 ka) remains a key challenge, but is important for accurately projecting future changes in Antarctic ice sheet mass balance. Here we perform a spatial and temporal analysis of two transient deglacial clima...

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Veröffentlicht in:	Climate of the past Jg. 15; H. 1; S. 189 - 215
Hauptverfasser:	Lowry, Daniel P., Golledge, Nicholas R., Menviel, Laurie, Bertler, Nancy A. N.
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	Katlenburg-Lindau Copernicus GmbH 30.01.2019 Copernicus Publications
Schlagworte:	Accumulation Air temperature Albedo Albedo (solar) Analysis Antarctic climate Antarctic ice sheet Climate Climate change Climate models Climatic evolution Coastal zone Computer simulation Continental margins Duration Evolution Glaciation Holocene Ice Ice cover Ice sheet models Last Glacial Maximum Mass balance Mass balance of ice sheets Meltwater Ocean circulation Ocean currents Ocean models Ocean temperature Oceans Paleoclimatology Regions Scaling Sea ice Spatial analysis Surface temperature Surface-air temperature relationships Temperature Temperature effects Water circulation Younger Dryas Antarctica Southern Ocean
ISSN:	1814-9332, 1814-9324, 1814-9332
Online-Zugang:	Volltext
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