Destabilization of glacial climate by the radiative impact of Atlantic Meridional Overturning Circulation disruptions

During each of the dramatic global warmings that ended the Pleistocene ice ages, the Atlantic Meridional Overturning Circulation (AMOC) was disrupted. It is not clear whether this was a contributing cause or simply an effect of deglaciation. Here we show that in an ensemble of simulations with a glo...

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Veröffentlicht in:	Geophysical research letters 2016-08, Vol.43 (15), p.8214-8221
Hauptverfasser:	Galbraith, Eric D., Merlis, Timothy M., Palter, Jaime B.
Format:	Artikel
Sprache:	eng
Schlagworte:	Accumulation Atlantic Meridional Overturning Circulation (AMOC) bipolar seesaw Carbon dioxide Circulation Climate climate model Climate models Computer simulation Convection Deglaciation Destabilization Disruption Dynamics Geophysics Glacial climates Glaciation Global climate Heat Ice Ice ages Ice sheet dynamics Instability Marine Mathematical models Meltwater ocean circulation Pleistocene radiative balance
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