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Abrupt North Atlantic circulation changes in response to gradual CO2 forcing in a glacial climate state
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Abstract
During glacial climates, the strength of the Atlantic overturning circulation has
changed abruptly. Climate model simulations show that gradual changes in atmospheric
CO2 levels can trigger such events via atmospheric moisture transport.
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Most cited references38
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A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates
G Randall Bond (1997)
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A Dynamic Thermodynamic Sea Ice Model
W. D. Hibler (1979)
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Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint
Sidney R Hemming (2004)