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• W1909403247 endingPage "3704" @default.
• W1909403247 startingPage "3698" @default.
• W1909403247 abstract "Abstract Abrupt decadal climate changes during the last glacial‐interglacial cycle are less pronounced during maximum glacial conditions and absent during the Holocene. To further understand the underlying dynamics, we conduct hosing experiments for three climate states: preindustrial (PI), 32 kiloannum before present (ka B.P.), and Last Glacial Maximum (LGM). Our simulations show that a stronger temperature inversion between the surface and intermediate layer in the South Labrador Sea induces a faster restart of convective processes (32 ka B.P. > LGM > PI) during the initial resumption of the Atlantic meridional overturning circulation (AMOC). A few decades later, an AMOC overshoot is mainly linked to the advection of warmer and saltier intermediate‐layer water from the tropical Atlantic into the South Labrador Sea, which causes a stronger deep‐water formation than that before the freshwater perturbation. This mechanism is most pronounced during the 32 ka B.P., weaker during the LGM and absent during the PI." @default.
• W1909403247 created "2016-06-24" @default.
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• W1909403247 date "2013-07-19" @default.
• W1909403247 modified "2023-10-10" @default.
• W1909403247 title "Dependence of abrupt Atlantic meridional ocean circulation changes on climate background states" @default.
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• W1909403247 doi "https://doi.org/10.1002/grl.50701" @default.
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