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Glacial climate sensitivity to different states of the Atlantic Meridional Overturning Circulation: results from the IPSL model

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Figure

Fig. 1.Fig. 1.ional Overturning Circulation (in Sv, 1 Sv=10 Time evolution of the maximum of the Atlantic Meridional Overturning Circulation (in Sv,
Fig. 2. Atlantic meridional streamfunction (l.h.s) and maximum mixed layer depth reached overfor LGMa (top), LGMb (middle), LGMc (bottom), years 201–250 for LGMa and b, 521–570 for LGMc
Fig. 3.anomalous (LGMb–LGMa) freshwater budget (in kg/m
Fig. 4. Timeseries of winter mean mixed layer depth (m) averaged over areas of anomalous deep convection (indicated on the maps belowthe time series)
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