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Variations of the Atlantic meridional overturning circulation in control and transient simulations of the last millennium

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Table 1. List of all experiments. Note that the length for the CTRL1500 and the CTRL1000 simulation also includes the 50 yrs that werenot used in the analysis.
Fig. 1. Forcing from 1000 to 2000 A.D.: (a) the total radiative forc-ing due to solar irradiance and GHGs; (b) the optical depth changesin the visible band due to volcanic aerosols
Fig. 2.Annual mean northern hemisphere SAT anomaly fromand the HadCRUT3v data since 1860
Fig. 4.Low-pass filtered time series of the AMOC index. Thetime series of the control integrations show the anomaly from theirmean, while the time series of the transient simulations are calcu-lated as the anomaly from the mean of the initializing control e
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