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Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern

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Figure

Table 1. Comparison of the eight models that have performed coupled simulations in the PlioMIP.
Fig. 1. δ13C data in the Atlantic. (a) Site position and depthplotted in a global map
Table 1). The depth of the AMOC cell is highly model-dependent, ranging from 2000 to 4000 m.Compared to the pre-industrial control runs, three mod-
Fig. 4. Comparison of pre-industrial (red) and mid-Pliocene (blue) Atlantic northward ocean heat transport (PW) simulated in the PlioMIP.
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