Fig. 4: Temperature anomaly (based on simulated potential seawater temperature, MPIOM variable THO) between the PlioMIP2 Pliocene background state of COSMOS and the simulation with added Newtonian salinity restoring mimicking the Mediterranean Overflow Water (MOW). | Communications Earth & Environment

Fig. 4: Temperature anomaly (based on simulated potential seawater temperature, MPIOM variable THO) between the PlioMIP2 Pliocene background state of COSMOS and the simulation with added Newtonian salinity restoring mimicking the Mediterranean Overflow Water (MOW).

From: Mediterranean heat injection to the North Atlantic delayed the intensification of Northern Hemisphere glaciations

Fig. 4

a Intrusion along a meridional transect (30°–55°N; 20°W) and (b) zonal cross-section (10°–45°W; 40°N) of the North Atlantic. Locations of referenced data sets from Sites U1313 and DSDP548 are indicated.

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