213743.fig.003a
(a) IPSL-CM5A-LR
213743.fig.003b
(b) MIROC-ESM
213743.fig.003c
(c) MPI-ESM-P
213743.fig.003d
(d) MRI-CGCM3
Figure 3: Ocean cooling profiles of global mean and ocean basins. The abscissa is temperature anomaly in °C and the ordinate is water depth in m. The maximum surface warming occurs in the North Atlantic. Ocean cooling mostly concentrates in the upper 1000 m with rapid variations in different basins.