213743.fig.004a
(a) IPSL-CM5A-LR
213743.fig.004b
(b) MIROC-ESM
213743.fig.004c
(c) MPI-ESM-P
213743.fig.004d
(d) MRI-CGCM3
Figure 4: Ocean heat content change (  Jm−2) at the Last Glacial Maximum. Most cooling occurs between 40°S and 40°N. All the four models show cooling in the Atlantic. But, cooling in the Pacific and Indian Oceans varies.