Research Article

Ocean Cooling Pattern at the Last Glacial Maximum

Figure 5

Ocean heat content change in ocean basins. (a) Average OHC change (  Jm−2) and (b) total OHC change (  J). Cooling in the North Pacific and Southern Ocean differs in magnitude among the four models. SA—South Atlantic, NA—North Atlantic, SP—South Pacific, NP—North Pacific, SI—South Indian, NI—North Indian, South—Southern Ocean, Arc—Arctic.