Extended Data Fig. 2: Simulated 40ka temperature and salinity distribution and the Last Glacial Maximum anomalies to this state as zonal averages in the Atlantic sector.
From: A salty deep ocean as a prerequisite for glacial termination

Temperature (°C) and salinity (PSU, white contours) distribution for a) intermediate climate conditions (40kaCTRL). Panels b) and c) show the glacial - 40ka difference (LGMCTRL – 40kaCTRL) for temperature and salinity, respectively. All fields represent 100-year averages.