Fig. 6: Verifying the role of the ocean thermostat mechanism.
From: Early emergence and determinants of human-induced Walker circulation weakening
a Initial and (b) long-term sea surface temperature (SST) anomaly patterns in the abrupt4×CO2 experiments for Group-L models. c–d The same as (a–b) but for Group-E models. The SST anomalies are derived by comparing them to the piControl experiments and then subtracting the average ocean warming within the 40°S–40°N, 60°E–60°W region. Shown are the ensemble mean. White slant hatchings denote areas where all the models agree in sign.
