Fig. 1: Differences in the spatial pattern of SST and estimated inversion strength trends.
From: Recent global climate feedback controlled by Southern Ocean cooling
The pattern of change is calculated by regressing local annual-mean SST (or EIS) against global-mean annual-mean surface air temperature. a,b, Differences in the spatial pattern of SST trends between SOPACE and HIST (a) and AMIP and HIST (b). c,d, Similar to a,b, but for EIS. Regions with a pattern difference significant at the 95% confidence level based on a Student’s t test are stippled.
