Fig. 4: Contributions of local SST pattern differences to global-mean climate feedback differences Δλ.
From: Recent global climate feedback controlled by Southern Ocean cooling

a, Green’s function for cloud feedback multiplied by the difference in SST pattern changes between SOPACE and HIST (a) and AMIP and HIST (b). c,d, Similar to a and b, but for total climate feedback. The Green’s function maps are shown in Extended Data Fig. 7. Global sum corresponds to the global-mean climate feedback difference Δλ.