In this study, we performed ‘pacemaker’ simulations by restoring the satellite era tropical SST changes over the Atlantic, the Indian Ocean, and the Pacific, respectively, in a fully coupled model – the CESM1. Results reveal that the Atlantic warming heats the Indo-Western Pacific and cools the Eastern Pacific, enhances the Walker circulation and drives the subsurface Pacific to a La Niña mode, On the other hand, The Indian Ocean warming also contribute to the La Nina type changes over the Pacific, while the Pacific changes cools the Indian Ocean and the north tropical Atlantic slightly. The east Pacific cooling and the west Pacific warming play different roles in changing the status over the Indian Ocean and the Atlantic, which requests further investigation.