Spring North tropical Atlantic (SNTA) sea surface temperature (SST) variability enhances in a warming climate.
Larger SNTA SST variability has greater impacts on East Asian Summer Monsoon (EASM) via Kelvin wave response.
Wetter tropical Pacific in a warming climate also amplifies SNTA SST impact on EASM via Rossby wave response.
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Relationship between SNTA SST and EASM in observations and CMIP6 models
Enhanced influence of SNTA SST on EASM in a warmer climate
Enhanced influence of SNTA SST on East Asian climate in a warmer climate
Increased frequency of SNTA SSTAs followed by anomalous EASM events under greenhouse warming
Enhanced SNTA SST variability in a warmer climate
Mechanisms for enhanced impact of SNTA SST on EASM in a warmer climate
Numerical experiments confirming enhanced impact of SNTA SSTAs on EASM due to increased NTA SST variability and wetter mean state in tropical Pacific