The anomalous EAWM may lead to the surface heat flux anomalies through air-sea interaction, which then result to the SST anomalies in the SCS and the northwestern Pacific (NWP).

• 结果表明，东亚冬季风异常通过海气相互作用，导致海气之间的热通量异常，进而影响可到南海及西北太平洋的海温异常；