Combined impact of tropical central‐eastern Pacific and North Atlantic sea surface temperature on precipitation variation in monsoon transitional zone over China during August–September

• Published in: International Journal of Climatology
• Main Authors: Zhao, Wei, Chen, Wen, Chen, Shangfeng, Yao, Shuai‐Lei, Nath, Debashis
• Other Authors: National Basic Research Program of China, National Natural Science Foundation of China, China Association for Science and Technology
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2019
• Subjects: North Atlantic
• Online Access: http://dx.doi.org/10.1002/joc.6231; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.6231; https://onlinelibrary.wiley.com/doi/pdf/10.1002/joc.6231; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/joc.6231; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.6231

Abstract Previous studies suggested that sea surface temperature (SST) anomalies in the tropical central‐eastern Pacific (TCEP) and tropical Northern Atlantic (TNA) both have significant impacts on the inter‐annual variation of precipitation over the monsoon transitional zone (MTZ) in China during August–September. This study further reveals that the relationship between TCEP (TNA) SST and MTZ precipitation during August–September is strongly modulated by the sign of the TNA (TCEP) SST. When TCEP and TNA SST anomalies have the same sign, connections of the TCEP and TNA SST with the MTZ precipitation are unclear. In contrast, TCEP and TNA SST changes both have significant relation with the MTZ precipitation when they have the opposite sign. During the same‐sign years, the anticyclonic (cyclonic) anomaly over the western North Pacific generated by the TCEP SST cooling (warming) is weakened by the cyclonic (anticyclonic) anomaly triggered by the TNA SST cooling (warming). Thus, connections of the MTZ precipitation with the TCEP and TNA SST are weak. However, during the opposite‐sign years, the anticyclonic anomalies over the western North Pacific generated by the TCEP SST anomalies have a constructive superposition on those induced by the TNA SST changes. As such, connections of the TCEP and TNA SST with the MTZ precipitation variation are significant. Further analysis shows that the prediction skill of precipitation over the MTZ is enhanced if taking both the TCEP and TNA SST signals into account.