Genesis of westerly wind bursts over the equatorial western Pacific during the onset of the strong 2015–2016 El Niño

• Published in: Atmospheric Science Letters
• Main Authors: Chen, Shangfeng, Wu, Renguang, Chen, Wen, Yu, Bin, Cao, Xi
• Other Authors: China Postdoctoral Science Foundation, National Natural Science Foundation of China
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2016
• Subjects: Arctic; Pacific
• Online Access: http://dx.doi.org/10.1002/asl.669; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fasl.669; https://onlinelibrary.wiley.com/doi/pdf/10.1002/asl.669; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/asl.669; https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/asl.669

Abstract The strong 2015–2016 El Niño was initiated by several strong westerly wind bursts over the equatorial western Pacific in March and May 2015. These westerly wind bursts trigger eastward propagating warm Kelvin waves and lead to large sea surface temperature ( SST ) warming in the equatorial eastern Pacific. The first burst of westerly winds in early March was mainly induced by the Arctic Oscillation ( AO ) event. These westerly wind anomalies were enhanced subsequently due to the Madden‐Julian Oscillation activity and northerly cold surges from East Asia‐western Pacific in mid‐March. Another westerly wind burst in May, induced by anomalous southerly winds from the Australian continent, further increased the SST anomaly in the equatorial eastern Pacific. This study provides an evidence of the AO influence on this strong El Niño‐Southern Oscillation ( ENSO ) event and demonstrates the complexity in the genesis of westerly wind bursts during the El Niño outbreak, which may help improve the prediction of ENSO .