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EL NINO AND THE ANOMALOUS CLIMATE IN CHINA
作者姓名:Zhao Hanguang  Zhang Xiangong  Ding Yihui
作者单位:National Meteorological Center State Meteorological Administration,Beijing,Academy of Meteorological Science,State Meteorological Administration,Beijing,Academy of Meteorological Science,State Meteorological Administration,Beijing
摘    要:The similar features of two El Nino(1982/83 and 1986/88)events in the formation and developmentprocess are revealed based on the analysis of the oceanic and atmospheric data in the present paper Forinstance,the timing of the warming onset and ending was late,the warming region first took place in theequatorial central Pacific,and the propagation of warming event is from west to east.Moreover,it is shownthat the two El Nino events both exerted a significant impact to the strength and the westward extension ofthe subtropical high over the Northwest Pacific.The atmospheric response to this SST anomaly was alsovery marked with the persistent PNA pattern observed in Pacific-North American region.Both events hadthe striking impact on the winter weather process and climate in China,but with considerable differences.On the basis of the analysis of all El Nino events in the recent 40 years,it has been found that the rainfallduring Meiyu period in Changjiang River Basin is associated with the season of El Nino onset.

收稿时间:3/3/1988 12:00:00 AM

EL NINO AND THE ANOMALOUS CLIMATE IN CHINA
Zhao Hanguang,Zhang Xiangong,Ding Yihui.EL NINO AND THE ANOMALOUS CLIMATE IN CHINA[J].Acta Meteorologica Sinica,1989,3(4):471-481.
Authors:Zhao Hanguang  Zhang Xiangong and Ding Yihui
Institution:National Meteorological Center, State Meteorological Administration, Beijing;Academy of Meteorological Science, State Meteorological Administration, Beijing;Academy of Meteorological Science, State Meteorological Administration, Beijing
Abstract:The similar features of two El Nino (1982/83 and 1986/88) events in the formation and development process are revealed based on the analysis of the oceanic and atmospheric data in the present paper For instance,the timing of the warming onset and ending was late,the warming region first took place in the equatorial central Pacific,and the propagation of warming event is from west to east.Moreover,it is shown that the two El Nino events both exerted a significant impact to the strength and the westward extension of the subtropical high over the Northwest Pacific.The atmospheric response to this SST anomaly was also very marked with the persistent PNA pattern observed in Pacific-North American region.Both events had the striking impact on the winter weather process and climate in China,but with considerable differences.On the basis of the analysis of all El Nino events in the recent 40 years,it has been found that the rainfall during Meiyu period in Changjiang River Basin is associated with the season of El Nino onset.
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