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Gao Shiying,Wang Jinshu. 1989. The strong winter monsoon in East Asia and El Nino. Acta Oceanologica Sinica, (2):217-221
The strong winter monsoon in East Asia and El Nino
The strong winter monsoon in East Asia and El Nino
Received:July 12, 1987  Revised:December 10, 1987
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Author NameAffiliation
Gao Shiying National Research Center for Marine Environment Forecasts, State Oceanic Administration Beijing, China 
Wang Jinshu National Research Center for Marine Environment Forecasts, State Oceanic Administration Beijing, China 
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Abstract:
      The relationship between meridional wind in mid-latitudes of East Asia and SST in the Equatorial Eastern Pacific is analysed in this paper. It is pointed out that there exist close relations between the seasonal changes of the meridional wind in mid-latitudes of East Asia and SST in the Equatorial Eastern Pacific. The intensification of north winds over East Asia also plays an important role in the rise of SST in Equatorial Eastern Pacific one year later. The strong winter monsoon usually occurs in previous winter of El Nino and it causes low temperature to a great extent in China. The low temperature in China can be regarded as a precursor of El Nino.
中文摘要:
      The relationship between meridional wind in mid-latitudes of East Asia and SST in the Equatorial Eastern Pacific is analysed in this paper. It is pointed out that there exist close relations between the seasonal changes of the meridional wind in mid-latitudes of East Asia and SST in the Equatorial Eastern Pacific. The intensification of north winds over East Asia also plays an important role in the rise of SST in Equatorial Eastern Pacific one year later. The strong winter monsoon usually occurs in previous winter of El Nino and it causes low temperature to a great extent in China. The low temperature in China can be regarded as a precursor of El Nino.
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