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Gao Shiying,Wang Jingshu. 1988. El Nino and the Southern Oscillation. Acta Oceanologica Sinica, (4):521-532
El Nino and the Southern Oscillation
El Nino and the Southern Oscillation
Received:June 13, 1987  Revised:November 10, 1987
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Author NameAffiliation
Gao Shiying National Research Center for Marine Environment Forecasts, Beijing, China 
Wang Jingshu National Research Center for Marine Environment Forecasts, Beijing, China 
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Abstract:
      Using the Comprehensive Ocean-Atmosphere Data Set (COADS), wind, surface pressure and SST fields in the Equatorial Eastern Pacific and the Equatorial South Indian Ocean were analysed comprehensively.lt is pointed out that the seesaw between surface pressure in the Equatorial South Indian Ocean and the Equatorial Southeast Pacific causes the seesaw between the wind fields in the two areas, and the seesaw of wind fields results in the seesaw of SST between Indonesia and the Equatorial Eastern Pacific.El Nino is the response of ocean to the forcing of monsoon system in the Indian Ocean and the trade system in the Pacific.
中文摘要:
      Using the Comprehensive Ocean-Atmosphere Data Set (COADS), wind, surface pressure and SST fields in the Equatorial Eastern Pacific and the Equatorial South Indian Ocean were analysed comprehensively.lt is pointed out that the seesaw between surface pressure in the Equatorial South Indian Ocean and the Equatorial Southeast Pacific causes the seesaw between the wind fields in the two areas, and the seesaw of wind fields results in the seesaw of SST between Indonesia and the Equatorial Eastern Pacific.El Nino is the response of ocean to the forcing of monsoon system in the Indian Ocean and the trade system in the Pacific.
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