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Hu Zeyong,Tang Maocang. 1993. East-west oscillation of sea temperature in the Equatorial Pacific and its modelling. Acta Oceanologica Sinica, (2):207-218
East-west oscillation of sea temperature in the Equatorial Pacific and its modelling
East-west oscillation of sea temperature in the Equatorial Pacific and its modelling
Received:March 18, 1991  Revised:August 25, 1992
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Author NameAffiliation
Hu Zeyong Lanzhou Institute of Plateau Atmospheric physics, Academia Sinica, Lanzhou 730000, China 
Tang Maocang Lanzhou Institute of Plateau Atmospheric physics, Academia Sinica, Lanzhou 730000, China 
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Abstract:
      In this paper, by analyzing the data of sea temperature in the Equatorial Western Pacific (EWP), we found that the sea temperature at sensitive district (WSST) (about at 6°N, depth of 125-150 m) is correlated negatively to the sea temperature in the Equatorial Eastern Pacific (EEP). On the basis of basic characteristics of Equatorial Pacific atmosphere and ocean, we designed a simple air-sea coupled model. Using this model,an ocean circulation was simulated. The east-west oscillation of sea temperature in Equatorial Pacific is related to this ocean circulation.
中文摘要:
      In this paper, by analyzing the data of sea temperature in the Equatorial Western Pacific (EWP), we found that the sea temperature at sensitive district (WSST) (about at 6°N, depth of 125-150 m) is correlated negatively to the sea temperature in the Equatorial Eastern Pacific (EEP). On the basis of basic characteristics of Equatorial Pacific atmosphere and ocean, we designed a simple air-sea coupled model. Using this model,an ocean circulation was simulated. The east-west oscillation of sea temperature in Equatorial Pacific is related to this ocean circulation.
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