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Numerical simulation of the upper ocean currents in South China Sea
作者姓名:Li Rongfeng  Huang Qizhou  Wang Wenzhi
作者单位:Li Rongfeng; Huang Qizhou and Wang Wenzhi(Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100080. China)(South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 510301,China)
基金项目:This study was supported by the National Natural Foundation of China under contract No. 48970268.
摘    要:NumericalsimulationoftheupperoceancurrentsinSouthChinaSea¥LiRongfeng;HuangQizhouandWangWenzhi(InstituteofAtmosphericPhysics,C...

关 键 词:Upper  ocean  current  numerical  simulation  SCS  warm  current  the  SCS  branch  of  Kuroshio  slope  of  sealevel
收稿时间:1995/1/10 0:00:00
修稿时间:3/5/1995 12:00:00 AM

Numerical simulation of the upper ocean currents in South China Sea
Li Rongfeng,Huang Qizhou,Wang Wenzhi.Numerical simulation of the upper ocean currents in South China Sea[J].Acta Oceanologica Sinica,1995,14(3):306-317.
Authors:Li Rongfeng  Huang Qizhou and Wang Wenzhi
Institution:1.Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100080, China2.South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
Abstract:The upper ocean currents in the Pacific Ocean are calculated by using an ocean model with higher horizontal resolution. The large current systems in the Pacific Ocean, such as Kuroshio, Oyashio, NEC, SEC, NECC,Califomia Current and East Australia Current, are well simulated. This paper only gives the numerical simulation results of the upper ocean currents of the representative months in four seasons in the South China Sea (SCS). It showsthat the SCS branch of Kuroshio is the most important current in the northem SCS and it is not only the water resourceof the SCS warm current but also a significant part of the overall SCS circulation. There is a relatively strong northeastward flow entering the SCS through the Taiwan Strait throughout the year except for specific months. Some of thenumerical results have been confirmed by the observational evidences.
Keywords:Upper ocean current  numerical simulation  SCS warm current  the SCS branch of Kuroshio  slope of sealevel
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