An extended variable-grid global ocean circulation model and its preliminary results of the equatorial Pacific circulation  

作　　者：FANGGuohong WEIZexun WANGYonggang CHENHaiying WANGXinyi 

机构地区：[1]KeyLaboratoryofMarineScienceandNumericalModelling,FirstInstituteofOceanography,StateOceanicAdministration,Qingdao266061,China [2]InstituteofOceanology,ChineseAcademyofSciences,Qingdao266071,China [3]GraduateSchoolofChineseAcademyofSciences,Beijing100039,China

出　　处：《Acta Oceanologica Sinica》2004年第1期23-29,共7页海洋学报（英文版）

基　　金：This study is supported by the National Natural Sci-ence Foundation of China under contract No.40136010;the Major State Basic Research Program of China under contract No.G1999043808;the Youth Fund of National“863”Project of China under contract No.2002AA639350.

摘　　要：To investigate the interaction between the tropical Pacific and China seas a variable-grid global ocean circulation model with fine grid covering the area from 20°S to 50°N and from 99° to 150°E is developed. Numerical computation of the annually cyclic circulation fields is performed. The results of the annual mean zonal currents and deep to abyssal western boundary currents in the equatorial Pacific Ocean are reported. The North Equatorial Current,the North Equatorial Countercurrent, the South Equatorial Current and the Equatorial Undercurrent are fairly well simulated. The model well reproduces the northward flowing abyssal western boundary current.From the model results a lower deep western boundary current east of the Bismarck-Solomon-New Hebrides Island chain at depths around 2 000 m has been found. The model results also show that the currents in the equatorial Pacific Ocean have multi-layer structures both in zonal currents and western boundary currents, indicating that the global ocean overturning thermohaline circulation appears of multi-layer pattern.To investigate the interaction between the tropical Pacific and China seas a variable-grid global ocean circulation model with fine grid covering the area from 20°S to 50°N and from 99° to 150°E is developed. Numerical computation of the annually cyclic circulation fields is performed. The results of the annual mean zonal currents and deep to abyssal western boundary currents in the equatorial Pacific Ocean are reported. The North Equatorial Current,the North Equatorial Countercurrent, the South Equatorial Current and the Equatorial Undercurrent are fairly well simulated. The model well reproduces the northward flowing abyssal western boundary current.From the model results a lower deep western boundary current east of the Bismarck-Solomon-New Hebrides Island chain at depths around 2 000 m has been found. The model results also show that the currents in the equatorial Pacific Ocean have multi-layer structures both in zonal currents and western boundary currents, indicating that the global ocean overturning thermohaline circulation appears of multi-layer pattern.

关 键 词：global ocean circulation model variable grid equatorial Pacific zonal currents lower deep western boundary current abyssal western boundary current 

分 类 号：P721[天文地球—海洋科学] P731.21