| NUMERICAL STUDY ON THE FORMATION OF THE SOUTH CHINA SEA WARM CURRENT Ⅰ.BAROTROPIC CASE |
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| 引用本文： | 王凯 方越. NUMERICAL STUDY ON THE FORMATION OF THE SOUTH CHINA SEA WARM CURRENT Ⅰ.BAROTROPIC CASE[J]. 中国海洋湖沼学报, 2001, 19(1): 1-9. DOI: 10.1007/BF02842783 |
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| 作者姓名： | 王凯 方越 |
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| 作者单位： | InstituteofOceanology,ChineseAcademyofSciences,Qingdao266071,China） |
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| 基金项目： | Project4 95762 80and 4 98760 1 0supportedbyNSFC，thisworkwasalsosupportedbyKZCX2 -2 0 2fromChineseAcademyofSciences，theMajor |
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| 摘 要： | In this work, Princeton Ocean Model (POM) was used to study the formation of the South China Sea Warm Current (SCSWC) in the barotropic case. Monthly averaged wind stress and the inflow/outflow transports in January were used in the numerical simulation which reproduced the SCSWC. The effects of wind stress and inflow/outflow were studied separately. Numerical experiments showed thatthe Kuroshio intrusion through the Luzon Strait and the slope shelf in the northern SCS are necessary conditions for the founation of the SCSWC. In a flat bottom topography experiment, the wind stress drivennortheast current in the northern SCS is a compensatory current.
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| 关 键 词： | 南海 斜压扰动 数值实验 暧流 相图结构 |
| 收稿时间： | 1999-05-14 |
| 修稿时间： | 1999-09-20 |
Numerical study on the formation of the South China Sea Warm Current I. Barotropic case |
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| Wang Kai,Fang Yue. Numerical study on the formation of the South China Sea Warm Current I. Barotropic case[J]. Chinese Journal of Oceanology and Limnology, 2001, 19(1): 1-9. DOI: 10.1007/BF02842783 |
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| Authors: | Wang Kai Fang Yue |
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| Affiliation: | (1) Institute of Oceanology, Chinese Academy of Sciences, 266071 Qingdao, China;(2) Ocean Remote Sensing Laboratory of Ministry of Education of China, Ocean University of Qingdao, 266003 Qingdao, China |
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| Abstract: | In this work, Princeton Ocean Model (POM) was used to study the formation of the South China Sea Warm Current (SCSWC) in the barotropic case. Monthly averaged wind stress and the inflow/outflow transports in January were used in the numerical simulation which reproduced the SCSWC. The effects of wind stress and inflow/outflow were studied separately. Numerical experiments showed that the Kuroshio intrusion through the Luzon Strait and the slope shelf in the northern SCS are necessary conditions for the formation of the SCSWC. In a flat bottom topography experiment, the wind stress driven northeast current in the northern SCS is a compensatory current. |
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| Keywords: | South China Sea Warm Current barotropic circulation numerical experimex |
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