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THREE-DIMENSIONAL BAROCLINIC NUMERICAL SIMULATION OF THE SOUTH CHINA SEA CIRCULATION'S SEASONAL CHARACTERISTICS II. MIDDLE AND DEEP CIRCULATION

最后更新:2018年07月29日 06:00 点击数:3

【类型】期刊

【基金项目】国家重点基础研究发展计划(973计划)(Project 49636230)

【作者】蔡树群;甘子钧;苏纪兰;刘秦玉 

【关键词】 South China Sea monsoon circulation model eddy numerical simulation

【期刊名】中国海洋湖沼学报(英文版)

【内容提要】A three-dimensional baroclinic shelf sea model's numerical simulation of the South China Sea (SCS) middle and deep layer circulation structure showed that: 1. In the SCS middle and deep layer, a southward boundary current exists along the east shore of the Indo-China Peninsula all year long. A cyclonic eddy (gyre) is formed by the current in the above sea areas except in the middle layer in spring, when an anticyclonic eddy exists on the eastern side of the current. In the deep layer, a large-scale anticyclonic eddy often exists in the sea areas between the Zhongsha Islands and west shore of southern Luzon Island. 2. In the middle layer in summer and autumn, and in the deep layer in autumn and winter, there is an anticyclonic eddy (gyre) in the northeastern SCS, while in the middle layer in winter and spring, and in the deep layer in spring and summer, there is a cyclonic one. 3. In the middle layer, there is a weak northeastward current in the Nansha Trough in spring and summer, while in autumn and winter it evolves into an anticyclonic eddy (gyre), which then spreads westward to the whole western Nansha Islands sea areas.

【年份】2018-07

【ISSN号】0254-4059

【页码】9-15

【期号】第1期

【作者单位】South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China;The Second Institute of Oceanography, SOA, Hangzhou 310012, China;Ocean University of Qingdao,Qingdao 266003, China

【卷号】第20卷

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