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《Chinese Journal of Atmospheric Sciences》 2004-01
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Seasonal Variation of the Barrier Layer in the South China Sea and Its Relationship to the Sea Surface Flux

Du Yan 1,2), Wang Dongxiao 1), Shi Ping 1), Guo Peifang 2), and Chen Ju 1)1) (Key Laboratory of Tropical Marine Environmental Dynamics, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301) 2) (Marine Environmental College, Ocean University of China, Qingdao 266003)  
Analysis of the climatological temperature and salinity shows the evidence of the barrier layer(BL) in the southern South China Sea(SCS) in the summer. The net fresh water flux is a key factor to determine the occurrence of the BL. The structure and distribution of the BL is dominated by the wind fields, and adjusted by the development of the mixed layer (ML) and isothermal layer (IL). During summer, the SCS boundaries restrict the easterly Ekman transport, and the Ekman pumping is negative in the eastern SCS. Those two effects result in the fresher water pile up in the southeastern SCS. The high temperature waters detrain from ML and retain in IL, which cause the most deepest and thickest BL in southeastern SCS. The maximum reaches 30 m. The thickest BL occurs where the SCS Warm Water occurs, so the “heat barrier effect” facilitates the development of the SCS Warm Water.
【Fund】: 国家自然科学基金资助项目 40 1 760 0 6;; “十五”社会公益研究专项 2 0 0 1DIA5 0 0 41;; 国家重点基础研究发展规划项目G1 9990 43 80 6资助
【CateGory Index】: P732
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