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Simulation and analysis on seasonal variability of average salinityin the Yellow Sea
作者姓名:马建  乔方利
作者单位:The First Institute of Oceanography,State Oceanic Administration,SOA,Qingdao 266061,China,Key Laboratory of Marine Sciences and Numerical Modeling (MASNUM),SOA,Qingdao 266061,China
基金项目:SupportedbytheNationalBasicResearchProgramofChina(No.G1999043809) theNationalScienceFoundationofChina(No.49736190).
摘    要:The CTD (conductivity, temperature and depth) data collected by six China-Korea joint cruises during 1996-1998 and the climatological data suggest that the seasonal variability of average salinity in the Yellow Sea (Sa) presents a general sinusoid pattern. To study the mechanism of the variability, annual cycles of Sa were simulated and a theoretical analysis based on the governing equations was reported.Three main factors are responsible for the variability: the Yellow Sea Warm Current (YSWC), the Changji-ang (Yangtze) River diluted water (YRDW) and the evaporation minus precipitation (E-P). From December to the next May, the variability of Sa is mainly controlled by the salt transportation of the YSWC. But in early July, the YSWC is overtaken and replaced by the YRDW which then becomes the most important controller in summer. From late September to November, the E-P gradually took the lead. The mass exchange north of the 37癗 line is not significant.

关 键 词:季节形变化  仿真  平均盐度  黄海
收稿时间:20 April 2004
修稿时间:16 May 2004

Simulation and analysis on seasonal variability of average salinity in the Yellow Sea
Ma?Jian,Qiao?Fangli.Simulation and analysis on seasonal variability of average salinityin the Yellow Sea[J].Chinese Journal of Oceanology and Limnology,2004,22(3):306-313.
Authors:Ma Jian  Qiao Fangli
Institution:(1) The First Institute of Oceanography, State Oceanic Administration, SOA, 266061 Qingdao, China;(2) Key Laboratory of Marine Sciences and Numerical Modeling (MASNUM), SOA, 266061 Qingdao, China
Abstract:The CTD (conductivity, temperature and depth) data collected by six China-Korea joint cruises during 1996–1998 and the climatological data suggest that the seasonal variability of average salinity in the Yellow Sea (Sa) presents a general sinusoid pattern. To study the mechanism of the variability, annual cycles ofSa were simulated and a theoretical analysis based on the governing equations was reported. Three main factors are responsible for the variability: the Yellow Sea Warm Current (YSWC), the Changjiang (Yangtze) River diluted water (YRDW) and the evaporation minus precipitation (E-P). From December to the next May, the variability ofSa is mainly controlled by the salt transportation of the YSWC. But in early July, the YSWC is overtaken and replaced by the YRDW which then becomes the most important controller in summer. From late September to November, the E-P gradually took the lead. The mass exchange north of the 37°N line is not significant. Supported by the National Basic Research Program of China (No. G1999043809) and the National Science Foundation of China (No. 49736190).
Keywords:Yellow Sea  average salinity  wave-tide-circulation coupled model  Yellow Sea Warm Current  Changjiang (Yangtze) River diluted water  evaporation minus precipitation
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