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《Chinese Journal of Geophysics》 2005-05
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Synchronous response of tropical ocean to meridional and zonal wind stress

CHEN Hua 1, WANG Zhang-Gui 2, LIU Shi-Kuo 3,DENG Zi-Wang 1, MIN Jin-Zhong 11 Nanjing University of Information Science & Technology, Key Laboratory of MeteorologicalDisaster Environmental Variation, Nanjing 210044, China2 National Marine Environment Forecast Center, Beijing 100081, China3 Department of Atmospheric Sciences, Physical School, Peking University, Beijing 100871, China  
The synchronous response of tropical ocean to meridional and zonal wind stress has been studied. The results show that meridional wind stress of one class that diverges or converges affects velocity and geopotency field. The disturbed termocline and the zonal flow of zero class are driven directly by wind stress and affected by Kelvin wave and short Rossby wave. Rossby wave is produced by meridional wind stress. The disturbed termocline and the zonal flow of second class are driven directly by wind stress and affected by short Rossby wave. At the same time, meridional wind stress also produces short Rossby wave. In addition, warm water is recruited to the equator district strongly at the west boundary, which indicates that meridional wind stress may have warm water conveyed to the equator. West wind stress has warm water at the west boundary conveyed easterly.
【Fund】: 国家自然科学基金(40045016)资助.
【CateGory Index】: P732
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