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台湾海峡水体和热盐通量季节变化研究
The Seasonal Variations of Fluxes for Mass,Heat and Salinity in Taiwan Strait
【摘要】 利用HYCOM模式在台湾海峡附近一个断面处1 a的温盐流输出结果,计算了南海和东海之间通过台湾海峡输运的水体及热盐通量。结果表明:夏季的水体通量和热盐通量最大,秋季的水体通量和盐通量最小,而春季的热通量最小,3个通量均呈现出明显的季节变化。水体通量和热盐通量的季平均值分别为1.14 Sv,1.1×1014W,3.97×1010 g/s。
【Abstract】 The fluxes of mass,heat and salinity between the South China Sea and the East China Sea via Taiwan Strait were estimated using hydrologic and current data of one year in a section of Taiwan Strait from HYCOM model.The following conclusions can be obtained.The three fluxes are all reach maximum in summer while the time they reach minimum is not coincident: autumn for the mass and salinity fluxes and spring for the heat flux.Despite of which,the results represent significantly seasonal variations for the three fluxes.The year-averaging values for mass flux,heat flux and salinity flux are 1.14 Sv,1.1×1014 W and 3.97×1010 g/s,respectively.
- 【文献出处】 海洋技术 ,Ocean Technology , 编辑部邮箱 ,2013年02期
- 【分类号】P731
- 【被引频次】3
- 【下载频次】121