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潜居于闽、浙外海深、底层的台湾暖流深层水(又称东海上层水或东海次表层水),是东海陆架西部海域的主要水团之一。台湾暖流深层水的消长变化,对于东海陆架西部海域的水文状况,以及渔业生产的影响非常显著。关于台湾暖流深层水,国内、外海洋学者曾对其温、盐度特性和来源作过一些研究,但对其变化(季节变化和多年变化)特征研究尚少。探讨这一问题,将有助于进一步了解该水团的基本特征。
Living in Fujian, Zhejiang and the sea depth, the bottom of the Taiwan warm current deep water (also known as the upper East China Sea or the East China Sea sub-surface water), the East China Sea Shelf of the western waters one of the major water. The variation of the growth and decline of deep water in Taiwan’s warm current is very significant for the hydrological conditions in the western waters of the East China Sea Shelf and the fishery production. With regard to the deep currents of warm current in Taiwan, some studies on the characteristics and sources of temperature and salinity have been made by domestic and overseas marine scholars. However, there are few studies on the characteristics of their changes (seasonal variations and years of changes). Exploring this issue will help to further understand the basic characteristics of the water regiment.