台湾海峡的温度逆跃层

The inversion thermocline in Taiwan Strait

本文利用1940～1986年国内外海洋观测资料约3600站次,分析了116°～121°E,21°30′～26°N区域内海水的温度逆跃层,结果表明本海域秋、冬、春季西岸海区出现温度逆跃层,同渤海相比,本区温度逆跃层的上界深度较深,厚度较大强度也较大,文中对该类温度逆跃层的成因作了初步探讨。

This paper discusses the inversion thermoeline in the Taiwan Strait. The result indicates the thermocline appears along western Taiwan Strait during autumn, winter and spring. In comparison with that in the Bohai Sea, the upper bound of the thermoeline in the Taiwan Strait is deeper, thicker and stronger.