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本文利用现有的CTD资料估算了东海大陆架和大陆坡一个断面上的温度梯度垂向波数谱;揭示了一个断面上不同深度的测站和不同层次的谱特性,并与深水大洋中的主温跃层作了比较;文中还推测了细结构的某些可能的产生机制。
In this paper, we use the available CTD data to estimate the vertical wave number spectrum of the temperature gradient on a section of the East China Sea continental shelf and the continental slope. We reveal the spectral characteristics at different depths of stations and at different levels in a section, The comparison between the thermocline and the thermocline shows that some possible mechanisms of the fine structure are also speculated.