...的影响，相对应地会出现温跃层（Thermocline，温度梯度较大）和盐跃层 （Halocline，盐度梯度较大），并导致密跃层（Pycnocline）的出现，其出现的深度一 般在300～1000m处。
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In particular,the applications of these models in sea surface height and thermocline/pycnocline depth variability in the North Pacific Ocean were described in detail.
这些模型被广泛地应用到北太平洋海表面高度和温度/密度跃层深度等要素变化的机理研究中,得到了不同的模型在大洋的不同区域有不同的作用等结论。
参考来源 - 北太平洋Rossby波研究进展·2,447,543篇论文数据，部分数据来源于NoteExpress
以上来源于: WordNet
The oceanic temperature anomaly is mainly located in pycnocline both on the interannual and interdecadal time scales.
年际和年代际尺度上，热带太平洋的温度异常主要发生在密度跃层附近。
In this experiment, typical pycnocline-type profiles are employed, and the internal waves are generated by a wave maker designed by the authors.
实验中的密度分层采用典型跃层型剖面，而内波是由自行研制的造波机生成。
It is pointed out that ICW occurs in the pycnocline and superimposes on the pycnocline due to the buoyancy effect of Taiwan Warm Current water with high density.
中层冷水是存在于密跃层之中，高密度（台湾暖流）水的浮力效应使其叠置于它的上方；
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