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.