stratified ocean

基本解释

The interfacial waves on large-scale currents in the ocean is typical of stratified flow.
在海洋水域，界面波对大尺度变化流的作用是一种典型的分层流动现象。
As the ocean warms, it becomes more stratified, with the warmer water remaining at the top where the organisms need to be in order to do photosynthesis.
但是随着海水变暖，它的层次会更加分明，温度更高的海水会停留在表面，而这里正是生物体进行光合作用必需的地方。
The dissertation firstly introduces the primary concepts, observational methods, generation mechanism, distribution, evolution and breaking of internal waves in the stratified ocean.
本论文首先介绍了内波的基本概念：内波的观测、生成机制、分布、传播演变过程以及内波和混合等。

分层海洋
A new simulation model of SAR signatures of internal solitary waves is put forward by us, which is based on continuous stratified ocean model.
我们建立一种新的基于连续分层海洋模型的内孤立波SAR遥感仿真模型。
层化海洋