本文首先从地球流体力学基本方程出发，通过一些基本假设，推导出海洋内波控制方程。
In the thesis, we firstly derive control equations of oceanic internal wave by basic hypothesis which is based on equation of Geophysical Fluid Mechanics.
矿脉其实有时会像植物图鉴，是因为地球的熔融性质和流体力学机制：当我们俯视的时候，就能看到像树枝一样的分支河流。
If mineral veins sometimes resemble botanical illustrations, blame it on Earth's molten nature and fluid mechanics: when seen from above, a branching river also looks like a tree.
地球磁场的演化历史对研究地核与地幔边界的动力学和地核内的磁流体力学过程提供了重要的信息。
The history of the Earth's magnetic field provides basic information on the dynamics of core mantle boundary and core convection.
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