The wave induced Reynolds stress is introduced into the wind wave interaction and closed by the eddy viscosity model.
在风波相互作用中引入波诱导雷诺应力并用涡流粘度予以封闭。
Bound infragravity waves are forced by wave-wave nonlinear interaction of two wind waves, depended only on the swell energy and water depth.
强迫次重力波的形成机制为海浪的波-波非线性相互作用，它仅依赖于海浪和水深的大小。
The cause of the packet energy variation is wave-flow interaction produced by temporal variation of the wind.
能量变化的实质是，风场的时变性引起了波流相互作用。
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