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Numerical simulations of laminar air-water flow of a non-linear progressive wave at low wind speed

机译:低风速下非线性行波的层流气水流动数值模拟

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摘要

A numerical simulation for two-dimensional laminar air-water flow of a non-linear progressive water wave with large steepness is performed when the background wind speed varies from zero to the wave phase speed. It is revealed that in the water the difference between the analytical solution of potential flow and numerical solution of viscous flow is very small, indicating that both solutions of the potential flow and viscous flow describe the water wave very accurately. In the air the solutions of potential and viscous flows are very different due to the effects of viscosity. The velocity distribution in the airflow is strongly influenced by the background wind speed and it is found that three wind speeds, U=0 U=um (the maximum orbital velocity of a water wave), and U=c (the wave phase speed), are important in distinguishing different features of the flow patterns.
机译:当背景风速从零变化到波相速度时,对陡峭的非线性渐进水波进行二维层流空气流动的数值模拟。结果表明,在水中,势流的解析解与粘性流的数值解之间的差异很小,表明势流和粘性流的解都非常准确地描述了水波。在空气中,由于粘度的影响,势能流和粘性流的解决方案非常不同。气流中的速度分布受背景风速的强烈影响,发现三个风速分别为U = 0 U = um(水波的最大轨道速度)和U = c(波相速度)对于区分流型的不同特征很重要。

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    Wen X; Mobbs S;

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  • 年度 2014
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