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Numerical Simulations of Air-Water Flow of a Non-linear Progressive Wave in an Opposing Wind

机译:逆风中非线性渐进波空气-水流的数值模拟

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We present detailed numerical results for two-dimensional viscous air-water flow of a non-linear progressive water wave when the speed of the opposing wind varies from zero to 1.5 times the wave phase speed. It is revealed that at any speed of the opposing wind there exist two rotating airflows, one anti-clockwise above the wave peak and one clockwise above the wave trough. These rotating airflows form a buffer layer between the main stream of the opposing wind and the wave surface. The thickness of the buffer layer decreases and the strength of rotation increases as the wind speed increases. The profile of the average -component of velocity reveals that the water wave behaves as a solid surface producing larger wind stress compared to the following-wind case.
机译:当逆风的速度从零到波速的1.5倍变化时,我们给出了非线性渐进水波的二维粘性空气-水流的详细数值结果。结果表明,在逆风的任何速度下,都存在两个旋转的气流,一个在波峰上方逆时针旋转,另一个在波谷上方逆时针旋转。这些旋转的气流在逆风的主流和波浪表面之间形成缓冲层。随着风速的增加,缓冲层的厚度减小,旋转强度增加。速度的平均分量的分布表明,与随风情况相比,水波表现为产生较大风应力的固体表面。

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