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WAVE-INDUCED EFFECT ON THE AIRSIDE VELOCITY FIELD ABOVE THE WIND- GENERATED WATER WAVES

机译:风产生的水波上方对波速场的波诱导效应

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An experimental study was conducted to investigate the influence of surface waves on the airside flow behavior over the water surface. Two-dimensional velocity field in a plane perpendicular to the surface was measured using particle image velocimetry (PIV) at wind speeds of 3.7 and 4.4 m s~(-1). The results show that the wave induced velocities are significant immediately adjacent to the water surface and their magnitudes decreases with height and become negligible at a height three times the significant wave height. The structure of the wave induced vorticity indicates two different type of flow pattern on the windward and leeward sides of the wave crest. Positive and negative magnitudes of the turbulent and wave induced Reynolds stress respectively, indicates upward and down transfer of momentum flux across air water interface. The results also indicate that the flow dynamics in the region two to three times significant wave heights are significantly different than that at greater heights. Higher magnitudes of the turbulent and wave induced Reynolds stresses were observed in this region which could not be predicted from the measurements at greater heights. Thus, it is concluded the understanding of the wave effects to the airflow field especially within the crest-trough region is vital to improve our knowledge about the air-water heat, mass and momentum exchange.
机译:进行了一项实验研究,以研究表面波对水面空气流动特性的影响。使用粒子图像测速仪(PIV)在风速3.7和4.4 m s〜(-1)下测量垂直于表面的平面中的二维速度场。结果表明,波浪感应速度在紧邻水面的位置非常显着,并且其幅度随着高度的增加而减小,并且在三倍于重要波浪高度的高度处可以忽略不计。波浪引起的涡度的结构在波峰的上风侧和下风侧指示了两种不同类型的流动模式。湍流和波引起的雷诺应力的正负幅值分别表示动量通量在空气-水界面上的向上和向下传递。结果还表明,在波高的2到3倍的区域中,流动动力学与在较大波高处的流动动力学显着不同。在该区域中观察到了更高的湍流和波浪诱发的雷诺应力,这无法从更高高度的测量结果中预测到。因此,可以得出结论,特别是在波峰-波谷区域内,对波场对气流场的影响的理解对于增进我们对空气-水的热量,质量和动量交换的认识至关重要。

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