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APS -70th Annual Meeting of the APS Division of Fluid Dynamics- Event - Wave-Induced Momentum Flux over Wind-driven Surface Waves

机译:APS-流体动力学APS部门第70届年会-事件-风驱动的面波上的波动量通量

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In recent years, the exchange of momentum between the atmosphere and the ocean has been the subject of several investigations. Although the role of surface waves on the air-sea momentum flux is now well established, detailed quantitative measurements of wave-induced momentum fluxes are lacking. In the current study, using a combined Particle Image Velocimetry (PIV) and Laser Induced Fluorescence (LIF) system, we obtained laboratory measurements of the airflow velocity above surface waves for wind speeds ranging from 0.86 to 16.63 m s-1. The mean, turbulent, and wave-coherent velocity fields are then extracted from instantaneous measurements. Wave-induced stress can, therefore, be estimated. In strongly forced cases in high wind speeds, the wave-induced stress near the surface is a significant fraction of the total stress. At lower wind speeds and larger wave ages, the wave-induced stress is positive very close to the surface, below the critical height and decreases to a negative value further above the critical height. This indicates a shift in the direction of the wave-coherent momentum flux across the critical layer.
机译:近年来,大气与海洋之间的动量交换已成为几项研究的主题。尽管表面波在海气动量通量上的作用现已确立,但仍缺乏详细的波致动量通量定量测量方法。在当前的研究中,结合使用了粒子图像测速(PIV)和激光诱导荧光(LIF)系统,我们获得了风速在0.86至16.63 m s-1范围内的表面波上方气流速度的实验室测量结果。然后从瞬时测量中提取出平均,湍流和波相干速度场。因此,可以估计波浪引起的应力。在高风速的强力情况下,表面附近的波浪感应应力占总应力的很大一部分。在较低的风速和较大的波浪年龄下,波浪感应应力非常接近表面,处于临界高度以下,为正值;而在临界高度以上,则减小为负值。这表明跨临界层的波相干动量通量方向发生了变化。

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