Wind waves impact on the velocity in wave boundary layer in the condition of dynamically smooth surface

K. L. Yegorov, K. Bulgakov
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Abstract

One of the factors of wind wave impact on vertical distributions in atmosphere surface layer is the flux of momentum produced by the wave-produced fluctuations. Wave surface are supposed to be a dynamically rough and effects of the molecular viscosity are neglected. In this paper impact of wave momentum fluxes with values of wind velocity which lead to dynamically smooth ocean surface is estimated. The well-known theoretical aspects and results of experimental research are applied. Dependence of dimensionless thickness of viscosity layer on dimensionless roughness of smooth surface is analyzed. The equations of motion are formed taking into account the manifestation of three factors: molecular, turbulent and wave momentum flux. The models based on these equations are described.The choice of constant coefficients that are set in calculations with this model is considered. Results of calculations and analysis of vertical profiles of wind speed and the dependence of the drag coefficient on wind velocity under various wave age.
动态光滑表面条件下风浪对波浪边界层速度的影响
风浪对大气表层垂直分布的影响因素之一是风浪产生的波动所产生的动量通量。波浪表面应该是动态粗糙的,分子粘度的影响被忽略了。本文估算了波浪动量通量对风速值的影响,风速值会导致动态光滑的海洋表面。本文应用了众所周知的理论和实验研究成果。分析了粘性层的无量纲厚度与光滑表面无量纲粗糙度的关系。考虑到分子、湍流和波浪动量通量这三个因素的表现,形成了运动方程。对基于这些方程的模型进行了描述,并考虑了在使用该模型进行计算时对常数系数的选择。计算结果和风速垂直剖面分析,以及不同波龄下阻力系数与风速的关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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