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A laboratory observation of the surface temperature and velocity distributions on a wavy and windy air-water interface

机译:在波浪和有风的空气-水界面上进行表面温度和速度分布的实验室观察

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摘要

Temperature and velocity distributions of the water surface are examined experimentally with infrared imaging techniques. The surface velocity is determined from the movement of the pattern of surface temperature cell. It is found that the mean wind drift is about 30%u(*), much less than the widely cited measurements of 55%u(*). Although many complicated thermal and dynamical processes control the surface temperature, we found that the probability distribution function (PDF) of the standardized water surface temperature does not vary significantly with wind speed. The increasing nonlinear effects of wave orbital motions and wave breaking on surface motion are shown by the similarity and trend of change in the PDFs of the water surface velocity normalized by the wave orbital velocity at different wind speeds. The standard deviation of the speed distribution increases with the wind speed while the basic skewed distribution shape remains. (C) 2004 American Institute of Physics. [References: 18]
机译:用红外成像技术对水表面的温度和速度分布进行了实验检查。表面速度由表面温度单元的图案的运动确定。结果发现,平均风漂移约为30%u(*),远低于被广泛引用的55%u(*)的测量值。尽管许多复杂的热力和动力学过程控制着地表温度,但我们发现标准化水面温度的概率分布函数(PDF)不会随风速显着变化。波浪轨道运动和波浪破碎对地表运动的非线性影响越来越大,这是由在不同风速下通过波浪轨道速度归一化的水面速度PDF的相似性和变化趋势表明的。速度分布的标准偏差随风速增加,而基本的偏斜分布形状保持不变。 (C)2004美国物理研究所。 [参考:18]

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