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Characterization of Wind Meandering in Low-Wind-Speed Conditions

机译:低风速条件下的蜿蜒曲折特性

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Investigation of low-wind cases observed during the Urban Turbulent Project campaign (Torino, Italy) and at the Santa Maria meteorological station (Santa Maria, Brazil) provides insight into the wind-meandering phenomenon, i.e. large, non-turbulent oscillations of horizontal wind speed and temperature. Meandering and non-meandering cases are identified through analysis of the Eulerian autocorrelation functions of the horizontal wind-velocity components and temperature. When all three autocorrelation functions oscillate, meandering is present. As with weak turbulence, meandering shows no dependence on stability but is influenced by presence of buildings and depends on wind speed. We show that, while the standard deviation of the horizontal velocity is always large in low-wind conditions, the standard deviation of the vertical velocity shows very different behaviour in meandering and non-meandering conditions. In particular, the value of the ratio of the standard deviations of the vertical and horizontal velocities typifies the meandering condition.
机译:对城市湍流项目运动(意大利都灵)和圣玛丽亚气象站(巴西圣玛丽亚)观测到的低风情况进行了调查,可以深入了解风向现象,即水平风的大的非湍流振荡速度和温度。通过分析水平风速分量和温度的欧拉自相关函数,可以确定蜿蜒和不蜿蜒的情况。当所有三个自相关函数都振荡时,就会出现曲折。与湍流一样,蜿蜒曲折不依赖于稳定性,但受建筑物的存在影响,并依赖于风速。我们表明,尽管在低风条件下水平速度的标准偏差始终很大,但在蜿蜒和非曲折条件下垂直速度的标准偏差却表现出非常不同的行为。特别地,垂直和水平速度的标准偏差之比的值代表曲折条件。

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