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Observed winds, turbulence, and dispersion in built-up downtown areas of Oklahoma City and Manhattan

机译:在俄克拉荷马州市区和曼哈顿市区的市区观察到的风,湍流和散射

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Wind and tracer data from the Oklahoma City Joint Urban 2003 (JU2003) and the Manhattan Madison Square Garden 2005 (MSG05) urban field experiments are being analyzed to aid in understanding air flow and dispersion near street-level in built-up downtown areas. The mean winds are separately calculated for groups of anemometers having similar exposures such as near street level and on building top. Several general results are found, such as the scalar wind speed at street level is about 1/3 of that at building top. Turbulent standard deviations of wind speed components and temperature, and vertical fluxes of momentum and sensible heat, are calculated from sonic anemometers near street level at 20 locations in JU2003 and five locations in MSG05, and from two rooftop locations in MSG05. The turbulence observations are consistent with observations in the literature at other cities, although the JU2003 and MSG05 data are unique in that many data are available near street level. For example, it is found that the local (i.e., at the measuring height) [graphic removed] averages about 1.5 and the local [graphic removed] averages about 0.25 in the two cities, where [graphic removed] is the standard deviation of vertical velocity fluctuations, [graphic removed] is the friction velocity, and u is the wind speed. The ratio of temperature fluctuations to temperature scale, [graphic removed] , averages about -3 in both cities, consistent with similarity theory for slightly unstable conditions, where [graphic removed] is the standard deviation of temperature fluctuations, and [graphic removed] is the temperature scale. The calculated Obukhov length, L, is also consistent with slightly unstable conditions near street level, even at night during JU2003. The SF tracer concentration observations from JU2003 are analyzed. Values of [graphic removed] for the continuous releases are calculated for each release and arc distance, where [graphic removed] is the 30-min average arc maximum concentration, Q is the continuous source emission rate, and u is the spatial-averaged wind speed in the downtown area. The basic characteristics of the JU2003 plot of averaged [graphic removed] agree reasonably well with similar plots for other urban experiments in Salt Lake City and London (i.e., at [graphic removed] . A is found to be about 3 during the day and about 10 during the night.
机译:正在分析来自俄克拉荷马州城市联合城市2003(JU2003)和曼哈顿麦迪逊广场花园2005(MSG05)城市野外实验的风和示踪剂数据,以帮助理解市区繁华街道附近的气流和扩散。平均风速是分别针对具有类似暴露量的风速计组(如靠近街道水平和建筑物顶部)计算的。发现了一些一般结果,例如街道级别的标量风速约为建筑物顶部的标速风速的1/3。风速分量和温度以及动量和显热的垂直通量的湍流标准偏差是根据JU2003的20个位置和MSG05的5个位置的街道风速计和MSG05的两个屋顶位置计算的。尽管JU2003和MSG05数据是独特的,因为许多数据可在街道附近获得,湍流观测结果与其他城市的文献观测结果一致。例如,发现在两个城市中,本地(即,在测量高度处)[已删除图形]的平均值约为1.5,而本地[已删除图形]的平均值约为0.25,其中[已删除图形]是垂直方向的标准偏差速度波动,[去除图形]是摩擦速度,u是风速。在两个城市中,温度波动与温度标度的比率[图表去除]平均值约为-3,与轻微不稳定条件下的相似性理论一致,其中[图表去除]是温度波动的标准偏差,而[图表去除]为温度刻度。计算得出的奥布霍夫长度L也与街道水平附近的稍微不稳定的条件一致,即使在JU2003期间的晚上也是如此。分析了JU2003中的SF示踪剂浓度观测值。对于每个释放和电弧距离,计算连续释放的[去除图形]的值,其中[去除图形]是30分钟平均电弧最大浓度,Q是连续源排放率,u是空间平均风市区的速度。 JU2003平均值图的基本特征[去除的图形]与盐湖城和伦敦其他城市实验的类似图(即[去除图形的]的图形)相当吻合。在一天中,A大约为3。晚上10点。

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