Assessing methods to extrapolate the vertical wind-speed profile from surface observations in a city centre during strong winds
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Assessing methods to extrapolate the vertical wind-speed profile from surface observations in a city centre during strong winds

机译:在强风中,评估从城市中心的表面观测外推动垂直风速曲线的方法

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AbstractKnowledge of the vertical wind-speed profile in cities is important for the construction and insurance industries, wind energy predictions, and simulations of pollutant and toxic gas release. Here, five methods to estimate the spatially- and temporally-averaged wind-speed profile are compared in London: the logarithmic wind law (LOG); the Deaves and Harris equilibrium (DHe) and non-equilibrium (DHv) models; an adaptation of the power law (PL) and the Gryning et?al. (GR) profile. Using measurements at 2.5 times the average building height, a source area model is used to determine aerodynamic roughness parameters using two morphometric methods, which assume homogeneous and variable roughness-element heights, respectively. Hourly-averaged wind speeds are extrapolated to 200?m above the canopy during strong wind conditions, and compared to wind speeds observed with Doppler lidar. Wind speeds are consistently underestimated if roughness-element height variability is not considered during aerodynamic parameter determination. Considering height variability, the resulting estimations with theDHeandGRprofiles are marginally more similar to observations than theDHvprofile, which is more accurate than theLOGandPLmethods. An exception is i
机译:<![CDATA [ 抽象 在城市中的垂直风速曲线知识对于建筑和保险行业,风能预测很重要,和污染物和有毒气体释放的模拟。在这里,在伦敦比较了五种估计空间和时间平均风速曲线的方法:对数风法( log ); deaves和harris均衡( dh e )和非均衡( dh v )模型;权力法的改编( pl )和gryning等。 ( gr )配置文件。使用平均建筑高度的2.5倍的测量值,使用两个形态学方法来确定空气动力学粗糙度参数,分别呈现均匀和可变粗糙度元素高度。在强风条件下,每小时平均风速将在遮篷上方推到200μm,并且与用多普勒·丽达观察到的风速相比。如果在空气动力学参数确定期间不考虑粗糙度元素高度可变性,则风速始终低估。考虑高度可变性,结果估计与 dh e gr 概况与观察更类似于 dh v < / ce:斜体> 配置文件,它比 log pl 方法更准确。我是一个例外

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