Observation Analysis of Wind Shear Characteristics from Troposphere Wind Profiler

Wenlin Chen, Debin Su, Lijuan Wang, Tonggen Wang
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Abstract

Observed data of each sampling height from P-band troposphere type □ wind profiler in Sichuan Yanyuan station(2466m ASL) and Qianwei station(486m ASL) in March 2018 is taken to study the temporal and spatial characteristics as well as the differences of wind shear from troposphere wind profiler at different altitudes. The values of horizontal wind speed and wind direction obtained by wind profiler are used to calculate the wind shear index at different time and different altitudes based on the power-law formula. By calculating vector difference and fitting the index on account of least square method, the vertical wind shear characteristics over the two stations are analyzed and compared with the products measured by wind profiler. The results show that the algorithm of wind shear index based on the power-law formula can preferable to reflect the wind shear characteristics of the wind field. The wind shear index tends to decrease with the increase of altitude because of the influence of the underlying surface on the wind speed. In addition, wind shear index also shows a trend of smaller in daytime, larger at night, smaller in plain area and larger in hilly area.
对流层风廓线风切变特征观测分析
利用2018年3月四川盐源站(2466m ASL)和前卫站(486m ASL) p波段对流层型□风廓线各采样高度观测资料,研究不同高度对流层风廓线风切变的时空特征及差异。利用风廓线仪获取的水平风速和风向值,根据幂律公式计算不同时间、不同高度的风切变指数。通过计算矢量差值,利用最小二乘法拟合指标,分析了两站垂直风切变特征,并与风廓线仪实测结果进行了比较。结果表明,基于幂律公式的风切变指数算法能较好地反映风场的风切变特征。由于下垫面对风速的影响,风切变指数有随海拔升高而减小的趋势。此外,风切变指数也呈现白天小、夜间大、平原地区小、丘陵地区大的趋势。
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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