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Analysis of Characteristics of Atmospheric Structure Constant of Refractive Index Based on Wind Profiler Radar in Precipitation

机译:基于风分析雷达在沉淀下的折射率大气结构常数特征分析

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The atmospheric structure constant of refractive index is an important parameter to describe the turbulent characteristics of the atmosphere. Using the ROBS data obtained by the Sichuan Provincial Meteorological Bureau in the Yanyuan, Dayi, Xinjin, Xindu, and Longquanyi districts, the real-time sampling of ROBS data combined with the hourly precipitation data provided by conventional meteorological observation stations was used for statistical analysis. Study the change trend of atmospheric structure constant of refractive index in the precipitation process in different regions. The results show that the convective movement during the precipitation process and the drag effect of the precipitation particles on the surrounding atmosphere, with the occurrence and development of the precipitation process, atmospheric structure constant of refractive index has a significant increasing trend, indicating the significance of precipitation. The vertical velocity and C~2_n are consistent with the change of precipitation, which can better reflect the change of precipitation intensity. The C~2_n value corresponding to the maximum precipitation time is two to five orders larger than that before and after the occurrence of precipitation.
机译:折射率的大气结构常数是描述大气的湍流特性的重要参数。利用由亚源,大邑,新金,新城和龙田地区的四川省气象局获得的ROBS数据,使用常规气象观察站提供的Robs数据的实时采样与常规气象观察站提供的每小时降水数据一起用于统计分析。研究不同地区沉淀过程中折射率大气结构常数的变化趋势。结果表明,在沉淀过程中的对流运动和沉淀颗粒对周围大气中的沉淀颗粒的阻力作用,随着沉淀过程的发生和发展,折射率大气结构常数具有显着的趋势,表明了重要性沉淀。垂直速度和C〜2_N与降水的变化一致,这可以更好地反映降水强度的变化。与最大降水时间相对应的C〜2_N值是比在发生沉淀之前和之后的两到五个订单。

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