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风廓线雷达对折射率结构常数的实测分析
引用本文:范潇,张福贵,张利华.风廓线雷达对折射率结构常数的实测分析[J].成都信息工程学院学报,2013(6):611-616.
作者姓名:范潇  张福贵  张利华
作者单位:[1]成都信息工程学院电子工程学院,四川成都610225 [2]成都信息工程学院电子工程学院,四川成都610225;中国气象局大气探测重点开放实验室四川成都610225 [3]广州军区空军气象中心工程师,广东广州510071
基金项目:公益性行业(气象)科研专项资助项目(GYHY200906039);四川省教育厅重大培育资助项目(11ZZ015).
摘    要:大气折射率结构常数(Cn2)是大气中折射率大小的体现,为了改善风廓线雷达(WPR)数据质量,提高WPR数据业务应用的可靠性,对边界层风廓线雷达近1年的实测数据采用归纳对比的方法,分析得到Cn2与温度湿度变化的关系,并总结出成都地区晴朗天气下,四季Cn2量级的变化范围,与理论推导一致.夏天10-12到10-20,春秋10-13到10-20,冬天10-14到10-21,此外,根据降水量大小不同,Cn2提升3到6个量级,获得这些定量的范围,为相关风廓线雷达产品识别提供了方法和依据.

关 键 词:气象雷达  边界层风廓线雷达  折射率结构常数  归纳对比  实测分析

Measurement and Analysis of Refractive Index Structure Constant with the Wind Profile Radar
FAN XiaoSchool of Electronic Engineering Chengdu University of Information Technology,Chengdu,China ZHANG Fu-guiSchool of Electronic Engineering Chengdu University of Information Technology,Chengdu,China;Key Laboratory of Atmospheric Sounding,Chengdu,China ZHANG Li-hua.Measurement and Analysis of Refractive Index Structure Constant with the Wind Profile Radar[J].Journal of Chengdu University of Information Technology,2013(6):611-616.
Authors:FAN XiaoSchool of Electronic Engineering Chengdu University of Information Technology  Chengdu  China ZHANG Fu-guiSchool of Electronic Engineering Chengdu University of Information Technology  Chengdu  China;Key Laboratory of Atmospheric Sounding  Chengdu  China ZHANG Li-hua
Institution:FAN Xiao(School of Electronic Engineering Chengdu University of Information Technology, Chengdu 610225, China) ZHANG Fu-gui(School of Electronic Engineering Chengdu University of Information Technology, Chengdu 610225, China;Key Laboratory of Atmospheric Sounding,Chengdu 610225,China) ZHANG Li-hua(Meteorology Center of Guangzhou Military District Air Force,Guangzhou 510071 ,China)
Abstract:Refractive index structure constant (Cn2) reflects the intensity of atmospheric reflectivity.To improve the data quality and reliability of service application,this paper summarizes the relationships between Cn2 and temperature,humidity by applying inductions and statistics method to the observed data of boundary layer WPR for a whole year.Meanwhile a vary magnitude range of Cn2 is summarized during the fine days in Chengdu,which is consistent with the theory.The range of summer is from 10-12 to 10-20,and winter is from 10-14 to 10-21.Spring and autumn are from 10-13 to 10-20.In addition,Cn2 promotes its magnitude about 3 to 6 grade based on different precipitations.These quantitative ranges provide approach and basis for the product recognition of WPR.
Keywords:meteorological radar  boundary layer Wind Profile Radar  refractive index structure constant  inductions and statistics  analyses of observed data
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