利用微脉冲激光雷达识别过冷水云层  

Identification of Supercooled Water Clouds by Using Micro Pulse Lidar

作　　者：宋继烨 檀望舒[1] 李成才 于营丽[1] 李建 初奕琦[1] SONG Jiye;TAN Wangshu;LI Chengcai;YU Yingli;LI Jian;CHU Yiqi(Department of Atmospheric and Oceanic Sciences,School of Physics,Peking University,Beijing 100871;Baicheng Ordnance Test Center of China,Baicheng 137001)

机构地区：[1]北京大学物理学院大气与海洋科学系,北京100871 [2]中国白城兵器试验中心,白城137001

出　　处：《北京大学学报（自然科学版）》2018年第5期961-969,共9页Acta Scientiarum Naturalium Universitatis Pekinensis

基　　金：国家重点研发计划(2016YFC0202004);国家自然科学基金(41375008)资助

摘　　要：在已有的云识别算法基础上,利用微脉冲激光雷达后向散射信号区分云和气溶胶。按照云粒子的退偏振比,区分冰云、水云、混合云以及水平导向的冰晶云。结合大气温度廓线,对过冷水云层进行有效的识别。利用观测点上空持续一年的观测资料,统计各种云出现的高度及比例的逐月变化,结果显示,过冷水云出现的时间占有云时间的9.84%,对于0^-40℃的云层,过冷水云出现的时间占11.99%。On the basis of a previous algorithm of cloud detection,clouds and aerosols are distinguished by analyzing the backscatter signals of a micro pulse lidar.In this way,the content of clouds are classified into ice,water,mixed-phase clouds and horizontal oriented ice flakes.Finally,the supercooled water clouds are distinguished from water clouds by the information of temperature profiles.The monthly changes of the appearance heights and proportions of the various clouds are also calculated with one-year observations over the lidar site.The supercooled clouds are found to appear at 9.84%of all the cloudy time,and 11.99%of all the time for clouds at from 0℃to?40℃.

关 键 词：过冷水云层 微脉冲激光雷达 退偏振比 温度廓线 

分 类 号：P407[天文地球—大气科学及气象学]