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首页> 外文期刊>Annalen der Meteorologie >LIDAR AND RADAR MEASUEMENTS OF THE MELTING LAYER IN THE FRAME OF THE CONVECTIVE AND OROGRAPHICALLY-INDUCED PRECIPITATION STUDY
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LIDAR AND RADAR MEASUEMENTS OF THE MELTING LAYER IN THE FRAME OF THE CONVECTIVE AND OROGRAPHICALLY-INDUCED PRECIPITATION STUDY

机译:对流和地形诱发降水研究框架中融化层的激光和雷达测量

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摘要

During the Convective and Orographically-induced Precipitation Study (COPS), lidar dark/ bright and bands were observed by the Univ. of BASILicata Raman lidar system (BASIL) on several IOPs and SOPs (among others, 23 July, 15 August, 17 August). Darklbright band signatures appear in the lidar measurements of the particle backscattering. Lidar data are supported by measurements from the University of Hamburg cloud radar MIRA 36 (36 GHz), the University of Hamburg dual-polarization micro rain radars (24.1 GHz) and the University of Manchester Radio UHF clear air wind profiler (1.29 GHz). Results from BASIL and the radars will be illustrated and discussed at the Conference to support in the comprehension of the microphysical and scattering processes responsible for the appearance of the lidar dark band and radar bright band.
机译:在对流和地形诱发的降水研究(COPS)中,大学观测到了激光雷达的暗/亮和条带。几个IOP和SOP上的BASILicata Raman激光雷达系统(BASIL)(7月23日,8月15日,8月17日)。 Darklbright带签名出现在粒子反向散射的激光雷达测量中。汉堡大学云雷达MIRA 36(36 GHz),汉堡大学双极化微雨雷达(24.1 GHz)和曼彻斯特大学无线电超高频晴空风廓线仪(1.29 GHz)的测量结果为激光雷达数据提供了支持。会议上将对BASIL和雷达的结果进行说明和讨论,以支持理解造成激光雷达暗带和雷达亮带出现的微物理和散射过程。

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