首页> 外文会议>2018 2nd URSI Atlantic Radio Science Meeting >Microphysical and Kinematic Characteristics of Precipitation Systems Derived from Quasi-Vertical Profiles of Radar Measurables
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Microphysical and Kinematic Characteristics of Precipitation Systems Derived from Quasi-Vertical Profiles of Radar Measurables

机译:从雷达可测物的准垂直剖面得出的降水系统的微物理和运动学特征

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摘要

Dual-polarization parameters provide detail information on microphysical processes in precipitation systems. The vertical structures of precipitation systems vary with the different microphysical processes, such as size sorting, evaporation, melting, freezing, riming, aggregation, etc. The upward air motion within the precipitation system is also related to the development of precipitation systems. The studies on precipitation systems have been carried out to estimate the linear wind field synthesis (wind direction, speed, vertical air motion, horizontal divergence, etc.) using the radar-observed velocity-azimuth display curve.
机译:双极化参数提供了有关降水系统中微物理过程的详细信息。降水系统的垂直结构随不同的微观物理过程而变化,例如大小分选,蒸发,熔融,冻结,边缘化,聚集等。降水系统内的向上空气运动也与降水系统的发展有关。已经进行了关于降水系统的研究,以利用雷达观测的速度-方位角显示曲线估算线性风场的合成(风向,速度,垂直空气运动,水平散度等)。

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  • 会议地点 Meloneras(ES)
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    National Institute of Meteorological Research, Forecast Research Division, Seogwipo, 697-845, ROK;

    Kyungpook National University, Center for Atmospheric Remote sensing (CARE), Daegu, ROK;

    Kyungpook National University, Center for Atmospheric Remote sensing (CARE), Daegu, ROK;

    Kyungpook National University, Center for Atmospheric Remote sensing (CARE), Daegu, ROK;

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