Microphysical modes of precipitation growth determined by S‐band vertically pointing radar in orographic precipitation during MAP
Microphysical modes of precipitation growth determined by S‐band vertically pointing radar in orographic precipitation during MAP
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S波段垂直指向雷达确定MAP期间地形降水的降水增长微物理模式
DOI：
10.1256/qj.01.216
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发表时间：
2003
影响因子：
8.9
通讯作者：
R. Houze
中科院分区：
文献类型：
--
作者：
S. Yuter;R. Houze
在中尺度阿尔卑斯山计划（MAP）密集观测期（IOPs）2b和8期间，华盛顿大学地形降水雷达（OPRA）在瑞士洛迦诺-蒙蒂获得的地形雨内的高分辨率垂直指向S波段多普勒雷达数据被检查以表征细尺度降水结构。在同一柱中，雨滴收集云水与冰粒收集云水（雾凇）的相对作用使用一维（1D）Kessler水连续性模型进行评估，使用观测数据特征作为输入。
High‐resolution vertically pointing S‐band Doppler radar data obtained within orographic rain by the University of Washington Orographic Precipitation Radar (OPRA) at Locarno‐Monti, Switzerland during the Mesoscale Alpine Programme (MAP) Intensive Observing Periods (IOPs) 2b and 8 are examined to characterize the fine‐scale precipitation structure. The relative roles of collection of cloud water by raindrops versus collection of cloud water by ice particles (riming) in the same column are assessed with a one‐dimensional (1D) Kessler water‐continuity model using the observed data characteristics as input.