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Rainfall events and Hailstorms Analysis Program (RHAP)

机译:降雨事件和雹暴分析计划(RHAP)

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RHAP (Rainfall events and Hailstorms Analysis Program) is a new tooldesigned for analysing rainfall events and hailstorms. The aim of thiscontribution is to present the RHAP tool, which is under development, andits application to different hailstorms and rainfall episodes. The programassimilates multiple data bases (meteorological radar, meteorological modeloutputs, radiosondes and surface observations) with the purpose to getbetter event reanalysis. It is based on Storm Cell Identification andTracking Algorithm (SCIT) with an improved version of the method, and alsoon a new 2-D algorithm which automatically identifies and classifies theprecipitation systems distinguishing between Mesoscale Convective Systems,Multicellular systems, Isolated convection, Stratiform precipitation andConvective precipitation embedded in stratiform precipitation. These twomethods allow to obtain the 2-D and 3-D features of the precipitation systemlike top height of the cells, maximum reflectivity, Vertical IntegratedLiquid content (VIL) and VIL density (VILD), kinetic energy, severe hailprobability (SHP), number of 3-D cells exceeding a given threshold, Z/Rrelations,... that are useful to analyse both heavy rainfall and hailevents. As application, two events produced on NE Spain are discussed: theheavy rainfall event recorded on 6 September 2004, characterised by agreat number of cells that crossed the affected area and that had a maximumactivity associated to high values of VIL(37.5 kg/m2), Zmax (54 dBZ) andSHP (73%); and the hail event produced on 29 August 2004, with a rapiddevelopment of the convective system and with hail observations in surfacewhen the following thresholds were exceeded: Zmax=54 dBZ, VIL=25 kg/m2 and SHP=63%.
机译:RHAP(降雨事件和雹暴分析程序)是设计用于分析降雨事件和冰雹的新工具。该文稿的目的是介绍正在开发的RHAP工具,并将其应用于不同的冰雹和降雨事件。该程序将多个数据库(气象雷达,气象模型输出,无线电探空仪和地面观测)相结合,目的是更好地重新分析事件。它基于风暴信元识别和跟踪算法(SCIT),具有改进的方法,并且基于新的二维算法,可自动识别并分类降水系统,以区分中尺度对流系统,多细胞系统,孤立对流,层状降水和对流降水嵌入层状降水中。这两种方法可以获取沉淀系统的2-D和3-D特征,例如细胞的顶部高度,最大反射率,垂直积分液体含量(VIL)和VIL密度(VILD),动能,严重的易失性(SHP),数量超过给定阈值Z / Rrelations的3-D单元,可用于分析暴雨和大风量。作为应用,讨论了西班牙东北部发生的两个事件:2004年9月6日记录的大降雨事件,其特征是越过受影响区域的细胞总数越多,并且具有与高VIL值(37.5 kg / m 2 ),Z max (54 dBZ)和SHP(73%);以及2004年8月29日发生的冰雹事件,这是对流系统的快速发展,并且在超过以下阈值时在地面上出现冰雹观测:Z max = 54 dBZ,VIL = 25 kg / m 2 和SHP = 63%。

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