学科分类
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3 个结果
  • 简介:纸从6月7日把卫星红外影像的黑身体的日平均值温度的分布给10,1998在HUAMEX期间并且检验14中央--α-放大对流系统和很多个中央--β-在1-h间隔用卫星红外影像放大对流系统。中央在6月7日放大对流系统并且9,它在台湾的中间和珍珠河(ZhujiangR.)的河口区域上导致了严重暴风雨,强烈地被分析。中央的连续开发放大对流系统被卫星红外影像的黑身体温度的分布揭示。许多中央连续地在放大对流系统的环境条件发生了被诊断。设想的工具,LiveView,在上面、更低的水平风之间的连接回答的显示和垂直发行量和湿空气的3-dimensional轨道打手势,基于客观分析的数据。

  • 标签: RAINSTORM MESOSCALE CONVECTIVE system environmental conditions
  • 简介:ThisstudyinvestigatesclassificationanddiurnalvariationsoftheprecipitationechoesoverthecentralTibetanPlateaubasedontheobservationscollectedfromaC-bandvertically-pointingfrequency-modulatedcontinuous-wave(C-FMCW)radarduringtheThirdTibetanPlateauAtmosphericScientificExperiment(TIPEX-Ⅲ)2014-IntensiveObservationPeriod(2014-IOP).Theresultsshowthat51.32%oftheverticalprofileshavevalidechoeswithreflectivity>-10dBZ,and35.06%ofthevalidechoprofilesproduceprecipitationattheground(precipitationprofiles);stratiformprecipitationwithanevidentbright-bandsignature,weakconvectiveprecipitation,andstrongconvectiveprecipitationaccountfor52.03%,42.98%,and4.99%oftheprecipitationprofiles,respectively.About59.84%oftheprecipitationoccursintheafternoontomidnight,while40.16%oftheprecipitationwithweakerintensityisobservedinthenocturnalhoursandinthemorning.Diurnalvariationofoccurrencefrequencyofprecipitationshowsamajorpeakduring2100-2200LST(localsolartime)with59.02%beingthestratiformprecipitation;thesecondarypeakappearsduring1300-1400LSTwith59.71%beingtheweakconvectiveprecipitation;thestrongconvectiveprecipitationoccursmostly(81.83%)intheafternoonandeveningwithtwopeaksover1200-1300and1700-1800LST,respectively.Startingfromapproximately1100LST,precipitationechoesdevelopwithenhancedverticalairmotion,elevatedechotop,andincreasingradarreflectivity.Intenseupwardairmotionoccursmostfrequentlyin1700-1800LSTwithasecondarypeakin1100-1400LST,whilethetopsofprecipitationechoesandintenseupwardairmotionreachtheirhighestlevelsduring1600-1800LST.Theatmosphericconditionsintheearlymorningaredisadvantageousforconvectiveinitiationanddevelopment.Aroundnoon,theconvectiveavailablepotentialenergy(CAPE)increasesmarkedly,convectiveinhibition(CIN)isgenerallysmall,andasuper-dry-adiabaticlayerispresentnear

  • 标签: TIPEX-Ⅲ vertically-pointing RADAR precipitation ECHOES DIURNAL