摘要
BasedontheTropicalCyclone(TC)YearbooksdataandJRA-25reanalysisdatafromtheJapanMeteorologicalAgency(JMA)during1979-2008,dynamiccompositeanalysisandcomputationofkineticenergybudgetareusedtostudytheintensifyingandweakeningTCsduringExtratropicalTransitionoverChina.TheTCIshowsstrongupper-leveldivergence,strengthenedlow-levelconvergenceandsignificantlyenhancedupwardmotionundertheinfluenceofstrongupper-leveltroughsandhigh-leveljets.TheTCIiscorrespondinglyintensifiedafterExtratropicalTransition(ET);TCWexhibitsstrongupper-leveldivergence,subduedlow-levelconvergenceandslightlyenhancedupwardmotionundertheinfluenceofweakupper-leveltroughsandhigh-leveljets.ItthenweakensafterET.Theincrease(decrease)ofthegenerationofkineticenergybydivergencewindinTCI(TCW)atlowlevelisoneofthemajorreasonsforTCI’sintensification(TCW’sweakening)aftertransformation.Thegenerationofkineticenergybydivergencewindiscloselyrelatedtothedevelopmentofalow-levelbaroclinicfrontalzone.ThegrowthofthegenerationofkineticenergybyrotationalwindinTCIatupperlevelisfavorableforTCI’smaintenance,whichisaffectedbystrongupper-leveltroughs.ThedissipationofthegenerationofkineticenergybyrotationalwindinTCWatupperlevelisunfavorableforTCW’smaintenance,whichisaffectedbyweakupper-leveltroughs.
出版日期
2015年01月11日(中国期刊网平台首次上网日期,不代表论文的发表时间)