简介:Therelationshipbetweentheauroralovalpattern,i.e.,location,size,shape,andintensity,andtheauroralelectrojetactivityindex(AEindex)isstudied.Itisfoundthatthemaximalauroralintensityisellipticallydistributed,andthelengthsofsemimajorandsemiminoraxesarepositivelycorrelatedtoAE.TheintensityalongthenormaloftheauroralovalcanbesatisfyinglydescribedbyaGaussiandistribution,andthemaximumandthefullwidthathalfmaximumoftheGaussiandistributionarebothpositivelycorrelatedtoAE.Basedonthesestatisticalresults,aseriesofexperimentalformulasasafunctionofAEaredevelopedtocalculatethelocation,size,shape,andintensityoftheauroraloval.TheseformulasarevalidatedbytheauroralimagesreleasedbySWPC/NOAA.
简介:StormsthatoccurattheBayofBengal(BoB)areofabimodalpattern,whichisdifferentfromthatoftheotherseaareas.ByusingtheNCEP,SSTandJTWCdata,thecausesofthebimodalpatternstormactivityoftheBoBarediagnosedandanalyzedinthispaper.TheresultshowsthattheseasonalvariationofgeneralatmospherecirculationinEastAsiahasaregulatingandcontrollingimpactontheBoBstormactivity,andthe'bimodalperiod'ofthestormactivitycorrespondsexactlytotheseasonalconversionperiodofatmosphericcirculation.Theminorwindspeedofshearspringandautumncontributedtothestorm,whichwasacrucialfactorforthegenerationandoccurrenceofthe'bimodalpattern'stormactivityintheBoB.Theanalysisonseasurfacetemperature(SST)showsthattheSSTsofalltheyeararoundintheBoBareameettheconditionsrequiredforthegenerationoftropicalcyclones(TCs).However,theSSTsinthecentralareaofthebayarehigherthanthatofthesurroundingareasinspringandautumn,whichfacilitatestheoccurrenceofa'two-peak'stormactivitypattern.Thegenesispotentialindex(GPI)quantifiesandreflectstheenvironmentalconditionsforthegenerationoftheBoBstorms.ForGPI,theintenselow-levelvortexdisturbanceinthetroposphereandhigh-humidityatmospherearethesufficientconditionsforstorms,whilelargemaximumwindvelocityofthegroundvortexradiusandsmallverticalwindsheararethenecessaryconditionsofstorms.
简介:Theeffectoflocalbasicflowstructurepattern(BFSP)onablockinghighformationisinvestigatedwithintheframeworkofforceddissipationKDVdynamics.Thezonalandmeridionalpositionsofthehigh’scenterexcitedbyaheatsourcedependontheBFSPselected.
简介:Limitationsofdifferencemapsshowingcirculationanomaliesareanalyzed,andthedefinitionofthelocalpatternanaloguecoefficient(LPAC)isgiventogetherwiththeprocedureforconstructingsuchamap,followedbyanexampleillustratingitsusefulapplicationincirculationanomaly.
简介:许多有缺点的雷达回响可以用雷达数据应用,特别雷达数据吸收和量的降水估计引起严重问题。在这研究,测试模式在CINRAD(中国新一代天气雷达)由测试信号或雷达硬件失败引起了SA和SB雷达运作的观察被调查。为了把测试模式与雷达回响的另外的类型区分开来,例如降水,清除空气和另外的非气象学的回响,包括有效反射率数据百分比(RZ)的五个特征参数,速度RF(合拢的范围)数据百分比(RRF),失踪的速度数据百分比(RM),平均沿着方位角反射率变化$\left({R_{N_{r,Z}}}\right)$并且平均沿着横梁反射率变化$\left({R_{N_{一,Z}}}\right)$被建议。基于模糊逻辑方法,一个测试模式鉴定算法被开发,并且从雷达回响的所有不同类型的统计结果显示算法的表演。有在测试模式内定位的重降水回响的二个典型箱子的分析被执行。统计结果证明测试模式鉴定算法表现很好,自从测试模式在大多数情况中被认出。而且,算法能有效地移开测试模式信号并且在重降雨事件保留强壮的降水回响。
简介:Bymeansofsimulationexperimentswithatwo-dimensionalzonal-meanmodel,astudyismadeoftheinfluenceofthewesternNorth-Pacificmidlatitudesea-surfacetemperature(SST)anomaliesonthecirculationpatternandwet-seasonalprecipitationovertheEast-ChinaChangjiang-HuaihereachesandtheNorth-Chinaplain.TheSSTanomaliesaredividedintotwotypes,onebeing“colderinthesouthandwarmerinthenorth”andtheotherjustopposite,dependingonseason.Resultsshowthattheoccurrenceoftheanomaliesisfollowedbyconsiderablechangesinthepositionofthesubtropicalhighhappeningfor3-5monthstocome.Forinstance,thespring“colderinthesouthandwarmerinthenorth”anomaloustype(i.e.,colderfor20—35°N,andwarmernorthof35°N)leadstotheintensificationofthesummersubtropicalhigh,withtheridgelinemovedslightlynorthward,resultingindroughtoverChangjiangreachesforJuly-AugustandinexcessiverainfallintheNorth-Chinaplain,andviceversa.
简介:Earlyproxy-basedstudiessuggestedthattherepotentiallyoccurreda"southerndrought/northernflood"(SDNF)overEastChinainthemid-Holocene(fromroughly7000to5000yearsbeforepresent).Inthisstudy,weusedbothglobalandregionalatmosphericcirculationmodelstodemonstratethattheSDNF—namely,theprecipitationincreasesoverNorthChinaanddecreasesoverthethelowerreachesoftheYangtzeRiverValley—couldhavetakenplaceinthemid-Holocene.WefoundthattheSDNFinthemid-HolocenewaslikelycausedbythelowerSSTinthePacific.TheloweredSSTandthehigherairtemperatureovermainlandChinaincreasedtheland–seathermalcontrastand,asaresult,strengthenedtheEastAsiansummermonsoonandenhancedtheprecipitationoverNorthChina.