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大连地区2009年12月29~30日寒潮天气过程分析(英文) AnalysisoftheColdWaveWeatherProcessinDalianAreafromDecember29thto30th,2009 Introduction Thecoldwaveweatherprocessisacommonnaturaleventthatoccursinvariousregionsoftheworld.Itischaracterizedbyasuddendropintemperatureandstrongwinds,whichcanhaveasignificantimpactonhumanlivesandeconomicactivities.Inthewinterof2009,theDalianareaexperiencedacoldwaveweatherprocessfromDecember29thto30th,whichwascausedbytheinfluenceofanarcticcoldairmass.Thisstudyaimstoanalyzethecharacteristicsofthiscoldwaveweatherprocessusingmeteorologicaldataandprovidesomeinsightsintothemechanismsofsuchphenomena. Weatherconditionsanddataanalysis Accordingtometeorologicaldata,thecoldwaveweatherprocessinDalianstartedonDecember28th,2009,andlasteduntilDecember30th.Duringthisperiod,thelowesttemperaturereached-15.9℃,andthehighestwindspeedwas13.2m/s.Theairtemperaturedroppedsharply,andthetemperaturewasbelowfreezingthroughouttheday.Inaddition,therewasasignificantdecreaseinatmosphericpressure.FromDecember29thto30th,themaximumvalueofatmosphericpressurewas1027.4hPa,andtheminimumvaluewas1017.6hPa,indicatingthatthearcticcoldairwasrapidlyflowingintotheDalianarea,resultinginthedecreaseofthelocalatmosphericpressure. Thedatashowedthatthewinddirectionduringthiscoldwaveweatherprocesswasmainlyfromthenorthwest,withagustywindstrengthandlongduration.Thegustywindnotonlyledtoasignificantdropintemperaturebutalsocausedsnowandiceontheroads,reducingthelevelofgroundtransportation.Moreover,thewindledtoanincreaseinthewind-chillfactor,makingtheapparenttemperaturemuchcolderthantheactualtemperature. Intermsofprecipitation,theweatherinDalianwasmainlysunnybutdryduringthiscoldwaveweatherprocess.FromDecember29thto30th,thetotalprecipitationwasonly0.2mm.Nonetheless,duetothegustywindandlowtemperatures,thedrysnowwasblownawayandformedalayerofsnowandiceontheroads,makingtheroadconditionsdangerous. Mechanismanalysis TheoccurrenceanddevelopmentofthecoldwaveweatherprocessinDalianwererelatedtotheinfluenceofthearcticcoldairandit

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