SEASONAL TRANSITION OF EAST ASIAN SUBTROPICAL MONSOON AND ITS POSSIBLE MECHANISM

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摘要 TheNCEP/NCARreanalysisdatasetsandClimatePredictionCenter(CPC)MergedAnalysisofPrecipitation(CMAP)raindataareusedtoinvestigatethelargescaleseasonaltransitionofEastAsiansubtropicalmonsoon(EASM)anditspossiblemechanism.ThekeyregionofEASMisdefinedaccordingtotheseasonaltransitionfeatureofmeridionalwind.Bycombiningthe’thermalwind’formulaandthe’thermaladaptation’equation,anew’thermal-wind-precipitation’relationisdeduced.Theareameanwinddirectionsandthermaladvectionsindifferentseasonsareanalyzedanditisshownthatinsummer(winter)monsoonperiod,theaveragedwinddirectionintheEASMregionvariesclockwise(anticlockwise)withaltitude,andtheEASMregionisdominatedbywarm(cold)advection.TheseasonaltransitionofthewinddirectionatdifferentlevelsandthecorrespondingmeridionalcirculationconsistentlyindicatesthatthesubtropicalsummermonsoonisestablishedbetweentheendofMarchandthebeginningofApril.Finally,aconceptualschematicexplanationforthemechanismofseasonaltransitionofEASMisproposed.
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出版日期 2012年03月13日(中国期刊网平台首次上网日期,不代表论文的发表时间)
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