简介：BasedonNCEP/CFSR0.5°reanalysisdataandthebesttrackdatafromtheJapanTokyoTyphoonCenter,compositeandcomparativeanalysesdemonstratetheasymmetricalstructuresofthetemperatureandhumidityintropicalcyclonesovertheWesternNorthPacificandtheSouthChinaSeafrom1979to2010.Theresultsareshownasfollows.（1）Withintensifyingtropicalcyclones,theflowfieldtendstobecomegraduallymoreaxisymmetric;however,theasymmetryofthespecifichumidityintheouterregionsismoreobvious.（2）Ingeneral,tropicalcycloneshaveanon-uniform,vertical,'doublewarm-core'structure.The'warm-cores'inthelowerlevelofweaktropicalcyclonesandinthehigherlevelofstrongtropicalcyclonesarethestrongerofthetwo.（3）Thedistributionareaofa'warm-core'isenhancedwithcycloneintensificationandtendstobecomemoreaxisymmetric.At200hPa,the'warm-core'ofaweakcyclonehasaweakanticycloneinthecenter,whereasthatofastrongcyclonehasaweakcycloneinthecenter.（4）The'wet-core'ofatropicalcycloneisprimarilylocatedinthelowerlevel（700-850hPa）.Withthecyclone’sintensification,theintensityofthe'wet-core'increasesandthescopeofthe0.8gkg-1specifichumidityanomalytendstoexpandtohigherlevels.（5）Withthecyclone’sdeepening,thepseudo-equivalentpotentialtemperatureatdifferentlevelsindifferentregionsincreases.Inaddition,thelargestwarmingratesateachintensitylevelinthedifferentregionsoccurinthecorearea,followedinturnbytheenvelopeandouterareas.