摘要
Theinfluenceoftheinterannualvariationofcross-equatorialflow(CEF)ontropicalcyclogenesisoverthewesternNorthPacific(WNP)isexaminedinthispaperbyusingthetropicalcyclone(TC)besttrackdatafromtheJointTyphoonWarningCenterandtheJRA-25reanalysisdataset.TheresultsshowedthatthenumberofTCsformingtotheeastof140°EoverthesoutheasternpartofthewesternNorthPacific(WNP)isinhighlypositivecorrelationwiththevariationoftheCEFnear125°Eand150°E,i.e.,thenumberoftropicalcyclogenesesincreaseswhenthecross-equatorialflowsarestrong.CompositeanalysesshowedthatduringtheyearsofstrongCEF,thevariationsofOLR,verticalwindshearbetween200-850hPa,850hParelativevorticityand200hPadivergencearefavorablefortropicalcyclogenesistotheeastof140°EoverthetropicalWNP,andviceversa.Moreover,itisalsodiscussedfromtheviewofbarotropicenergyconversionthatduringtheyearsofstrongCEF,aneastward-extendedmonsoontroughleadstotherapidgrowthofeddykineticenergyovertheeasternpartofWNP,whichisfavorablefortropicalcyclogenesis;butduringtheyearsofweakCEF,themonsoontroughislocatedwestwardinthewesternpartoftheWNP,consistentwiththegrowthareaofeddykineticenergy.Asaresult,therearefewerTCgenesesovertheeasternpartofWNP.Besides,theabruptstrengtheningofaclose-byCEF2-4daysbeforetropicalcyclogenesismaybetheoneofitstriggers.
出版日期
2017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)