位涡倾向在Muifa台风路径转折中的应用  

Application of Potential Vorticity Tendency in Track Recurvature Study of Typhoon Muifa

作　　者：袁敏[1,2,3] 平凡 李国平[4] YUAN Min;PING Fan;LI Guoping(Laboratory of Cloud-Precipitation Physics and Severe Storms, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029;University of Chinese Academy of Sciences, Beijing 100049;College of Air Traffic Management, Civil Aviation Flight University of China, Guanghan, Sichan Province 618307;College of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu 610225)

机构地区：[1]中国科学院大气物理研究所云降水物理与强风暴实验室,北京100029 [2]中国科学院大学,北京100049 [3]中国民用航空飞行学院空中交通管理学院,四川广汉618307 [4]成都信息工程大学大气科学学院,成都610225

出　　处：《大气科学》2018年第2期281-291,共11页Chinese Journal of Atmospheric Sciences

基　　金：国家自然科学基金项目Y41301E801;U1333130~~

摘　　要：利用ECMWF资料诊断分析了位涡倾向方程中的水平平流项和非绝热加热项分别在Muifa台风两次路径转折中的作用。结果表明:第一次路径转折过程中,非绝热加热项的量级比水平平流项小一个量级,水平平流项所表征的外部大尺度环流因素是第一次路径转折的主要原因;第二次路径转向过程由水平平流项和非绝热加热项共同控制,其中水平平流项控制台风的移向,非绝热加热项表征的内部非对称结构对台风转向有抑制作用。Horizontal advection and diabatic heating terms in the potential vorticity tendency equation are used to diagnose the twice track changes of typhoon Muifa based on ECMWF data. The results show that horizontal advection is about one order of magnitude larger than diabatic heating; large-scale steering flows represented by horizontal advection mainly contributed to the first track change; horizontal advection and diabatic heating both contributed to the second track change, while horizontal advection controlled the direction and diabatic heating restrained its track recurvature.

关 键 词：位涡倾向 水平平流项 非绝热加热项 非对称结构 

分 类 号：P444[天文地球—大气科学及气象学]