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投稿时间：2009-01-03 修订日期：2009-07-20
投稿时间：2009-01-03 修订日期：2009-07-20
中文摘要: 应用NCEP再分析资料，计算分析了台风凤凰发生和发展过程中的积云对流潜热加热和海面感
热通量。表明：感热释放通过海气相关作用使海面风及对流层涡度增强,可能是台风初始低
压的形成机制；积云对流潜热释放不但使台风中心增暖并使台风中间层上升运动增强，从而
促使台风加强和发展，因此，对流凝结潜热是台风凤凰维持和发展的主要热力和动力因子。
Abstract:With the NCEP reanalysis data, the cumulus convect
ive latent heating and the sea surface sensible heat flux in the cours
e of the development of Typhoon Fung Wong are analyzed. It shows that through t
he air sea interaction,
the sensible heat release strengthened the sea surface wind and tropospheric vor
ticity, which may be the possible cause for the initial low pressure of typhoon;
the cumulus convective latent heat not only heated the center of typhoon but al
so reinforced the ascending motion at middle levels,thereby made it increase a
nd develop. The convective condensation latent heat is considered to be the majo
r thermal and dynamic factor for the development of Typhoon Fung wong.
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引用文本：
刘裕禄,方祥生,金飞胜,方素青,2009.台风凤凰形成发展过程中对流凝结潜热和感热的作用[J].气象,35(12):51-57.
Liu Yulu,Fang Xiangsheng,Jin Feisheng,Fang Suqing,2009.Effects of Sensible Heat and Convective Condensation Latent Heat on Typhoon Fung Wong During the Course of Its Formation and Development[J].Meteor Mon,35(12):51-57.
刘裕禄,方祥生,金飞胜,方素青,2009.台风凤凰形成发展过程中对流凝结潜热和感热的作用[J].气象,35(12):51-57.
Liu Yulu,Fang Xiangsheng,Jin Feisheng,Fang Suqing,2009.Effects of Sensible Heat and Convective Condensation Latent Heat on Typhoon Fung Wong During the Course of Its Formation and Development[J].Meteor Mon,35(12):51-57.