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云南暴雨涡散场动能转换函数的动态分析
引用本文:段旭,尤卫红,许美玲. 云南暴雨涡散场动能转换函数的动态分析[J]. 热带气象学报, 1999, 15(2): 186-191
作者姓名:段旭  尤卫红  许美玲
作者单位:云南省气象台!昆明,650034
摘    要:对1996年云南主汛期(6-8月)逐日散度风动能和旋转风动能之间的转换函数C(KD,KR)特征进行深入研究,同时分析了C(KD,KR)各项Af、Az、B、C在动能转换函数中所起的作用。研究结果表明,对流层内C(KD,KR)>0,同时对流层低层的C(K,KR)>中高层的C(KD,KR)之和.极易出现暴雨过程;Af项在整个动能转换中起主要作用,71%的Af与C(KD,KR)具有相同的符号,Az项和B项在动能转换中起振荡作用,Az+B控制着29%的动能转换方向。

关 键 词:动能转换  涡散场  函数  暴雨
收稿时间:1998-04-27
修稿时间:1998-06-29

THE DYNAMICAL ANALYSES FOR THE CHARACTERISTICS OF DIVERGENT AND ROTATIONAL COMPONENTS OF KINETIC ENERGY FOR HEAVY RAIN IN YUNNAN
Duan Xu,You Weihong and Xu Meiling. THE DYNAMICAL ANALYSES FOR THE CHARACTERISTICS OF DIVERGENT AND ROTATIONAL COMPONENTS OF KINETIC ENERGY FOR HEAVY RAIN IN YUNNAN[J]. Journal of Tropical Meteorology, 1999, 15(2): 186-191
Authors:Duan Xu  You Weihong  Xu Meiling
Affiliation:Yunnan Meteorological Observatory, Kunming, 650034;Yunnan Meteorological Observatory, Kunming, 650034;Yunnan Meteorological Observatory, Kunming, 650034
Abstract:This paper further studies the kinetic energy conversion function in the flood season(June toAugust) in 1996,and analyses effects on C(KD,KR) by terms Af, Az, B, C. The results showthat heavy rain processes will occur if C(KD,KR)>0 and C(KD,KR) in the lower torpephericlayers is larger than the sum of C(KD,KR) in the middle and high tropepheric layers. Term Afacts the main role in the kinetic energy conversion. 71% of signs of term Az are the same as that of C(KD,KR). Terms Az and B act to vibrate in the kinestic energy conversion. 29% of signs of the sum of terms Az and B are the same as C(KD,KR).
Keywords:Kinetic energy conversion Divergent and rotational components Function Heavy rain
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