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。
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 thatof C(KD, KR). Terms Az and B act to vibrate in the kinestic energy conversion. 29% of signs ofthe sum of terms Az and B are the same as C(KD,KR).
出处
《热带气象学报》
CSCD
北大核心
1999年第2期186-191,共6页
Journal of Tropical Meteorology
关键词
动能转换
涡散场
函数
暴雨
云南
Kinetic energy conversion Divergent and rotational components Function Heavy rain
