摘要
选取云南暴雨和非暴雨两类天气过程,分别应用涡散场能量收支方程,计算了暴雨区面积-时间平均能量收支各项量值,给出了对流层整层和上(200~400hPa)、中(400~600hPa)、下(600~800hPa)各层的涡散场动能源汇特征,同时还指出了两类天气在动能制造、能量转换等方面存在的较大差异。
By using budget equations for rotational and divergent components of kinetic energy,the area-time averages of each term are computed for 200~400,400~600,600~800 hPa layers to describe energetics of the lower,middle and upper troposphere for heavy rain and no-heavy rain processes The results show that the generation,conversion and transport for divergent components of kinetic energy are different and the signs of the major energy budget are opposite in heavy rain and no-heavy rain processes
出处
《高原气象》
CSCD
北大核心
1997年第2期204-209,共6页
Plateau Meteorology
关键词
暴雨
能量收支
涡散场
暴雨过程分析
Heavy rain No-heavy rain Energy budget Transport Divergent and rotational components