摘要
2011年"7.3"成都短时强降水是在有利的大尺度环流背景和高低空要素配合下产生的,分析常规观测资料可以预判出成都及其周边区域具有强降水发生的有利条件;地面加密自动站观测的风场辐合区对强降水的落区及移动具有指示意义,地面变压场的正负变压区表明重力波的传播和频散是中尺度系统发生发展的重要因素。
The "7.3" short -time heavy rainfall is appeared by the favourable background of large -scale circulation and meteorological element, there are some favorable conditions by analysis of the conventional observation ; the observation data of the mesoscale convergence in surface automatic meteorological station has premonitory for the heavy precipitation , the surface observation data of the positive - negative'variable pressure show the gravity wave is the important factors for the mesoscale sys- tem.
出处
《高原山地气象研究》
2012年第2期65-69,共5页
Plateau and Mountain Meteorology Research
基金
区域重大科研业务项目--西南涡诱发川渝暴雨天气机理分析研究
关键词
短时强降水
常规观测
加密自动站
中尺度特征
short -time heavy rainfall, routine observation, automatic meteorological station, mesoscale characteristics