一次特大暴雨过程的中尺度低压特征及发展因子分析

Features and Development Factors of Two Types of Meso-scale Low in an Excessive Heavy Rain Event

1.Unit 95871,PLA,Hengyang 421001;2.Meteorology Institute,PLAUST,Nanjing 211101;3.State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100081

摘要: 以2008年6月12日广西特大暴雨为例,使用2008年华南野外暴雨试验获取的地面降水资料和LAPS 0.045°×0.045°再分析资料,采用带通滤波方法提取暴雨过程中的中尺度系统,对中尺度低压进行分类:第一类中尺度低压先于降水产生,第二类则
- 中尺度低压 /
- 雨团 /
- 垂直结构 /
- 发展因子
Abstract: Taking an excessive heavy rain event which occurred in Guangxi on 12 June 2008 for example,based on the surface precipitation data and the LAPS 0.045°×0.045°data collected in the SCHeREX,the meso-scale disturb
- Meso-scale low /
- Rain mass /
- Evolution /
- Vertical structure