固阳“6·13”强对流天气过程成因分析  

The Cause Analysis on Severe Convection Weather Process of Guyang "6 o 13"

作　　者：刘澜波[1] 王明力[1] 黄炜[1] 张慧[1] 李岩[1] 

机构地区：[1]包头市气象局,内蒙古包头014030

出　　处：《内蒙古气象》2013年第5期6-7,共2页Meteorology Journal of Inner Mongolia

摘　　要：2011年6月13日发生在固阳县的强对流天气系统具有尺度小、突发性、变化迅速等特点,采用常规的观测手段和预报方法常常难以监测和预报,文章采用将多普勒雷达资料与中尺度模式提供的资料相结合的方法来探讨强对流天气的成因。The severe convection weather system that happened in Guyang county had the characteristics of small-scale, burstiness, rapid variation, etc. It was difficult to monitoring and forecast by conventional observation means and forecast methods. The article adopted the combinational methods of Doppler radar data and mesoscale pattern data to discuss the cause of the severe convection weather.

关 键 词：强对流天气 成因 分析 

分 类 号：P458.121[天文地球—大气科学及气象学]