摘要
对2005年6月17日～23日山西出现的连续高温天气进行了诊断分析,结果表明:此次高温天气主要是由于受深厚暖高脊持续控制,后期强度增强形成河套高压,高压系统区存在较强的下沉运动引起的;同时受地面热低压东移影响,地面高温出现增幅。
Diagnostic analysis of extreme high temperature during June 17 to 23, 2005 showed that the mechanism of the event is the area has been long term controlled by worm high range which developed to the He Tao high and then the down flow influenced the temperature. And the same time the area has been influenced by the Eastward worm low which leads to the increase of high temperature.
出处
《山西气象》
2007年第1期3-5,共3页
Shanxi Meteorological Quarterly
关键词
罕见高温
河套高压
诊断
机制
Seldom High, He Tao High, diagnostic, mechanism
