摘要
通过分析 2 0 0 2年 6月 8~ 9日汉中大暴雨的环流背景、物理量场的特征及其演变 ,表明热力、水汽条件在降水开始前 2 4小时有一定的反映 ,中低层大的正涡度和高空的负涡度集中在非常狭窄的同一地区 。
Based on the analysis of the features and evolution of the circulation background,and physical quantities of the heavy rain in Hanzhong during 8-9 June 2002, it is shown that thermal and water vapor conditions in Hanzhong have changed 24 hours before raining, strong positive vorticity at the middle and low levels and strong negative vorticity at the high level overlapped in a narrow region is also a inducement of the heavy rain.
出处
《气象》
CSCD
北大核心
2003年第4期53-55,57,共4页
Meteorological Monthly