CAJ | 학술논문

分析了2009年11月9日北京地区对流性降雪天气过程,冷锋是这次对流性降雪天气的天气尺度影响系统.干冷空气补充使锋面扰动增强,同时扰动上传使得中层不稳定能量释放,进而使得中尺度对流系统得到维持和发展,最终导致这次暴雪天气的出现.
분석료2009년11월9일북경지구대류성강설천기과정,랭봉시저차대류성강설천기적천기척도영향계통.간랭공기보충사봉면우동증강,동시우동상전사득중층불은정능량석방,진이사득중척도대류계통득도유지화발전,최종도치저차폭설천기적출현.
This paper analyzes the November 9, 2009, Beijing area convection sex snowfall weather process, cold front is the convectional snowfall weather weather scale influence system. Dry cold air supplement to frontal disturbance increase, and at the same time disturbance upload make middle unstable energy release, and then makes the mesoscale convective system for the maintenance and development, and ultimately lead to the emergence of the blizzard weather.