CAJ | 학술논문

利用常规、加密自动气象站分析了辽宁省2007年3月4日暴雪过程的天气尺度系统。结果表明，该次暴雪过程受南北2支高空槽合并加强影响，配合地面气旋稳定东移北上，低空急流的建立有利于水汽的持续输送，同时中低层的切变线提供了较好的动力条件。
이용상규、가밀자동기상참분석료요녕성2007년3월4일폭설과정적천기척도계통。결과표명，해차폭설과정수남북2지고공조합병가강영향，배합지면기선은정동이북상，저공급류적건립유리우수기적지속수송，동시중저층적절변선제공료교호적동력조건。
Conventional and confiden-tial autonomous weather stations were used to analyze the synoptic scale system of the snow storm on March 4, 2007. The results showed that this snow storm was co-influenced by the merging south and north high-level troughs, and moved northeast with the combination of ground cyclone, the low-altitude jet flow was fa-vorable for the continued conveying of water vapor, and the middle-low level shear line provided excellent dynamic conditions.