CAJ | 학술논문

对2011年2月6～9日钦州市连续性大雾天气过程进行分析,结果表明：有利的大气环流形势为大雾形成提供有利天气背景;持续的东南风和适宜的风速为大雾的形成提供了有利水汽条件;与稳定度有关的物理量场及与水汽条件有关的相对湿度场对预报大雾天气有一定的指导意义;逆温层结对水汽的聚集有重要贡献。
대2011년2월6～9일흠주시련속성대무천기과정진행분석,결과표명：유리적대기배류형세위대무형성제공유리천기배경;지속적동남풍화괄의적풍속위대무적형성제공료유이수기조건;여은정도유관적물리량장급여수기조건유관적상대습도장대예보대무천기유일정적지도의의;역온층결대수기적취집유중요공헌。
Basing the continuous fogs in Qinzhou city on February 6-9,2011,the synoptic situation and meteorological physical fields were analyzed.The results show that synoptic situation provides the favorable background to fog formation.And continuous southeast wind and appropriate wind speed provide fogs the favorable water vapor conditions.The physical quantities relating to atmospheric stability and the relative humidity have some significance to the fog forecast.Thermal inversion layer has important contribution to water vapor aggregation.