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气象:2009,35(9):84-90
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中国东部一场持续性大雾的诊断分析
(山东省菏泽市气象局, 荷泽 274000)
Diagnostic Analysis on a Sustained Heavy Fog Event in the Eastern China
(Heze Meteorological Office, Shandong Province, Heze 274000)
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投稿时间:2008-05-28    修订日期:2009-02-27
中文摘要: 利用常规资料及NCEP 1°×1°的6小时再分析资料对2007年12月18—23日中国东部大范围大 雾进行诊 断分析,结果表明:逆温层的高度及强度与雾的浓度关系密切,弱的冷暖平流均有利于产生 雾,但是温度平流在近地面一定高度迅速逆转使得温度层结由不稳定转为稳定更利于浓雾产 生。边界层在低层辐合上升和高层辐散下沉的界面中形成逆温层,是浓雾产生的重要因素。
中文关键词:   逆温层  温度层结  温度平流
Abstract:Based on the conventional observation and NCEP reanalysis data, the synoptic ana lysis of a rare heavy fog process occurring in the eastern China was carried out. The result shows that the height and intensity of the inversion layer are related to the formati o n and status of the fog, weak cold and warm advections are both advantageous to pr oducing fog. Furthermore, the temperature advection quickly turns into reverse at some height near the surface, and thus makes temper ature stratification from unstable into stable, all these are benefical to prod uce the hea vy fog. The inversion layer which formed in the interface of ascending and desce nding movement is the important fact for producing the heavy fog.
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王玮,黄玉芳,孔凡忠,刘继敏,2009.中国东部一场持续性大雾的诊断分析[J].气象,35(9):84-90.
Wang Wei,Huang Yufang,Kong Fanzhong,Liu Jimin,2009.Diagnostic Analysis on a Sustained Heavy Fog Event in the Eastern China[J].Meteor Mon,35(9):84-90.