摘要
通过分析2005年初春新疆温泉县出现的一次较罕见的持续性大雾天气发现:由于气温迅速回升、冬季偏厚的积雪迅速融化,在特定的天气形势及本地特殊的地形地貌影响下,水汽长时间达到饱和是此次大雾天气持续存在的主要原因。
Based on the analysis of a durative heavy fog happened during early spring in 2005, which was rare to be seen in Wenquan county, Bole, Xinjing. It was revealed that local air temperature lifted rapidly, the thick snow in winter melted all of sudden, regional unique terrain and ground feature, and the particular synoptic position as well as the local big saturation of water vapor led up to this durative heavy fog.
出处
《新疆气象》
2006年第6期6-8,共3页
Bimonthly of Xinjiang Meteorology
关键词
大雾
天气形势
地形
the analysis of heavy fog
durativet heavy fog
weather situation
unique terrain
