An observational study of aerosol and turbulence properties during dust storms in Northwest China

摘要：

1.Introduction Commonly in late winter and spring, as cold and dry continental polar air mass from northern latitudes moves southward or south-southeastward to exchange heat and moisture with warm and moist air mass at lower latitudes, the two different air masses meet in Mongolia or Inner-Mongolia of China to form the cold front or cold air outbreak (Wang,et al.,2008,Sun et al,2001).Given suitable atmospheric conditions, the strong surface winds associated with the baroclinic system of cold front lift dust from the dry sandy surface of the deserts in western China produce so-called Asian Dust Storms (ADS).

作者: Peijian Fu Shiyuan Zhong Jianping Huang Guangning Song

作者单位: Key Laboratory of Arid and Semi-Arid Climate,Ministry of Education,China College of Atmospheric Scie Department of Geography and Center for Global Climate Change and Earth Observations,Michigan State U

会议类型: 国内会议

会议名称: 第九届海峡两岸沙尘与环境治理学术研讨会

会议地点: 呼和浩特

会议语种:英文

页码: 238-255

在线出版日期: 2012-07-23（万方平台首次上网日期，不代表论文的发表时间）