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JOURNAL OF DESERT RESEARCH  2014, Vol. 34 Issue (6): 1605-1616    DOI: 10.7522/j.issn.1000-694X.2014.00018
    
Analysis of the Mechanism and Transmission of Dust in Northwest China Based on Satellite Remote-sensing Data
Liu Dan, Zhang Wu, Chen Yan, Yan Jiaolong
College of Atmospheric Sciences/Key Laboratory for Semi-Arid Climate Change of the Ministry of Education, Lanzhou University, Lanzhou 730000, China
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Abstract  The vertical distribution and transmission paths of dust aerosol in three cases of sandstorms in late April in 2009, 2010 and 2011 were analyzed using a combination of satellite remote sensing data of CALIOP/CALIPSO and OMI/Aura, as well as a HYSPLIT trajectory model. The results show that the Mongolia cyclone and cold front were the main systems causing the dust events. In mixed weather system, dust aerosol were mainly distributed in 0-7 km, and moved from west to east; in the pure cold front weather system, they were mainly distributed in 0-4 km, moving from west to southeast. The dust particles were located above 3 km with depolarization ratio about 0.5 and color ratio about 1.0 or higher in the most intense development of two weather systems; In the weakened period of sandstorm dust aerosols located in 0-2 km, with depolarization ratio about 0.3 and color ratio about 0.8. In mixed weather, the vertical distribution of dust aerosol located in 3-7 km was higher by comparison with in pure cold front.
Key words:  dust aerosol      CALIOP/CALIPSO      vertical distribution      aerosol index      HYSPLIT trajectory model     
Received:  13 December 2013      Published:  20 November 2014
ZTFLH:  P445.4  
Corresponding Authors:  张武(Email:wzhang@lzu.edu.cn)     E-mail:  wzhang@lzu.edu.cn
Articles by authors
Liu Dan
Zhang Wu
Chen Yan
Yan Jiaolong

Cite this article: 

Liu Dan, Zhang Wu, Chen Yan, Yan Jiaolong. Analysis of the Mechanism and Transmission of Dust in Northwest China Based on Satellite Remote-sensing Data. JOURNAL OF DESERT RESEARCH, 2014, 34(6): 1605-1616.

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http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2014.00018     OR     http://www.desert.ac.cn/EN/Y2014/V34/I6/1605

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