Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1017/S1350482706002404 |
Synoptic characteristics of dust storms observed in Inner Mongolia and their influence on the downwind area (the Beijing-Tianjin Region) | |
Gao Tao; Xu Yongfu; Bo Yuhua; Yu Xiao | |
通讯作者 | Gao Tao |
来源期刊 | METEOROLOGICAL APPLICATIONS
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ISSN | 1350-4827 |
EISSN | 1469-8080 |
出版年 | 2006 |
卷号 | 13期号:4页码:393-403 |
英文摘要 | Springtime meteorological and satellite data from 1971 to 2000 have been used to assess surface desertification and grassland deterioration to obtain a better understanding of the synoptic characteristics of dust storms observed in Inner Mongolia, the relationship between dust storms and their impact on the Beijing-Tianjin Region, and the effect of climatic change on the surface environment of dust storm source areas in Inner Mongolia. Based on the statistics and the analysis of weather charts during each dust storm event, details and characteristics of sand and dust source regions, such as cold air paths, areas of strong winds and typical synoptic types were obtained. Temperature was found to be the most significant indicator of climate change in the dust storm source regions, having increased by 1.01 degrees C in the Alxa source region and by 0.96 degrees C in Hunshdak over the past three decades. Other factors include lack of precipitation, higher evaporation, lower relative humidity, soil desertification and decrease of grasslands in the source regions. As a consequence, nearly two-thirds of the very strong dust storm events observed in Inner Mongolia (characterised by horizontal visibility below 1000 m and wind speeds of 12 m s(-1) or over) led to suspended dust or dust storms in the downwind area, the Beijing-Tianjin Region. This study also analyses the upper air and surface weather charts of 58 very strong dust storm events and established the direction of three cold air paths: northwesterly, westerly and northerly. The northwesterly cold air path is seen as the major one, responsible for 58.6% of the dust storm episodes. In addition, the observed areas where strong winds occur lie mostly across the central-west and central regions of Inner Mongolia. Finally, the synoptic situations associated with dust storm events can be classified into three types: trough, northwesterly current and Mongolian vortex. The predominant synoptic system is the trough, responsible for 63.8% of the 58 events analysed in this study. |
英文关键词 | dust storms suspended dust weather Inner Mongolia synoptic characteristics cold air paths sand and dust source regions surface environment |
类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
收录类别 | SCI-E |
WOS记录号 | WOS:000244308900008 |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
来源机构 | 中国科学院大气物理研究所 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/152492 |
作者单位 | (1)Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Atmospher Boundary Layer Phys & Atm, Beijing 100029, Peoples R China;(2)Inner Mongolia Meteorol Inst, Hohhot 010051, Peoples R China;(3)Comp Applicat Acad Inner Mongolia, Hohhot 010010, Peoples R China |
推荐引用方式 GB/T 7714 | Gao Tao,Xu Yongfu,Bo Yuhua,et al. Synoptic characteristics of dust storms observed in Inner Mongolia and their influence on the downwind area (the Beijing-Tianjin Region)[J]. 中国科学院大气物理研究所,2006,13(4):393-403. |
APA | Gao Tao,Xu Yongfu,Bo Yuhua,&Yu Xiao.(2006).Synoptic characteristics of dust storms observed in Inner Mongolia and their influence on the downwind area (the Beijing-Tianjin Region).METEOROLOGICAL APPLICATIONS,13(4),393-403. |
MLA | Gao Tao,et al."Synoptic characteristics of dust storms observed in Inner Mongolia and their influence on the downwind area (the Beijing-Tianjin Region)".METEOROLOGICAL APPLICATIONS 13.4(2006):393-403. |
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