Sand-dust storms in China: temporal-spatial distribution and tracks of source lands (original) (raw)
Abstract
Sand-dust storm is a special natural disaster that frequently occurs in deserts and their surrounding areas. With the data published on_Surface Meteorological Monthly Bulletin_ and_Surface Chart_ during 1971–1996, the temporal-spatial distribution and annual variation of sand-dust storms are analyzed on the basis of the case study of atmospheric processes. Furthermore, the tracks and source areas of sand-dust storms are determined with the aid of GIS. The results show that except some parts of Qinghai Province and Inner Mongolia as well as Beijing, sand-dust storms decrease apparently in time and space in recent decades in China. Sand-dust storms occur most frequently in spring, especially in April. According to their source areas, sand-dust storms are classified into two types, i.e., the inner-source and outer-source sand-dust storms. Most of the outer-source sand-dust storms move along the north and west tracks. The north-track outer-source sand-dust storms always intrude into China across the Sino-Mongolian border from Hami, a city in the eastern part ofXinjiang, to Xilin Gol, a league in Inner Mongolia, while the west-track ones intrude into China from both southern and northern Xinjiang. The source lands of inner-source sand-dust storms concentrate in the Taklimakan Desert and its surrounding areas in southern Xinjiang, southern part of the Junggar Basin in north of Xinjiang, the Hexi Corridor in western Gansu Province, the dry deserts of Inner Mongolia and the Qaidam Basin in Qinghai.
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Authors and Affiliations
- Urban & Resource Department, Nanjing University, 210009, Nanjing, China
Qiu Xin-fa - Department of Environmental Science, Nanjing Institute of Meteorology, 210044, Nanjing, China
Zeng Yan & Miao Qi-long
Authors
- Qiu Xin-fa
- Zeng Yan
- Miao Qi-long
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Correspondence toQiu Xin-fa.
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Xin-fa, Q., Yan, Z. & Qi-long, M. Sand-dust storms in China: temporal-spatial distribution and tracks of source lands.J. Geogr. Sci. 11, 253–260 (2001). https://doi.org/10.1007/BF02892308
- Received: 20 February 2001
- Accepted: 01 April 2001
- Issue date: July 2001
- DOI: https://doi.org/10.1007/BF02892308