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Modern dust storms in China: an overview 总被引:4,自引:0,他引:4
This paper discusses the sources, spatial distribution, frequency and trend of dust storms in China. Most dust storms in China originate from one of three geographic areas: the Hexi (River West) Corridor and western Inner Mongolia Plateau, the Taklimakan Desert, and the central Inner Mongolia Plateau. Dust is most likely from deteriorated grasslands, Gobi, alluvial, lacustrine sediments and wadis at the outer edge of deserts. But deserts themselves contribute only slightly to the dust storm directly. Two geographic areas frequently have dust storms: one is in the western Tarim Basin, a ground surface of deteriorated land and wadi, but it only affects its neighboring areas, and the other one is in the western Inner Mongolia Plateau, a ground surface of Gobi, alluvial and lacustrine sediments, but it causes most of the dust storms in north China. Generally speaking, dust storms have reduced in most regions of China from the 1950 to 2000. Dust storms are highly correlated with human activities and climate changes. 相似文献
12.
We give an outline of the scientific-methodological principles of using the regional-typological approach in geographical research. Based on analyzing cartographic products, we demonstrate the differences in understanding and implementing the approach. The structurallogical schematic diagram for the regional-typological approach has been developed, which opens up possibilities for its implementation in the study and mapping of geosystems and can provide an integral, systemic idea of this approach. 相似文献
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