Arid
DOI10.1007/s11442-008-0415-8
Dust storms evolution in Taklimakan Desert and its correlation with climatic parameters
其他题名塔克拉玛干沙漠沙尘演变及气候因素分析
XIAO Fengjin; ZHOU Caiping; LIAO Yaoming
来源期刊Journal of Geographical Sciences
ISSN1009-637X
出版年2008
卷号18期号:4页码:415-424
英文摘要Based on the sand dust storms data and climatic data in 12 meteorological stations around sand dust storm originating areas of the Taklimakan Desert,we analyzed the trends of the number of dust storm days from 1960 to 2005 as well as their correlations with temperature,precipitation,wind speed and the number of days with mean wind speed ≥ 5 m/s.The results show that the frequency of dust storm events in the Taklimakan region decreased with the elapse of time.Except Ruoqiang and Minfeng,in the other 10 meteorological stations,the frequency of dust storm events reduces,and in 4 meteorological stations of Kuqa,Korla,Kalpin and Hotan,the frequency of dust storm events distinctly decreases.The temperature has an increasing trend,while the average wind speed and the number of days with mean wind speed ≥ 5 m/s have decreasing trends.The correlation analysis between the number of days of dust storms and climatic parameters demonstrates that wind speed and the number of days with mean wind speed ≥ 5 m/s have strong positive correlation with the number of days of dust storms,with the correlations coefficients being 0.743 and 0.720(p<0.01),respectively,which indicates that strong wind is the direct factor resulting in sand dust storms.Whereas precipitation has significant negative correlation with the number of days of dust storms(p<0.01),and the prior annual precipitation has also negative correlation,which indicates that the prior precipitation restrains the occurrence of sand dust storms,but this restraining action is weaker than the same year's precipitation.Temperature has negative correlation with the number of dust storm days,with a correlations coefficient of-0.433(p<0.01),which means that temperature change also has impacts on the occurrence of dust storm events in the Taklimakan region.
英文关键词sand dust storm climatic parameter dust storm originating area Taklimakan Desert
类型Article
语种英语
收录类别CSCD
WOS研究方向Geology
CSCD记录号CSCD:3370669
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/334985
作者单位XIAO Fengjin, Laboratory for Climate Studies; National Climate Center, Beijing 100081, China.; LIAO Yaoming, Laboratory for Climate Studies; National Climate Center, Beijing 100081, China.; ZHOU Caiping, Institute of Geographic Sciences and Natural Resources Research; CAS, Beijing 100101, China.
推荐引用方式
GB/T 7714
XIAO Fengjin,ZHOU Caiping,LIAO Yaoming. Dust storms evolution in Taklimakan Desert and its correlation with climatic parameters[J],2008,18(4):415-424.
APA XIAO Fengjin,ZHOU Caiping,&LIAO Yaoming.(2008).Dust storms evolution in Taklimakan Desert and its correlation with climatic parameters.Journal of Geographical Sciences,18(4),415-424.
MLA XIAO Fengjin,et al."Dust storms evolution in Taklimakan Desert and its correlation with climatic parameters".Journal of Geographical Sciences 18.4(2008):415-424.
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