Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/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
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ISSN | 1009-637X |
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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