Climatological analysis of dust storms in the area surrounding the Tengger Desert during 1960-2007

被引:44
|
作者
Guan, Qingyu [1 ,2 ]
Yang, Jing [1 ,2 ]
Zhao, Shilei [1 ,2 ]
Pan, Baotian [1 ,2 ]
Liu, Chenglin [1 ,2 ]
Zhang, Di [1 ,2 ]
Wu, Tao [1 ,2 ]
机构
[1] Lanzhou Univ, Key Lab Western Chinas Environm Syst, Minist Educ, Lanzhou 730000, Gansu, Peoples R China
[2] Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 730000, Gansu, Peoples R China
基金
中国国家自然科学基金;
关键词
Tengger Desert; Dust storm; Wind; Precipitation; Temperature; NORTHERN CHINA; DIURNAL-VARIATION; SANDY LANDS; APRIL; 1998; FREQUENCY; EVENTS; ASIA; VARIABILITY; VEGETATION; MONGOLIA;
D O I
10.1007/s00382-014-2321-3
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Based on dust storm records and meteorological data from six stations in the area surrounding the Tengger Desert over the period 1960-2007, the diurnal, monthly and interannual variation of dust storms and severe dust storms, as well as their relation to wind speed, precipitation and temperature, are analyzed and discussed. Statistical analyses demonstrate that such storms occur more frequently from 9: 00 to 21: 00 local standard time and much more frequently between March and May, especially April. Dust storm frequency (DSF) and severe dust storm frequency (SDSF) show a significant linear decreasing trend from 1960 to 2007. For monthly variability, winds (especially strong ones with speeds 10-20 m/s) are the main factor controlling both dust storm types. Precipitation and temperature have an indirect effect on DSF and SDSF by controlling vegetation growth. For interannual variability, strong wind is still the main control, with precipitation a relatively important cofactor. Temperature has an irregular but somewhat negative relationship with dust storms. Precipitation and especially temperature have likely been important in the increase of DSF since 2000.
引用
收藏
页码:903 / 913
页数:11
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