Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2007, Vol. 27 Issue (5): 851-858    DOI:
天气与气候     
A Numerical Study on Influence of Sand Source Area in Inner Mongolia on the Dust Storm Expending Proces

LI Zhang-jun1,2, JIANG Xue-gong2, CHENG Cong-lan3

1.Nanjing University of Information Science and Technology, Nanjing 210044, China; 2.Inner Mongolia Autonomous Region Meteorological Observatory, Hohhot 010051, China; 3.Inner Mongolia Autonomous Regional Meteorological Bureau, Hohhot 010051, China
Download:  PDF (1613KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  

Based on a numerical study on the dust storm process occurred from March 18 to March 22, 2002, the influence of the dust source area in Inner Mongolia on the dust storm extending process was conducted. The results show that the degradation of the desert steppe in Inner Mongolia was a reason causing the frequent appearing of dust storm in northwest China. Owing to the distribution characteristic of terrain height in sand source area and the change of the geostrophic wind with height, two isolated preponderant transporting zones often appear in the dust particle transporting process. One lies in the mid\|troposphere while the other closely upon the surface. The transportation speed, distance and their impact area and time are different in the process. The raising dust in Inner Mongolia was transported mainly through the zone upon the surface. Its transportation in troposphere became less and less while the dust storm extended southward and eastward.

Key words:  dust storm      dust source area      dust particle transportation      numerical simulation     
Received:  06 September 2006      Published:  20 September 2007
ZTFLH:  P445.4  

Cite this article: 

LI Zhang-jun;JIANG Xue-gong;CHENG Cong-lan. A Numerical Study on Influence of Sand Source Area in Inner Mongolia on the Dust Storm Expending Proces. JOURNAL OF DESERT RESEARCH, 2007, 27(5): 851-858.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2007/V27/I5/851

[1]权建农,奚晓霞,王鑫,等.兰州市2001年沙尘气溶胶质量浓度的特征分析[J].中国沙漠,2005,25(1):93-97.
[2]李霞,胡秀清,崔彩霞,等. 南疆盆地沙尘气溶胶光学特性及我国沙尘天气强度划分标准的研究[J].中国沙漠,2005,25(4):488-495.
[3]牛生杰,章澄昌.贺兰山地区沙尘气溶胶化学组分及富集因子分析[J].中国沙漠,2000,20(3):264-268.
[4]沈建国,刘菲,牛生杰,等.一次沙尘暴过程TSP质量浓度的连续观测和分析.[J].中国沙漠,2006,26(5):786-791.
[5]宁海文,王式功,杜继稳,等.西安沙尘天气特征及其对空气质量的影响[J].中国沙漠,2005,25(6):886-890.
[6]叶笃正,丑纪范. 关于我国华北沙尘天气的成因与治理对策[J].地理学报,2000,55:513-521.
[7]石广玉,赵思雄.沙尘暴研究中的若干科学问题[J].大气科学,2003,27(4):591-606.
[8]周秀骥,徐祥德,颜鹏,等.2000年春季沙尘暴动力学特征[J].中国科学:D辑,2002,32(4):327-334.
[9]王式功,扬德保.我国西北地区黑风暴的成因和对策[J].中国沙漠,1995,15(1):19-30.
[10]钱正安,蔡英,刘景涛,等.中国北方沙尘暴研究若干问题[C]∥沙尘暴学术研讨会文集.台湾蒙藏委员会出版,2002:63-76.
[11]赛胜宝,智瑞年. 内蒙古北部荒漠化草原带的严重荒漠化及其治理[C]∥沙尘暴成因及综合防治.呼和浩特:内蒙古人民出版社,2004:260-265.
[12]郝敦元,刘仲龄. 内蒙古草原退化与生态安全[C]∥沙尘暴成因及综合防治.呼和浩特:内蒙古人民出版社,2004:227-241.
[13]程丛兰,王迎春,刘伟东,等.与动力场相耦合的区域沙尘分档模式及个例模拟[J].科学通报,2004,46(19):2007-2013.
[14]Anthes R A, Warner T T. Development of hydrodynamics models for air pollution and mesometeorological studies[J]. Mon Wea Rev,1978,106:1045-1078.
No Suggested Reading articles found!