Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2015, Vol. 35 Issue (5): 1128-1135    DOI: 10.7522/j.issn.1000-694X.2014.00202
    
Wind Regime Characteristics of the Bosten Lake Basin in Xinjiang, China
Liu Qiangji, Wu Shengli
College of Geographical Science and Tourism/Xinjiang Laboratory of Lake Environment and Resources, Xinjiang Normal University, Urumqi 830054, China
Download:  PDF (1949KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  

By statistics and calculation of the wind data, systematic research is made on the characteristics of wind regime in the Bosten Lake basin. The annual average wind speed is rather small, generally, it is 1.6-3.0 m·5s-1; the effective time of sand-driving wind when the wind speed is more than or equals to 6.0 m·5s-1 is obviously different in various regions. Among them, the days of sand-driving wind in Bayinbuluk account for 55.59% of the total number of days, in Yanqi, Luntai, Hejing, it is 18.75%, 12.72%, 11.48%, 12.72% respectively, in the rest of the stations it is lower than 10%. As the wind speed scale increases, the frequency of sand-driving wind reduces, and it is mostly concentrated 6.1-10.0 m·5s-1; Wind variability index is between 0.49 to 0.68 in research region, and it belongs to middle ratio, the characteristics of wind conditions belong to blunt bimodal or sharp bimodal; sand-transporting potential belongs to low wind energy environment, and there are huge regional differences.

Key words:  Bosten Lake basin      mean wind speed      sand-driving wind speed      sand-transporting potential     
Received:  18 September 2014      Published:  20 September 2015
ZTFLH:  X169  
Articles by authors
Liu Qiangji
Wu Shengli

Cite this article: 

Liu Qiangji, Wu Shengli. Wind Regime Characteristics of the Bosten Lake Basin in Xinjiang, China. JOURNAL OF DESERT RESEARCH, 2015, 35(5): 1128-1135.

URL: 

http://www.desert.ac.cn/EN/10.7522/j.issn.1000-694X.2014.00202     OR     http://www.desert.ac.cn/EN/Y2015/V35/I5/1128

[1] 俎瑞平,张克存,屈建军,等.塔克拉玛干沙漠地面风场特征及周边地区沙丘排列关系分析[J].应用气象学报,2006,16(4):468-475.
[2] 朱震达.中国沙漠、沙漠化、荒漠化及其治理对策[M].北京:中国环境出版社,1999:113-115.
[3] 张正偲,董治宝,赵爱国.输沙势计算中的“时距”问题[J].干旱区地理,2010,33(2):177-182.
[4] 俎瑞平,张克存,屈建军.塔克拉玛干沙漠风沙活动强度特征[J].地理研究,2005,24(5):699-707.
[5] 朱震达,陈志平,吴正.塔克拉玛干沙漠风沙地貌研究[M].北京:科学出版社,1981:27-55.
[6] 吴正.风沙地貌学[M].北京:科学出版社,1987:67-68.
[7] 凌裕泉.塔克拉玛干沙漠流场特征与风沙活动强度的关系[J].中国沙漠,1988,8(2):25-37.
[8] 凌裕泉.输沙量(率)水平分布的非均一性[J].实验力学,1994,9(4):352-356.
[9] 韩致文,王涛,孙庆伟,等.塔克拉玛干沙漠公路风沙危害与防治[J].地理学报,2003,58(2):201-208.
[10] Wang X M,Dong Z B,Zhang J W.Relations between morphology,air flow,sand fiux and particle size on transverse dunes,Taklimakan Sand Sea,China[J].Earth Surface Processes and Landforms,2002(5):215-226.
[11] Wang X M,Dong Z B,Zhang J W.Geomorphology of northeast Taklimakan Sand Sea[J].Geomorphology,2001,42:183-195.
[12] Dong Z B,Wang X M,Chen G T.Monitoring sand dune advance in the Taklimakan Desert[J].Geomorphology,2000,35:219-231.
[13] 杨兴华,李红军,何清,等.塔克拉玛干沙漠荒漠过渡带春季风沙活动特征—以肖塘为例[J].中国沙漠,2012,32(4):915-920.
[14] 杨兴华,何清,霍文,等.塔克拉玛干沙漠南缘风沙跃移运动研究—以策勒县为例[J].中国沙漠,2012,32(4):910-914.
[15] 何清,杨兴华,艾力·买买提明,等.塔克拉玛干沙漠风蚀起沙观测研究—试验介绍与观测结果初报[J].中国沙漠,2011,31(2):315-322.
[16] 陈渭南,董治宝,杨佐涛,等.塔克拉玛干沙漠的起沙风速[J].地理学报,1995,50(4):360-367.
[17] 李振山,陈广庭.塔克拉玛干沙漠起沙风况[J].中国沙漠,1999,19(1):43-45.
[18] 陈广庭,冯起.塔里木盆地沙漠石油公路沿线风沙环境的形成与演变[M].北京:中国环境科学出版社,1997:112-130.
[19] 武胜利.新疆和田河流域灌(草)丛沙堆发育机制研究[D].上海:华东师范大学,2007.
[20] 周向玲,俞胜清,阿布都米基提,等.布古里沙漠部分地区风沙环境特征分析[J].干旱区地理,2013,36(5):795-802.
[21] 李生宇,雷加强,徐新文.塔克拉玛干沙漠腹地沙尘暴发生条件分析[J].应用气象学报,2007,18(4):490-496.
[22] 杨兴华,何清,艾力·买买提明.塔克拉玛干沙漠塔中地区春夏季风蚀起沙研究[J].中国沙漠,2010,30(4):770-776.
[23] 刘新春,钟玉婷,何清,等.塔克拉玛干沙漠腹地及周边地区PM10时空变化特征及影响因素分析[J].中国沙漠,2011,31(2):323-330.
[24] 王敏仲,魏文寿,何清,等.边界层风廓线雷达资料在沙尘天气分析中的应用[J].中国沙漠,2011,31(2):352-356.
No Suggested Reading articles found!