Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2011, Vol. 31 Issue (3): 655-660    DOI:
国家重点基础研究发展规划     
Relationship between Sand Dust Transportation and Land Surface-Atmosphere Temperature Difference at Different Land Surface in Dust Source Areas
ZHAN Ke-jie1,2, ZHAO Ming3, YANG Zi-hui2, FANG Er-tian2, GUO Shu-jiang2, WANG Qiang-qiang2, WANG Duo-ze2
1.Lanzhou University, Lanzhou 730000, China; 2.Gansu Desert Control Research Institute, Lanzhou 730000, China; 3.Gansu Forestry Science and Technology Research Academy, Lanzhou 730000, China
Download:  PDF (2183KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  Most researches and statistical data showed that heat transport from underlying surface to the atmospheric provided energy to occurrence of sand storms and exerted important influence on it. From Jan. 2006 to May 2007, there were total 27 dust storms events occurred in the study area. Base on the statistic data of temperature difference between land surface and atmosphere in the dust storm days, we analyzed the influence of temperature difference to the vertical distribution characteristics of sand dust horizontal flux and mass-volume concentration. Results indicated that when the temperature difference exceeded 20 ℃, the vertical distribution of sand dust horizontal flux and mass-volume concentration in the oasis-underlying area would change to a certain degree, and the mass-volume concentration, especially, would decrease with the height; the vertical distribution of sand dust horizontal flux and mass-volume concentration oasis-underlying were more sensitive to the temperature difference than that in the desert area and the ecotone of desert-oasis.
Key words:  Minqin      surface-atmosphere temperature difference      dust storm      horizontal flux      dust mass-volume concentration     
Received:  12 December 2010      Published:  20 May 2011
ZTFLH:  P445.4  

Cite this article: 

ZHAN Ke-jie;ZHAO Ming;YANG Zi-hui;FANG Er-tian;GUO Shu-jiang;WANG Qiang-qiang;WANG Duo-ze. Relationship between Sand Dust Transportation and Land Surface-Atmosphere Temperature Difference at Different Land Surface in Dust Source Areas. JOURNAL OF DESERT RESEARCH, 2011, 31(3): 655-660.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2011/V31/I3/655

[1]钱正安.关于甘宁部分地区‘5·5’特强沙尘暴灾害的调查报告[J].大气情报,1993,30(4):1-13.
[2]胡隐樵,光田宁.强沙尘暴微气象特征和局地触发机制[J].大气科学,1997,21(5):581-589.
[3]卢琦,杨有林.全球沙尘暴警示录[M].北京:中国环境科学出版社,2001.
[4]Huang N,Ren Shan,Zheng X.Effects of the mid-air collision on sand saltation[J].Science in China Series G,2008,51(9):1416-1438.
[5]Zheng X J,Huang N,Zhou Y H.The effect of electrostatic force on the evolution of sand saltation cloud[J].The European Physical Journal E,2006,19:129-138.
[6]Zheng X J,Huang N,Zhou Y H.Laboratory measurement of electrification of wind-blown sands and simulation of its effect on sand saltation movement[J].Journal of Geophysical Research,2003,108 D(10):4322.
[7]Yue G W,Zheng X J.Effect of thermal diffusion and electrostatic force on evolution of wind-blown sand flow[J].Applied Mathematics and Mechanics,2007,28(2):183-192.
[8]牛生杰,岳平,刘晓云.2004年春夏季两次沙尘暴期间地面气象要素变化特征对比分析[J].中国沙漠,2007,27(6):1067-1071.
[9]牛生杰,岳平,张强,等.夏季强沙尘暴内部热力动力特征的个例研究[J].中国沙漠,2008,28(3):509-514.
[10]赵红岩,杨瑜峰,梁东升,等.中国北方沙尘暴与地温场的相关分析[J].中国沙漠,2007,27(3):509-513.
[11]钟海玲,高荣,李栋梁.地面风速的气候特征及其对沙尘暴的影响研究[J].中国沙漠,2009,29(2):321-326.
[12]王式功,杨德保,周玉素,等.我国西北地区“94·4” 沙尘暴成因探讨[J].中国沙漠,1995,15(4):332-338.
[13]王式功,杨德保,金炯.我国西北地区黑风暴的成因及对策[J].中国沙漠,1995,15(1):19-30.
[14]姜学恭,李彰俊,程丛兰,等.地面加热对沙尘暴数值模拟结果的影响研究[J].中国沙漠,2010,30(1):182-192.
[15]孙军,姚秀萍.一次沙尘暴过程锋生函数和地表热通量的数值诊断[J].高原气象,2002,21(5):488-494.
[16]王劲松,俞亚勋,赵建华.中国北方典型强沙尘暴的地面加热场特征分析[J].中国沙漠,2004,24(5):599-602.
[17]赵明,方峨天,詹科杰,等.民勤地区近地面沙尘监测系统的建立及其运行的初步评价[J].中国沙漠,2008,28(6):1163-1168.
[18]刘景涛,郑明倩.华北北部黑风暴的气候学特征[J].气象,1998,24(2):39-44.
[19]Zhao M,Zhan K J,Yang Z H,et al.Characteristics of the lower layer of sandstorms in the Minqin desert-oasis zone[J].Science in China Series,2010,53,doi:10.1007/s11430-010-4104-y.
No Suggested Reading articles found!