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JOURNAL OF DESERT RESEARCH  2007, Vol. 27 Issue (3): 509-513    DOI:
天气与气候     
Correlation Analysis on Soil Temperature Field and Dust-storms in Northern China
ZHAO Hong-yan1,2, YANG Yu-feng1, LIANG Dong-sheng2, TANG Mao-cang3, ZHANG Ju-ling1, LI Dong-liang3
1.Key Laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province; Lanzhou Institute of Arid Meteorology, China Meteorological Administration, Lanzhou 730020, China; 2.Lanzhou Regional Climate Center,Lanzhou 730020, China;3.Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
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Abstract  Based on the meteorological data of representative stations from 1954 to 2003, we analyzed the relationship between sand-dust storms and the soil temperature field at 3.2 m depth and precipitation field. Some conclusions have been obtained: the soil temperature fields showed remarkable differentiation between that in years with more sand-dust storms and that in years with less sand-dust storms; lower soil temperature appeared in more sand-dust storm years, but higher soil temperature appeared in less sand-dust storm years; less sand-dust storms happed in year with more precipitation during April, but more sand-dust storms happed in year with less precipitation during April. It was proved that the soil temperature at 3.2 m had good seasonal continuity, so that soil temperature in winter even in last autumn can be used to forecast the sand-dust frequency during next spring.
Key words:  northern China      sand-dust storms      soil temperature field      precipitation field     
Received:  16 February 2006      Published:  20 May 2007
ZTFLH:  P445.4  

Cite this article: 

ZHAO Hong-yan;YANG Yu-feng;LIANG Dong-sheng;TANG Mao-cang;ZHANG Ju-ling; LI Dong-liang. Correlation Analysis on Soil Temperature Field and Dust-storms in Northern China. JOURNAL OF DESERT RESEARCH, 2007, 27(3): 509-513.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2007/V27/I3/509

[1]史培军,严平,高尚玉,等.我国沙尘暴灾害及其研究进展与展望[J].自然灾害学报,2000,9(3):71-77.
[2]王式功,王金艳,周自江,等.我国沙尘天气的区域特征[J].地理学报,2003,58(2) :193-200.
[3]周自江,张国材.中国北方典型的强沙尘暴事件(1954—2002年)[J].科学通报,2003,48(11):1224-1228.
[4]叶笃正,丑纪范,刘纪远.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(2):514-521.
[5]王劲松,余亚勋,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.
[6]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.
[7]Tang Maocang, Shen Zhibao. Some basic characteristics of the climate of Qinghai—Xizang Plateau (Beijing) [J].1980, l(2):1563-1568.
[8]赵红岩,汤懋苍,杨瑜峰,等.西北区冰雹分布及与地温场的相关分析[J].高原气象,2004,23(6):781-786.
[9]汤懋苍,张拥军,李栋梁.短期气候预测地气图方法的7条预报规则[J].高原气象,2005,24(2):218-222.
[11]张拥军,汤懋苍,李栋梁.淮河大水的基本原因及预测途径探讨[J].高原气象,2005,24(1):112-116.
[12]汤懋苍,张拥军,唐红玉,等.青海省雪灾气候预测的地气图方法[J].高原气象,2005,24(3):315-319.
[13]赵红岩,俞亚勋,汤懋苍,等.中国西北区冰雹与地震的相关性分析[J].地球科学进展,2005,20(特刊):177-183.
[14]张杰,郭铌,荻潇泓.西北地区东部冬季降水与次年沙尘暴发生的关系[J].中国沙漠,2004,24(5):603-606.
[15]陈晓光,赵光平,郑广芬,等.宁夏春季典型沙尘暴年环流特征量分析[J].中国沙漠,2004,24(5):570-575.
[16]赵红岩,陈旭辉,王锡稳,等.西北地区春季沙尘暴气侯分析及预测方法研究[J].中国沙漠,2004,24(5):637-641.
[17]郭铌,张杰,韩涛,等.西北特殊地形与沙尘暴发生的关系探讨[J].中国沙漠,2004,24(5):676-581.
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