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JOURNAL OF DESERT RESEARCH  2009, Vol. 29 Issue (4): 744-749    DOI:
天气与气候     
Statistic Climate Characteristics and Thunderstorm Weather Tendency in Ningxia during the Last 45 Years
JI Xiao-ling1,2,3, MU Jian-hua3, ZHOU Hu3, YANG Kan3, ZHENG Guang-fen3, CHEN Xiao-juan3
1.College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China; 2.State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Science, Beijing 100081, China; 3.Ningxia Meteorological Observatory, Yinchuan 750002, China
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Abstract  The daily thunderstorm data of Ningxia during 1961—2005 are used to analyze the climatic change characteristics by methods of mathematical statistics, linear analysis, and wavelet analysis and so on. Some conclusions are drawn as follows: Ningxia is located in the region with middle thunderstorm frequency, and the number of annual mean thunderstorm days is 86.62 days. During the last 45 years, there were 7 years with more thunderstorm days and 7 years with less thunderstorm days; the number of the most annual thunderstorm days was 118 and the least was 65; the inter-annual change range was large. There was a decreasing trend of thunderstorm weather frequency in these 45 years, with a decreasing rate of 3.072 d/10a, and a 3~4 years relatively short period and a 8 years relatively long period viration. Thunderstorm events mainly occurred in March to October, mostly in summer, and especially in July, it has obviously seasonal and monthly change, and the probability was extremely low in winter. The first thunderstorm occurred in mid-April and the last occurred in mid-September by mean; the mean duration between the first and the last in the whole region was about 139 days. There was obvious diurnal variation in thunderstorms occurrence, showing bimodal or unimodal types; most occurred during 11:00—22:00, with high frequency before or after 15:00. The occurrence of thunderstorms has close relationship with the terrain and topography.
Key words:  thunderstorm      climatic characteristic      tendency      wavelet analysis      Ningxia     
Received:  17 March 2008      Published:  20 July 2009
ZTFLH:  P427  

Cite this article: 

JI Xiao-ling;;MU Jian-hua;ZHOU Hu;YANG Kan;ZHENG Guang-fen;CHEN Xiao-juan. Statistic Climate Characteristics and Thunderstorm Weather Tendency in Ningxia during the Last 45 Years. JOURNAL OF DESERT RESEARCH, 2009, 29(4): 744-749.

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http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2009/V29/I4/744

[1]石定朴,顾映欣,陶祖钰.闪电活动和中小尺度对流系统[M]//中尺度气象文集.北京:气象出版社,1993:202-208.
[2]郄秀书,言穆弘,郭昌明.闪电资料及风暴短时预报初探[M]//中尺度气象文集.北京:气象出版社,1993:189-194.
[3]虞曼,臧庚援,张勋文.现代防雷技木基础[M].北京:清华大学出版社,1995.
[4]潘忠林.现代防雷技术[M].成都:电子科技大学出版社,1997.
[5]张敏锋,冯霞.我国雷暴天气的气候特征[J].热带气象学报,1998,14(2):156-162.
[6]孔燕燕,沈建国.强雷暴预报[M].北京:气象出版社,2001.
[7]郄秀书,张广庶,孔祥贞,等.青藏高原东北部地区夏季雷电特征的观测研究[J].高原气象,2003,22(3):209-216.
[8]张鸿发,程国栋,张彤.中国区域闪电分布和闪电气候的特点[J].干旱气象,2004,22(4):17-25.
[9]张美平,敖淑珍,刘翔等,等.广州白云国际机场近46年来雷暴气候的统计特征[J].应用气象学报,2004,15(1):66-73.
[10]杨国锋,汤达章,刘晓,等.一次强风暴天气闪电定位资料与雷达资料的综合分析[J].气象科技,2005,33(2):167-172.
[11]宋培国,李宁,杨慧娟.基于GIS技术的雷电监测系统[J].自然灾害学报,2006,15(6):72-76.
[12]李南,魏鸣,姚叶青.安徽闪电与雷达资料的相关分析以及机理初探[J].热带气象学报,2006,22(3):265-272.
[13]王新平,张景光,李新荣,等.沙坡头地区多年降水分布特征、趋势及其变率[J].中国沙漠,2001,21(4):260-264.
[14]马晓波,胡泽勇.青藏高原40年来降水变化趋势及突变的分析[J].中国沙漠,2005,25(1):137-139.
[15]丁瑞强,王式功,尚可政,等.近45 a我国沙尘暴和扬沙天气变化趋势和突变分析[J].中国沙漠,2003,23(3):306-310.
[16]钱正安,宋敏红,李万元.近50年来中国北方沙尘暴的分布及变化趋势分析[J].中国沙漠,2002,22(2):106-111.
[17]赵燕宁,时兴合,秦宁生,等.青海南部地区40多年来气候变化的特征分析[J].中国沙漠,2005,25(4):529-534.
[18]杨建平,丁永建,陈仁升.长江黄河源区水文和气象序列周期变化分析[J].中国沙漠,2005,25(5):351-355.
[19]Farge M.Wavelet transforms and their applications to turbulence[J].Annu Rev Fluid Mech,1992,24:395-457.
[20]陈涛,孙卫国,程炳岩.交叉小波变换在河南降水时频分析中的应用[J].南京气象学院学报,2002,25(5):685-692.
[21]崔锦泰.小波分析导论[M].西安:西安交通大学出版社,1995:66-99.
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