北京大学学报(自然科学版)

沙尘暴次数和持续时间呈指数关系N=A·10-bt

刘国梁1,郝丽珍2   

  1. 1山西大学环境与资源学院,太原,030006;2太原大学计算机科学系,太原,030009
  • 收稿日期:2004-08-24 出版日期:2005-07-20 发布日期:2005-07-20

Exponential Relationship of the Sand-Dust Storm Occurrence Frequency and the Duration Time: N=A·10-bt

LIU Guoliang1, HAO Lizhen2   

  1. 1School of Environmental Sciences and Resources, Shanxi University, Shanxi Taiyuan, 030006; 2Department of Computer Science, Taiyuan College, Shanxi Taiyuan, 030009
  • Received:2004-08-24 Online:2005-07-20 Published:2005-07-20

摘要: 通过分析中国国家气象局整理的中国沙尘暴资料,发现持续时间大于t的沙尘暴次数N满足:N=A·10-bt,其中Ab是正的常数。这个规律具有普适性。另外,还发现b值与沙尘暴阈值风速有关,沙尘暴阈值风速较小的地区,如沙漠、沙地以及干旱的黄土高原,b值较小;沙尘暴阈值风速较大的地区,如戈壁、高山等,则b的值较大。

关键词: 中国沙尘暴, 持续时间, 沙尘暴阈值风速

Abstract: The sanddust storm data compiled by the China State Meteorological Bureau for the period of 1960 to 2000 are analyzed to find the distribution of the sand-dust storm occurrence frequency against the duration time.There exits a universal relationship of N=A·10-bt, where N is the number of sand-dust storm occurrence frequency with the duration time greater than t, A and b are constants. It is also shown that the constant b is related with the threshold wind speed for the sand-dust storm with bigger value of b less threshold wind speed for the occurrence of the sand-dust storm at that site. In fact, the large value of b is found in the Gobi and high mountainous regions whereas the small value of b in the sand and dry loess regions.

Key words: sand-dust storm in China, duration time, threshold wind speed of the sand-dust storm

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