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中国沙漠 ›› 2005, Vol. 25 ›› Issue (3): 412-416.

• 研究论文 • 上一篇    下一篇

甘肃春季(3~5月)沙尘暴成因分析

郭慧1,2,3, 王式功3, 李栋梁1, 冯建英2, 陆登荣4, 张存杰2   

  1. 1. 中国科学院寒区旱区环境与工程研究所, 甘肃兰州 730000;
    2. 中国气象局兰州干旱气象研究所, 甘肃兰州, 730020;
    3. 兰州大学大气科学学院, 甘肃兰州, 730000;
    4. 甘肃省气象局, 甘肃兰州 730020
  • 收稿日期:2004-02-17 修回日期:2004-05-10 出版日期:2005-06-20 发布日期:2005-06-20
  • 作者简介:郭慧(1968-),女(汉族),陕西兴平人,硕士,高级工程师,主要从事气候研究。E-mail:guoh@gsma.gov.cn
  • 基金资助:
    国家重点基础研究发展规划项目(G2000048703);国家自然基金项目(40375015);科技部项目"西北干旱区沙尘暴预警、服务系统研究"(2000DIA10031)共同资助

Causes of Spring (Mar. to May) Sand-dust Storms in Gansu Province

GUO Hui1,2,3, WANG Shi-gong3, LI Dong-liang1, FENG Jian-ying2, LU Deng-rong4, ZHANG Cun-jie2   

  1. 1. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    2. Arid Meteorological Research Institute of China Meteorology Administration, Lanzhou 730020, China;
    3. Department of Atmospheric Science, Lanzhou University, Lanzhou 730000, China;
    4. Gansu Provincial Meteorological Bureau, Lanzhou 730020, China
  • Received:2004-02-17 Revised:2004-05-10 Online:2005-06-20 Published:2005-06-20

摘要: 甘肃春季(3~5月)沙尘暴小波变换分析清楚地反映了甘肃春季沙尘暴不同时间尺度周期振荡的交替作用。甘肃中西部自20世纪80年代以来变暖,其变暖与太阳黑子周期长度(SCL)密切相关。甘肃春季沙尘暴与甘肃中西部热力因子和降水研究表明,当冬季冷空气活动频繁,春季气温回升快,气温波动幅度大,降水偏少,甘肃春季容易发生沙尘暴。

关键词: 甘肃中西部, 热力作用, 沙尘暴, 小波分析, 太阳黑子周期长度(SCL)

Abstract: We analyzed the periodical variation of spring (from Mar. to May) sand-dust storms in Gansu province by using the Mexican Hat Wavelet method as well as their relation with thermal factors. There is positive correlation between the departure of pre-winter (from Dec. to Feb.) ground-air temperature difference and the spring sand-dust storm days in the middle and west Gansu province; the positive and the negative departure correspond very well to the more times of spring sand-dust storm before 1980's and the less times after 1980's in Gansu respectively. Contrary, there is negative correlation between the departure of the corresponding spring ground-air temperature difference and the spring sand-dust storm days.;When the cold air that affected the region is active in winter, the temperature rises rapidly in spring, the scope of spring daily temperature range is large and the precipitation is less, the spring sand-dust storms in Gansu happened easily. Otherwise, the spring sand-dust storms in Gansu are less. Especially, the warming winter phenomena happened in the 1990's, the minimum temperature rose prominently, the scope of daily temperature range reduced; in the other words, the heavy cold airs influencing the region weakened so much, the spring dust-sand storms tended to less. Global warming is the background of the warming in the west and middle of Gansu since 1980's. Furthermore, the warming in the region related closely to the sunspot cycle length (SCL).

Key words: west and middle in Gansu, thermal effect, sand-dust storm, wavelet, sunspot cycle length(SCL)

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