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中国沙漠 ›› 2001, Vol. 21 ›› Issue (s1): 6-11.

• 论文 • 上一篇    下一篇

2000年春季中国北方沙尘暴天气气候成因研究

杨民1, 蔡玉琴1, 王式功2, 李文莉1, 尚可政2, 董光荣3   

  1. 1. 甘肃省气象局, 甘肃兰州 730020;
    2. 兰州大学大气科学系, 甘肃兰州 730000;
    3. 中国科学院寒区旱区环境与工程研究所, 甘肃兰州 730000
  • 收稿日期:2000-12-22 修回日期:2001-03-07 出版日期:2001-12-31 发布日期:2001-12-31
  • 通讯作者: 王式功
  • 作者简介:杨民(1976-),男(汉族),新疆昌吉人,助理工程师,主要从事天气预报及灾害性天气研究。
  • 基金资助:
    国家重点基础研究发展规划项目(G2000048703);国家自然科学基金重大项目(39990490)共同资助

Synoptic and Climatological Analysis of Sandstorms in the Spring of 2000 over Northern China

YANG Min1, CAI Yu-qin1, WANG Shi-gong2, LI Wen-li1, SHANG Ke-zheng2, DONG Guang-rong3   

  1. 1. Lanzhou Central Meteorological Observatory of Gansu Province, Lanzhou 730020, China;
    2. Department of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China;
    3. Clod and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of sciences, Lanzhou 730000, China
  • Received:2000-12-22 Revised:2001-03-07 Online:2001-12-31 Published:2001-12-31

摘要: 从环境背景和天气气候成因两个方面,分析了2000年春季中国北方沙尘暴频繁爆发的原因。结果表明,① 2000年春季中国北方大风沙尘暴的源地、路径和天气形势可归纳为三种类型;②近年来中国北方干旱加剧土地荒漠化严重,使原本广阔的戈壁沙漠面积逐步扩大,为沙尘暴天气的爆发提供了物质基础;③ 2000年处于反厄尔尼诺(拉尼娜)事件的高峰期,使东亚冬季风加强;同时2000年春季极涡位于东半球新地岛附近,冷空气频繁南下,易形成大风天气;④ 2000年春季我国北方干旱少雨,气温回升迅速且温度偏高,使解冻的地表土层疏松,又提供了丰富的沙尘源。

关键词: 沙尘暴, 源地与路径, 天气气候成因, 中国北方

Abstract: The high-frequency of sandstorm occurrence in the Spring of 2000 over Northern China has been analyzed in respect of circulation background and synoptic-climatological theories. The results show that 1) there are three patterns of the source, course and weather to sandstorms in the Spring of 2000 over Northern China.;2) abundant duststorm origin resulting in the sandstorm outbreak comes from spreading desert area resulted from more intense drought and more severe wildness recently over Northern China;3) 2000 is the fastigium of La-Nina that means more intense monsoon over the east part of Asia in winter, at the same time, in the Spring of 2000 the pole eddies lie in near Xindi island of East-hemisphere, which results in cold air going down northward ready to form gale; 4) another abundant duststorm origin is from looser soil resulted from arid and rare rain in the spring of 2000 over Northern China, air temperature rising rapidly and high.

Key words: sandstorm, source and course, synoptic and climatological causes, Northern China

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