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中国沙漠 ›› 2004, Vol. 24 ›› Issue (5): 603-606.

• 研究论文 • 上一篇    下一篇

西北地区东部冬季降水与次年沙尘暴发生的关系

张杰1, 郭铌1, 荻潇泓2   

  1. 1. 中国气象局兰州干旱气象研究所 甘肃省干旱气候变化与减灾重点实验室, 甘肃 兰州 730020;
    2. 兰州中心气象台, 甘肃 兰州 730020
  • 收稿日期:2003-01-20 修回日期:2003-12-08 出版日期:2004-10-20 发布日期:2004-10-20
  • 作者简介:张杰(1975-),女(汉族),甘肃民勤人,学士,主要从事干旱生态环境演变和遥感技术应用研究。E-mail:jiezhangami@sohu.com
  • 基金资助:
    西北沙尘暴预警服务系统"项目(2000DIA10031)资助

Analysis on Precipitation in Winter and Relation with Sand Days in Northwest Region

ZHANG Jie1, GUO Ni1, DI Xiao-hong2   

  1. 1. Key Laboratory of A rid Climatic Changing and Reducing Disaster of Gansu Province, Institute of Arid Meteorology, China Meteorological Administration, Lanzhou 730020, China;
    2. Lanzhou Central Meteorological Observatory, Lanzhou, Gansu Lanzhou 730020, China
  • Received:2003-01-20 Revised:2003-12-08 Online:2004-10-20 Published:2004-10-20

摘要: 选用1970-2000年西北地区88个气象站的冬季降水量和1971-2000年沙尘暴日数资料, 用自然正交分解(EOF)分析了冬季降水的时空分布特征。结果表明, 西北冬季降水第一载荷向量分布有一定差异, 第二载荷向量零线位置基本以干旱和半干旱区界限为准, 各自然气候区冬季降水的时空分布具有不一致性的特征; 以民勤为代表站的A区、以敦煌为代表站的C区冬季降水量与次年沙尘日数呈相反的变化趋势。说明冬季降水对次年沙尘多发的春季下垫面土壤湿度、地表粗糙度等特征有一定的影响, 从而对代表了沙漠气候特征的A区和代表西风带影响的沙漠戈壁C区的沙尘暴发生起到抑制作用。

关键词: 西北地区东部, 冬季降水量, 次年沙尘日数

Abstract: The distribution and variation of precipitation in winter in northwest region is analysed and seven sections is divided by using EOF and REOF method and the data including winter precipitation and sandy days data of 88 weather stations. The result showed The result showed that the precipitation in winter in northwest is different from regions in all around, the first load vector of 7 sections is different, the zero position of the second load vector is between arid region and clouding region. A section including Minqin and some other stations represented desert climate, and C section including Dunhuang and some other stations represented desert and Gebi influenced by west wind cincture .The variety trend of the winter precipitation of A and C sections is contrary with sandy days of the next year, but there are no contrary variety of other sections between winter precipitation and sandy days of the next year. All those means that the soil humidity and surface roughness in Spring are influenced by the winter precipitation of previous year, therefore,the sandy days of A, C section is influenced by the winter precipitation of previous year,but the other sections isn't influenced.

Key words: East of northwest region, winter precipitation, sandy days of the next year

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