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黄河中游砒砂岩地区皇甫川流域气候变化特征分析
引用本文:高清竹,江源,李立业.黄河中游砒砂岩地区皇甫川流域气候变化特征分析[J].干旱区资源与环境,2005,19(1):116-121.
作者姓名:高清竹  江源  李立业
作者单位:1. 中国农业科学院农业环境与可持续发展研究所,北京,100081
2. 北京师范大学资源研究所,北京,100875
3. 内蒙古准格尔旗水土保持局,薛家湾,017100
基金项目:国家重点基础研究发展规划项目“中国陆地生态系统碳循环及其驱动机制研究”(2 0 0 2CB412 5 0 8),“草地与农牧交错带生态系统重建机理及优化生态—生产范式”(G2 0 0 0 0 1860 4)资助
摘    要:采用 1 961~ 2 0 0 0年连续 40年的逐月气象数据 ,分析黄河中游典型砒砂岩地区-皇甫川流域气候及其变化特征。分析结果表明 :皇甫川流域大陆性气候特点明显 ,降雨主要集中在每年的 6月~ 9月 ,这四个月的降雨量占全年的 76.7% ,形成河川径流的汛期。皇甫川流域年降雨量和汛期降雨量具有明显的减少趋势而且降雨量年际之间的波动很大 ;年均气温具有明显上升趋势 ,近 40年来年均气温升高了 0 .4℃ ;年平均风速总的变化趋势是逐渐降低的。另外 ,皇甫川流域湿度指数总体变化具有降低趋势 ,而温暖指数则是大幅度增高。可见 ,皇甫川流域气候变化具有明显地干和热的趋势。

关 键 词:气候变化  皇甫川流域  黄河中游砒砂岩地区
文章编号:1003-7578(2005)01-116-06
修稿时间:2003年12月15

Analysis on Climate Change of Huangfuchuan Watershed in Middle Yellow River
GAO Qing-zhu,JIANG Yuan,LI Li-ye.Analysis on Climate Change of Huangfuchuan Watershed in Middle Yellow River[J].Journal of Arid Land Resources and Environment,2005,19(1):116-121.
Authors:GAO Qing-zhu  JIANG Yuan  LI Li-ye
Institution:GAO Qing-zhu 1 JIANG Yuan 2 LI Li-ye 3
Abstract:Based on weather data from meteorological station of Huangfuchuan watershed in Middle Yellow River, the paper analyzed climate changes during 1961-2000. The results indicated that Huangfuchuan watershed had a typical continental climate and its rainfall has concentrated from June to September annually, which occupied in 76.7% of annual precipitation, and the four month had become the flood season in years at study area. Both annual rainfall and rainfall in flood season varied greatly from year to year, having an apparent declining tendency for decades. In recent 40 years, annual mean temperature had increased 0.4℃, and the annual mean wind speed had weakened. Humidity Index of Huangfuchuan watershed had trended to reducing while the warmth index had increased obviously. The tendency of climate changes in Huangfuchuan watershed were arid and warm in recent 40 years.
Keywords:Climate Changes  Huangfuchuan Watershed  the Soft Rock Area of Middle Yellow River
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