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中国沙漠 ›› 2003, Vol. 23 ›› Issue (5): 488-492.

• 研究论文 • 上一篇    下一篇

沙漠绿洲-高山冰雪气候带的垂直变化特征研究

史玉光, 杨青, 魏文寿   

  1. 中国气象局 乌鲁木齐沙漠气象研究所, 新疆 乌鲁木齐 830002
  • 收稿日期:2002-09-15 修回日期:2002-10-20 出版日期:2003-10-20 发布日期:2003-10-20
  • 作者简介:史玉光(1961-),男(汉族),山西人,副研究员,主要从事天气动力学和气候环境研究。E-mail:shiiyq2517@sina.com.cn
  • 基金资助:
    科技部重大基础研究前期专项(2002CCA04600);国家重点基础研究发展规划973项目(G1999043504)资助

Research about the Vertical Change in the Climatic Zones of Desert Oasis to Alp Ice-snow

SHI Yu-guang, YANG Qing, WEI Wen-shou   

  1. Institute of Desert Meteorology, China Meteorology Administration, Urumqi 830002, China
  • Received:2002-09-15 Revised:2002-10-20 Online:2003-10-20 Published:2003-10-20

摘要: 气候变化在垂直方向上的分布规律是气候变化研究的一个重要方面。利用在天山北坡中部径向剖面上的6个不同海拔高度的气象站的气象资料,研究了沙漠绿洲-高山冰雪气候带在冬季、夏季和年度的年际气候变化对高度的响应,指出20世纪90年代(1991-2000)与前30 a(1961-1990)相比,平均气温、年降水量增加幅度随高度呈现非线性变化,不论在哪个高度上,冬季的增温幅度都要大于夏季;在最靠近沙漠的低海拔地区,年降水量增加幅度并不是最大的,而在海拔较高的山前绿洲地带和在3 500 m的高山区降水量增幅相对较大。此外,对气温、降水、相对湿度、蒸发等气候因子的变化趋势倾向率进行了分析,比较了不同高度的线性倾向率,揭示了沙漠绿洲边缘至高山冰雪带的气候变化在垂直方向上的分布特征,表明不论在哪个高度上,冬季、夏季和年度的平均气温变化都具有上升趋势;在山前地带和高海拔山区,降水增加趋势相对明显;蒸发能力减弱,相对湿度增加。

关键词: 气候变化, 沙漠, 绿洲, 气候带

Abstract: The vertical distribution of climate change is an important aspect of climate research.The observations of meteorological stations at 6 different sea level elevations along the meridional cross-section in the central part of northern Tianshan Mountains slope are used to study the interannual climate changes of the desert/oasis to alp ice/snow climatic zones changing with heights in winter,summer and around the year.Compared with the previous 30 years(1961-1990),the increments of mean temperature and annual precipitation are nonlinear functions of height and they are larger in winter than in summer at all elevations in 1990s(1991-2000);The increment of annual precipitation is relatively larger in the oasis belt at high elevation in front of the mountain and the mountain region at a height of 3 500 m other than in the low elevations near desert.Additionally,the change tendencies of the climate factors such as temperature,precipitation,relative humidity and evaporation etc.are analyzed and the linear tendencies are compared at different elevations.The vertical distributions of climate change in the oasis edge to mountain ice/snow regions revealed that the changes of mean temperature have rising tendency at all elevations;in front of the mountain and in the high elevation areas the precipitation increment is relatively larger,evaporation decreases and relative humidity increases.

Key words: climate change, desert, oasis, climatic zones

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