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气候变化对内蒙古中东部沙地-湿地镶嵌景观的影响

李兴华1,2;韩芳1;张存厚1;娜日苏1;刘朋涛1   

  1. 1内蒙古生态与农业气象中心, 呼和浩特 010051; 2内蒙古气象经济研究所, 呼和浩特 010051
  • 收稿日期:2008-06-23 修回日期:1900-01-01 出版日期:2009-01-20 发布日期:2009-01-20

Influence of climate change on mosaic landscape of sand land-wetland in middle-east Inner Mongolia.

LI Xing-hua1,2;HAN Fang1;ZHANG Cun-hou1;NA Ri-su1;LIU Peng-tao1   

  1. 1Centre of Inner Mongolia Ecology and Agricultural Meteorology, Huhhot 010051, China;2Inner Mongolia Institute of Meteorological Economics, Huhhot 010051, China
  • Received:2008-06-23 Revised:1900-01-01 Online:2009-01-20 Published:2009-01-20

摘要: 利用小波分析和遥感技术相结合的方法,研究了气候变化对1961—2005年内蒙古中东部沙地-湿地镶嵌景观的影响.结果表明:1961—2005年,研究区年均气温呈直线上升趋势,增温率为0.32 ℃·(10 a)-1,年降水量变化呈现30 a的长周期和15 a的短周期,年均风速呈下降趋势,10 a的风速减小率为0.26 m·s-1;研究区东南部存在一个气候变化恒定区域,由此恒定区向西北进入浑善达克沙地腹地,向东逐步进入科尔沁沙地腹地;2010年以前,研究区仍将维持气温升高、降水偏少、风速减小的趋势;受气候暖干化的影响,浑善达克沙地及其周围湿地的总面积呈逐年缩小趋势,随着沙地内部植被的退化,流动沙地不断扩大、湿地萎缩、湖泊干涸,而相应的固定和半固定沙地面积则明显减少.

关键词: 森林, 拆分, 稳定同位素, 呼吸作用

Abstract: By using wavelet transform and remote sensing techniques, the influence of clima te change on the unique mosaic landscape of sand land-wetland in middle-east I nner Mongolia in 1961-2005 was studied. The results showed tha t in 1961-2005, the annual air temperature in study area had a n increment of 032 ℃·(10 a)-1, the annual precipitation fluctuated with a cycle of 30 years and of 15 years, and the annual average wind speed decreased by 026 m·s-1·(10 a)-1. In the southeast part of study area, which located in the places between Hunshandake sand land and Keerqin Deserts, there w as a district, in which, the climatic characteristics did not change evidently. Until 2010, the study area would still have an increasing air temperature, lesse r precipitation, and decreasing wind speed. Under the influence of warming and drying, the total area of Hunshandake sand land and the wetland a round reduced year after year, and, with the vegetation degradation on sand land , wetland shrunk and lake dried up, moving sand land enlarged ceaselessly, whil e immovable and semi-moving sand lands reduced obviously.

Key words: stable isotope, forest, partitioning., respiration