干旱气象 ›› 2015, Vol. 33 ›› Issue (1): 28-37.DOI: 10.11755/j.issn.1006-7639(2015)-01-0028

• 论文 • 上一篇    下一篇

黑河下游额济纳三角洲气候及生态环境变化分析

年雁云1, 2王晓利3蔡迪花4   

  1. 1. 兰州大学资源环境学院, 甘肃 兰州 730000;
    2. 中国科学院寒区旱区环境与工程研究所, 甘肃 兰州 730000;
    3. 北京大学城市与环境学院, 北京 100871;
    4. 中国气象局兰州干旱气象研究所, 甘肃 兰州 730020
  • 出版日期:2015-02-28 发布日期:2015-02-28
  • 作者简介:年雁云(1979-),男,汉族,甘肃临夏人,讲师,博士,研究方向:遥感和GIS在水文水资源研究中的应用.E-mail:yynian@lzu.edu.cn
  • 基金资助:

    国家基础科学人才培养基金项目(J1210065)、兰州大学中央高校基本科研业务费专项资金项目(lzujbky-2014-210|lzujbky-2013-bt01)、兰州大学西部环境教育部重点实验室开放基金及2013年留学人员科技活动择优资助项目“基于Rs与GIS的河西内陆河水库春季蓄水方案研究”共同资助

Analysis on Climate and Ecological Environment Change in the Ejin Delta,the Lower Reaches of the Heihe River

NIAN Yanyun 1, 2WANG Xiaoli3CAI Dihua4   

  1. 1.College of Earth and Environmental Sciences,Lanzhou University,Lanzhou 730000,China;
    2.Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Science,Lanzhou 730000,China;
    3. College of Urban and Environmental Sciences,Peking University,Beijing 100871,China;
    4. Institute of Arid Meteorology,CMA,Lanzhou 730020,China  
  • Online:2015-02-28 Published:2015-02-28

摘要:

气候是生态环境变化的重要驱动因子,分析其变化特征对生态环境监测具有重要意义.本文以生态环境急剧恶化的黑河流域下游额济纳三角洲为研究对象,利用1960~2012年额济纳气象站的气温降水资料,采用Mann-Kendall检验、回归分析及累积距平曲线分析气候特征,结合重标极差(R/S)分析法预测未来趋势结果表明:近53a额济纳三角洲气温显著升高降水无明显趋势;气温年代际增温幅度差异明显,1980年代1990年代增幅最大;降水呈“少多少”波动变化,21世纪暖干化明显;暖冬现象显著。结合GIMMS-NDVI及东居延海面积、正义峡径流量,通过Pearson相关分析,结果表明:气候暖干化及黑河干流下泄量减少导致东居延海萎缩盐化、植被退化;2003年以后东居延海面积增加是2002年开始人为生态输水的结果,而非气候暖湿化的表现。

 

关键词: 气温, 降水, Mann-Kendall检验, R/S分析, 额济纳三角洲

Abstract:

As a major driving factor of environment change,characteristic analysis of climate change is very important for environment detection. In this paper,by taking the Ejin delta in the lower reaches of the Heihe River as the research area,on the basis of temperature and precipitation data during 1960 - 2012 from Ejin meteorological station,the characteristic of climate change over the past 53 years was analyzed firstly by using the methods of Mann - Kendall test,regression analysis and accumulative anomaly,and then Mann - Kendall test and R/S analysis were used to predict the future climate change trend. The results were as followed:The temperature in the Ejin delta increased and precipitation appeared non - remarkable trend over the past 53 years. There were remarkable differences in different decades, the temperature increased most from the 1980s to the 1990s,while precipitation appeared fluctuating change with less - more - less. A dryer and warmer climate trend would be obvious in the 21st century,and the warm winter phenomenon would be significant. Combining the data of GIMMS - NDVI,the East Juyan Lake area and runoff at the Zhengyi gauge station,through the Pearson correlation analysis, we concluded that warm and dry climate trend and the runoff reduction of the Heihe River led to shrink and salinization of the West and East Juyan Lakes,and the vegetation degradation. While the increase of the East Juyan Lake area from 2003 was the result of ecological conveyance water project in 2002,rather than the warming - wetting trend of climate.

Key words: temperature, precipitation, Mann - Kendall test, R/S analysis, Ejin delta

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