1970—2000年青藏高原内流区冰川储量变化的初探

崔志勇, 李志伟, 李佳, 汪长城, 周文明. 1970—2000年青藏高原内流区冰川储量变化的初探[J]. 地球物理学报, 2014, 57(5): 1440-1450, doi: 10.6038/cjg20140509
引用本文: 崔志勇, 李志伟, 李佳, 汪长城, 周文明. 1970—2000年青藏高原内流区冰川储量变化的初探[J]. 地球物理学报, 2014, 57(5): 1440-1450, doi: 10.6038/cjg20140509
CUI Zhi-Yong, LI Zhi-Wei, LI Jia, WANG Chang-Cheng, ZHOU Wen-Ming. A preliminary study of the volume variation of the glaciers in the Qinghai-Tibetan Plateau Interior Area between 1970 and 2000[J]. Chinese Journal of Geophysics (in Chinese), 2014, 57(5): 1440-1450, doi: 10.6038/cjg20140509
Citation: CUI Zhi-Yong, LI Zhi-Wei, LI Jia, WANG Chang-Cheng, ZHOU Wen-Ming. A preliminary study of the volume variation of the glaciers in the Qinghai-Tibetan Plateau Interior Area between 1970 and 2000[J]. Chinese Journal of Geophysics (in Chinese), 2014, 57(5): 1440-1450, doi: 10.6038/cjg20140509

1970—2000年青藏高原内流区冰川储量变化的初探

详细信息
    作者简介:

    崔志勇,男,1985年生,大地测量学与测量工程专业,硕士,主要从事利用RS和GIS技术解译冰川变化及其时空变化规律的研究.

  • 中图分类号: P228

A preliminary study of the volume variation of the glaciers in the Qinghai-Tibetan Plateau Interior Area between 1970 and 2000

  • 青藏高原内流区特殊的地理位置和自然环境使得对本区域冰川体积变化的研究相比中国西部其他冰川发育区难度大很多.而作为本区域重要水源补给,同时又是区域气候变化重要指示器的冰川,其储量的变化又是迫切需要获知的信息.在此前提下,本文基于RS、GIS技术平台提取了本区域冰川面积变化数据,并结合冰川目录数据、本区域冰川面积变化的研究资料,采用冰川体积与面积之间的统计关系模型,探讨了本区域冰川自1970年至2000年的体积变化.结果表明在这30年间,区域内冰川体积大约减少了36.25亿m3,相比整个高亚洲区域的冰川退缩速度,本区域冰川的退缩表现的更缓慢.然后,对内流区6个二级流域的冰川体积变化做了详细的对比分析,发现整个内流区冰川体积变化有较大的区域差别:其中5Z3流域冰川体积的退缩率最大,年均退缩率达-11.19%,而变化最小的5Z1流域年均变化率仅为-0.79%.各二级流域在体积变化方面的相同点是,体积退缩率均大于面积退缩率.通过对冰川面积、体积变化特点及其原因的分析,认为气候变化的区域差异是该区域内各二级流域冰川变化存在差异的主要原因.最后根据本文得到的结果,讨论了冰川体积变化对本区域的生态环境造成的影响.
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出版历程
收稿日期:  2013-05-08
修回日期:  2014-04-26
上线日期:  2014-05-20

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