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    GPR,GPS与GIS支持下的冰川厚度及冰储量分析:以天山博格达峰黑沟8号冰川为例

    王璞玉 李忠勤 吴利华 李慧林 王文彬 金爽 周平

    王璞玉, 李忠勤, 吴利华, 李慧林, 王文彬, 金爽, 周平, 2012. GPR,GPS与GIS支持下的冰川厚度及冰储量分析:以天山博格达峰黑沟8号冰川为例. 地球科学, 37(S1): 179-187. doi: 10.3799/dqkx.2012.S1.018
    引用本文: 王璞玉, 李忠勤, 吴利华, 李慧林, 王文彬, 金爽, 周平, 2012. GPR,GPS与GIS支持下的冰川厚度及冰储量分析:以天山博格达峰黑沟8号冰川为例. 地球科学, 37(S1): 179-187. doi: 10.3799/dqkx.2012.S1.018
    WANG Pu-yu, LI Zhong-qin, WU Li-hua, LI Hui-lin, WANG Wen-bin, JIN Shuang, ZHOU Ping, 2012. Ice Thickness and Volume Based on GPR, GPS and GIS: Example from the Heigou Glacier No.8, Bogda-Peak Region, Tianshan, China. Earth Science, 37(S1): 179-187. doi: 10.3799/dqkx.2012.S1.018
    Citation: WANG Pu-yu, LI Zhong-qin, WU Li-hua, LI Hui-lin, WANG Wen-bin, JIN Shuang, ZHOU Ping, 2012. Ice Thickness and Volume Based on GPR, GPS and GIS: Example from the Heigou Glacier No.8, Bogda-Peak Region, Tianshan, China. Earth Science, 37(S1): 179-187. doi: 10.3799/dqkx.2012.S1.018

    GPR,GPS与GIS支持下的冰川厚度及冰储量分析:以天山博格达峰黑沟8号冰川为例

    doi: 10.3799/dqkx.2012.S1.018
    基金项目: 

    国家重点基础研究发展计划 2010CB951003

    中国科学院知识创新工程重要方向项目 KZCX2-YW-127

    国家自然科学基金项目 40631001

    国家自然科学基金项目 40701034

    国家自然科学基金项目 J0630966

    国家自然科学基金项目 41001040

    国家自然科学基金项目 41101066

    详细信息
      作者简介:

      王璞玉(1983-),女,助理研究员,主要从事冰川变化与环境研究.E-mail: wangpuyu@lzb.ac.cn

    • 中图分类号: P343.6

    Ice Thickness and Volume Based on GPR, GPS and GIS: Example from the Heigou Glacier No.8, Bogda-Peak Region, Tianshan, China

    • 摘要: 本研究以天山博格达峰黑沟8号冰川为例,基于2009年探地雷达(GPR)冰川厚度测量资料以及高精度RTK-GPS(全球定位系统)定位数据,在地理信息系统(GIS)技术的支持下,开展了冰川厚度分布、冰储量分析及其变化特征研究.结果表明,黑沟8号冰川冰舌平均厚度为58.7 m,冰储量为115.1×106 m3,相当于水量103.5×106 m3;1986—2009年,冰舌平均减薄13±6 m,年均减薄约0.57±0.26 m,冰储量亏损达(25.5±11.8)×106 m3((22.9±10.6)×106 m3水当量),是该区气温显著升高的结果.相比反距离加权法和径向基函数法,普通克里格法插值精度较高(计算误差均值:-0.166 5;误差均方根:2.822),更适合于黑沟8号此类山地冰川的厚度分布研究;该冰川减薄速率与中国西部典型监测冰川近几十年的变化基本保持一致.本项研究将GPR、GPS和GIS技术综合运用于冰川学领域,可以有效解决数据获取、精确定位、空间分析等一系列问题,具有广阔的应用前景.

       

    • 图  1  黑沟8号冰川位置

      Fig.  1.  Location map of Heigou glacier No.8

      图  2  黑沟8号冰川雷达测厚路线分布

      Fig.  2.  GPR measuring lines of Heigou glacier No.8

      图  3  黑沟8号冰川C1-C2测线雷达图像

      Fig.  3.  Radar image along the sounding transect C1-C2 on Heigou glacier No.8

      图  4  基于普通克里格法的黑沟8号冰川冰舌厚度分布及1962—2009年冰川末端变化

      Fig.  4.  Ice thickness isoline map of Heigou glacier No.8 using ordinary kriging interpolation method and the terminus change from 1962 to 2009

      表  1  冰川厚度不同方法插值结果比较

      Table  1.   Comparison of ice thickness using different interpolation methods

      插值方法 参数模型 误差均值(MEAN) 误差均方根(RMS)
      反距离加权法(IDW) 指数为2 -0.785 0 7.663
      径向基函数法(RBF) 函数参数为35.715 -0.800 2 6.795
      普通克里格方法(OK) - -0.166 5 2.822
      下载: 导出CSV

      表  2  我国西部典型监测冰川近几十年变化比较

      Table  2.   Comparison of the changes of the typical monitored glaciers in western China in recent years

      冰川名称 位置 末端海拔(m) 厚度变化 面积变化 末端变化 资料来源
      时间段 年均减薄(m·a-1) 时间段 年均(km2·a-1) 时间段 年均(m·a-1)
      黑沟8号冰川 43°46'N, 88°23"E 3 380 1986——2009 0.57±0.26 (冰舌) 1962——2009 -0.002(冰舌) 1962——2009
      1959——1993
      -11
      -4.5
      本研究
      乌鲁木齐河源1号冰川 43°06'N, 86°49'E 3 736 1981——2006 0.40~0.72 (东支中轴线剖面) 1962——2006 -0.006 1993——2004 -3.5(东支)
      -5.8(西支)
      李忠勤等, 2007a
      科其喀尔冰川 41°49'N, 80°10'E 3 060 1981——2004 0.5~1.5 (冰舌) - 1974——2004 -12.7 谢昌卫等, 2006
      哈密庙尔沟冰川 43°03'N, 94°19'E 3 840 1981——2005 0.21 (海拔4295~4 357 m) - - 李忠勤等, 2007b
      海螺沟冰川 29°36'N, 101°57'E 2 910 1966——2009 1.1±0.4 - - Zhang et al., 2010
      下载: 导出CSV
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    出版历程
    • 收稿日期:  2011-09-05
    • 网络出版日期:  2021-11-15
    • 刊出日期:  2012-05-01

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