• 中国出版政府奖提名奖

    中国百强科技报刊

    湖北出版政府奖

    中国高校百佳科技期刊

    中国最美期刊

    Volume 41 Issue 5
    May  2016
    Turn off MathJax
    Article Contents
    Huai Baojuan, Li Zhongqin, Wang Feiteng, Wang Puyu, Li Kaiming, 2016. Ice Thickness Distribution and Ice Volume Estimation of Muz Taw Glacier in Sawir Mountains. Earth Science, 41(5): 757-764. doi: 10.3799/dqkx.2016.064
    Citation: Huai Baojuan, Li Zhongqin, Wang Feiteng, Wang Puyu, Li Kaiming, 2016. Ice Thickness Distribution and Ice Volume Estimation of Muz Taw Glacier in Sawir Mountains. Earth Science, 41(5): 757-764. doi: 10.3799/dqkx.2016.064

    Ice Thickness Distribution and Ice Volume Estimation of Muz Taw Glacier in Sawir Mountains

    doi: 10.3799/dqkx.2016.064
    • Received Date: 2016-01-12
    • Publish Date: 2016-05-15
    • Ice bedrock topographic map and ice volume estimation play very important parts in glacier melt water research. Muz Taw glacier in Sawir Mountains was explored in this study by means of Landsat remote sensing image, digital elevation model data, ground penetrating radar (GPR) data and GPS positioning data. Its terminus thickness distribution was obtained by analysis and simulation of thickness distribution of its transverse and vertical sections, combined with a variety of interpolation methods, on basis of which the ice volume was estimated. Results show obvious differences between the two transverse profiles. Cross-section B1-B2 has typical "U"-type terrain, with maximum glacier thickness of up to 116.4 m; cross-section C1-C2 is relatively flat, and glacier thickness distribution is more uniform, with an average of about 70-90 m. In longitudinal profile, A1-A2 forms a ladder-like distribution, with an obvious depression in the middle of the ice bed topography. The average ice thickness in longitudinal profile is about 80.89 m, with maximum ice thickness of 122.67 m. The ice bed topographic map is in sharp contrast with the thickness contour map of the glacier. In addition, there is obvious cirque terrain at an altitude of 3 240 m and 3 280 m. The preliminary estimation of the average thickness and total terminus ice volume are approximately 60.5 m and 0.195 km3, respectively. It is concluded that GPR method has higher accuracy compared with the traditional ice volume estimation method, but it has restrictions because of measurement difficulties

       

    • loading
    • Arendt, A., Echelmeyer, K., Harrison, W., et al., 2006.Updated Estimates of Glacier Volume Changes in the Western Chugach Mountains, Alaska, and a Comparison of Regional Extrapolation Methods.Journal of Geophysical Research, 111(F3):F03019.doi: 10.1029/2005jf000436
      Bauder, A., Funk, M., Huss, M., 2007.Ice-Volume Changes of Selected Glaciers in the Swiss Alps since the End of the 19th Century.Annals of Glaciology, 46(1):145-149.doi: 10.3189/172756407782871701
      Evans, S., 1963.Radio Techniques for the Measurement of Ice Thickness.Polar Record, 11(73):406-410.doi: 10.1017/s0032247400053523
      He, M.B., Sun, B., Yang, Y.X., et al., 2004.Ice Thickness Determination and Analysis of No.1 Glacier at the Source of Urumchi River, Tianshan by Ground Penetrating Radar.Journal of East China Institute of Technology, 27(3):235-239(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HDDZ200403006.htm
      Jia, L.L., Wang, H.S., Xiang, L.W., 2014.Uncertainty of Approximate Relationship between GIA Induced Viscous Gravity and Radial Displacement.Earth Science, 39(7):905-914(in Chinese with English abstract).
      Li, Z.Q., Wang, F.T., Zhu, G.C., et al., 2007.Basic Features of the Miaoergou Flat-Topped Glacier in East Tianshan Mountains and Its Thickness Change over the Past 24 Years.Journal of Glaciology and Geocryology, 29(1):61-65 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-BCDT200701009.htm
      Liu, C.H., You, G.X., Pu, J.C., 1982.Glacier Inventory of China Ⅱ:Altay Mountains.Lanzhou Institute of Glaciology and Cryopedology, Chinese Academy of Sciences, Lanzhou, 1-18(in Chinese).
      Liu, S.Y., Sun, W.X., Shen, Y.P., et al., 2003.Glacier Changes since the Little Ice Age Maximum in the Western Qilian Shan, Northwest China, and Consequences of Glacier Runoff for Water Supply.Journal of Glaciology, 49(164):117-124.doi: 10.3189/172756503781830926
      Ma, L.L., Tian, L.D., Pu, J.C., et al., 2010 Recent Area and Ice Volume Change of Kangwure Glacier in the Middle of Himalayas.Chinese Sci.Bull., 55(18):1766-1774(in Chinese). doi: 10.1007%2Fs11434-010-3211-7.pdf
      Ma, L.L., Tian, L.D., Yang, W., et al., 2008.Measuring the Depth of Gurenhekou Glacier in the South of the Tibetan Plateau Using GPR and Estimating Its Volume Based on the Outcomes.Journal of Glaciology and Geocryology, 30(5):783-788(in Chinese with English abstract).
      Nolan, M., Motkya, R.J., Echelmeyer, K., et al., 1995.Ice-Thickness Measurements of Taku Glacier, Alaska, USA and Their Relevance to Its Recent Behavior.Journal of Glaciology, 41(139):541-553. doi: 10.1017/S0022143000034870
      Paterson, W.S.B., 1994.The Physics of Glacier (Third Edition).Pergamon Press, Oxford, 238-288.
      Plewes, L.A., Hubbard, B., 2001.A Review of the Use of Radio-Echo Sounding in Glaciology.Progress in Physical Geography, 25(2):203-236.doi: 10.1191/030913301668581943
      Pu, J.C., Yao, T.D., Tian, L.D., 2006.Change of the Gurenhekou Glacier in Yangbajain Area, Nyainqêntanglha Range.Journal of Glaciology and Geocryology, 28(6):861-864(in Chinese with English abstract).
      Lanzhou Institute of Glaciology and Cryopedology, Chinese Academy of Sciences, 1988.An Introduction to the Glaciers in China.Science Press, Beijing, 92-93 (in Chinese).
      Shi, Y.F., 2001.Estimation of the Water Resources Affected by Climatic Warming and Glacier Shrinkage before 2050 in West China.Journal of Glaciology and Geocryology, 23(4):333-341 (in Chinese with English abstract). https://www.researchgate.net/publication/284332700_Estimation_of_the_water_resources_affected_by_climatic_warming_and_glacier_shrinkage_before_2050_in_west_China
      Shi, Y.F., 2005.Concise China Glacier Inventory.Shanghai Popular Science Press, Shanghai, 101-105 (in Chinese).
      Sun, B., He, M.B., Zhang, P., et al., 2003.Determination of Ice Thickness, Subice Topography and Ice Volume at Glacier No.1 in the Tien Shan, China, by Ground Penetrating Radar.Chinese Journal of Polar Research, 15(1):35-44(in Chinese with English abstract).
      Wang, N.L., Pu, J.C., 2009.Ice Thickness, Sounded by Ground Penetrating Radar, on the Bayi Glacier in the Qilian Mountains, China.Journal of Glaciology and Geocryology, 31(3):431-435(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-BCDT200903004.htm
      Wang, P.Y., Li, Z.Q., Li, H.L., et al., 2012.Changes of Ice-Thickness and Volume for Representative Glaciers in Tianshan Mountains in the Past 50 Years.Acta Geographica Sinica, 67(7):929-940 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DLXB201207007.htm
      Wang, Z.T., 1988.New Statistical Figures and Distribution Feature of Glaciers on the Various Mountains in China.Journal of Glaciology and Geocryology, 11(3):8-14 (in Chinese with English abstract).
      Wu, L.H., Li, Z.Q., Wang, P.Y., et al., 2011.Sounding the Sigong River Glacier No.4 in Mt.Bogda Area, the Tianshan Mountains by Using Ground Penetrating Radar and Estimating the Ice Volume.Journal of Glaciology and Geocryology, 33(2):276-282 (in Chinese with English abstract).
      Wu, Z., 2011.The Research of Ice-Thickness and Englacial Structure Base on Ground Penetration Radar(Dissertation).University of Chinese Academy of Sciences, Beijing (in Chinese with English abstract).
      Wu, Z., Liu, S.Y., Zhang, S.Q., 2009.Structural Characteristics of the No.12 Glacier in Laohugou Valley, Qilian Mountain Based on the Ground Penetrating Radar Sounding.Advances in Earth Science, 24(10):1049-1158 (in Chinese with English abstract). doi: 10.11867/j.issn.1001-8166.2011.06.0631
      Yan, Y.J., Yan, J.X., Wu, S.Q., 2015.Sedimentary Records of Early Permian Major Glacial Sea-Level Falls in Southern Guizhou Province, China.Earth Science, 40(2):372-380(in Chinese with English abstract). https://www.researchgate.net/publication/281751298_Sedimentary_records_of_early_permian_major_glacial_sea-level_falls_in_southern_Guizhou_Province_China
      Zhang, T., Xiao, C.D., Qin, X., et al., 2012. Ice Thickness Observation and Landform Study of East Rongbuk Glacier, Mt.Qomolangma.Journal of Glaciology and Geocryology, 34 (5):1069-1066 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-BCDT201205005.htm
      Zhang, X.S., Zhu, G.C., Qian, S.L., et al., 1985.Radar Measuring Ice Thickness of Glacier No.1 at the Source of Urumqi River, Tianshan.Journal of Glaciology and Geocryology, 7(2):153-162 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-BCDT198502006.htm
      Zhu, G.C., Jing, X.P., Han, J.K., et al., 1994.Radar Sounding and Study of the Bedrock Topography on Collins Ice Cap.Antarctic Research (Chinese Edition), 6(2):40-45(in Chinese with English abstract).
      Zhu, M.L., Yao, T.D., Yang, W., et al., 2014.Ice Volume and Characteristics of Sub-Glacial Topography of the Zhadang Glacier, Nyainqěntanglha Range.Journal of Glaciology and Geocryology, 36(2):268-277 (in Chinese with English abstract).
      何茂兵, 孙波, 杨亚新, 等, 2004.天山乌鲁木齐河源一号冰川探地雷达测厚及其数据分析.东华理工学院学报, 27(3):235-239. http://www.cnki.com.cn/Article/CJFDTOTAL-HDDZ200403006.htm
      贾路路, 汪汉胜, 相龙伟, 2014.冰川均衡调整重力与径向位移近似关系的不确定性.地球科学, 39(7):905-914. http://www.earth-science.net/WebPage/Article.aspx?id=2885
      李忠勤, 王飞腾, 朱国才, 等, 2007.天山庙尔沟平顶冰川的基本特征和过去24 a间的厚度变化.冰川冻土, 29(1):61-65. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT200701009.htm
      刘潮海, 尤根祥, 蒲健辰, 1982. 中国冰川目录Ⅱ: 阿尔泰山区. 兰州: 中国科学院兰州冰川冻土研究所, 1-18.
      马凌龙, 田立德, 蒲健辰, 等, 2010.喜马拉雅山中段抗物热冰川的面积和冰储量变化.科学通报, 55(18):1766-1774. http://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201018004.htm
      马凌龙, 田立德, 杨威, 等, 2008.青藏高原南部羊八井古仁河口冰川GPR测厚及冰川体积估算.冰川冻土, 30(5):783-788. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT200805011.htm
      蒲健辰, 姚檀栋, 田立德, 2006.念青唐古拉山羊八井附近古仁河口冰川的变化.冰川冻土, 28(6):861-864. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT200606009.htm
      施雅风, 2001.2050年前气候变暖冰川萎缩对水资源影响情景预估.冰川冻土, 23(4):333-341. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT200104000.htm
      施雅风, 2005.简明中国冰川目录.上海:上海科学普及出版社, 101-105.
      中国科学院兰州冰川冻土研究所, 1988.中国冰川概论.北京:科学出版社, 92-93.
      孙波, 何茂兵, 张鹏, 等, 2003.天山1号冰川厚度和冰下地形探测与冰储量分析.极地研究, 15(1):35-44. http://www.cnki.com.cn/Article/CJFDTOTAL-JDYZ200301004.htm
      王宁练, 蒲健辰, 2009.祁连山八一冰川雷达测厚与冰储量分析.冰川冻土, 31(3):431-435. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT200903004.htm
      王璞玉, 李忠勤, 李慧林, 等, 2012.近50年来天山地区典型冰川厚度及储量变化.地理学报, 67(7):929-940. doi: 10.11821/xb201207006
      王宗太, 1988.中国各山脉的冰川最新统计及其分布特征.冰川冻土, 11(3):8-14. http://www.cnki.com.cn/Article/CJFDTOTAL-GHDL198803001.htm
      吴利华, 李忠勤, 王璞玉, 等, 2011.天山博格达峰地区四工河4号冰川雷达测厚与冰储量估算.冰川冻土, 33(2):276-282. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201102010.htm
      武震, 2011. 探地雷达冰川测厚与储量估算(博士学位论文). 北京: 中国科学院大学.
      武震, 刘时银, 张世强, 2009.祁连山老虎沟12号冰川冰下形态特征分析.地球科学进展, 24(10):1049-1158. http://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200910013.htm
      严雅娟, 颜佳新, 武思琴, 2015.黔南地区早二叠世大幅度冰川性海平面下降的沉积学新证据.地球科学, 40(2):372-380. http://www.earth-science.net/WebPage/Article.aspx?id=3055
      张通, 效存德, 秦翔, 等, 2012.珠穆朗玛峰东绒布冰川厚度测量与地形特征分析.冰川冻土, 34(5):1069-1066. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201205005.htm
      张祥松, 朱国才, 钱嵩林, 等, 1985.天山乌鲁木齐河源1号冰川雷达测厚.冰川冻土, 7(2):153-162. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT198502006.htm
      朱国才, 井晓平, 韩建康, 等, 1994.柯林斯冰帽雷达测厚和冰下地形研究.南极研究, 6(2):40-45. http://www.cnki.com.cn/Article/CJFDTOTAL-JDYZ402.003.htm
      朱美林, 姚檀栋, 杨威, 等, 2014.念青唐古拉山扎当冰川冰储量估算及冰下地形特征分析.冰川冻土, 36(2):268-277. http://www.cnki.com.cn/Article/CJFDTOTAL-BCDT201402004.htm
    • 加载中

    Catalog

      通讯作者: 陈斌, bchen63@163.com
      • 1. 

        沈阳化工大学材料科学与工程学院 沈阳 110142

      1. 本站搜索
      2. 百度学术搜索
      3. 万方数据库搜索
      4. CNKI搜索

      Figures(7)  / Tables(2)

      Article views (4862) PDF downloads(40) Cited by()
      Proportional views

      /

      DownLoad:  Full-Size Img  PowerPoint
      Return
      Return