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Variations of Laohugou Glacier No.12 in the western Qilian Mountains, China, from 1957 to 2015

机译:1957年至2015年中国西部祁连山老虎沟12号冰川的变化

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摘要

Glaciers were solid reservoirs and important water resources in western China,but they were retreating significantly in context of global warming.Laohugou Glacier No.12 was the largest valley glacier in Qilian Mountains.In this study,realtime kinematic (RTK) data,topographic map and WoddView-2 satellite imagery were used to measure changes in terminus,extent and volume of Laohugou Glacier No.12.Results showed that Laohugou Glacier No.12 was shrinking significantly since 1957.From 1960 to 2015,the terminus reduction of Laohugou Glacier No.12 was 402.96 m (3.99%) in total,and glacier length decreased to 9.7 km from 10.1 km.Reductio of glacier area and volume were the most obvious.From 1957 to 2015,glacier area and volume decreased by 1.54 km2 (7.03%) and 0.1816 km3,respectively.Reduction trend of terminus and area was slowing in 1950-1980s,even stable for a period in the mid-1980s,and then accelerated.Ice core analysis result and nearly meteorological station data shown an increasing trend of temperature in 1957-2015,it was a main reason of continuous retreating of Laohugou Glacier No.12.
机译:冰川是中国西部的固体水库和重要水资源,但在全球变暖的背景下它们正在显着退缩。老虎沟十二号冰川是祁连山最大的山谷冰川。在本研究中,实时运动(RTK)数据,地形图和WoddView-2卫星图像分别用于测量老虎沟12号冰川的终点,范围和体积的变化。结果表明,老虎沟12号冰川自1957年以来一直在明显缩小.1960年至2015年,老虎沟2号冰川终点减少。 .12为402.96 m(3.99%),冰川长度从10.1 km减小到9.7 km。冰川面积和体积的减少最为明显。从1957年到2015年,冰川面积和体积减少了1.54 km2(7.03%)。 1950-1980年代终点和面积的减少趋势减缓,在1980年代中期甚至稳定下来,然后再加速。冰芯分析结果和近气象台数据显示tre增加1957-2015年气温升高是老虎沟十二号冰川连续退缩的主要原因。

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  • 来源
    《山地科学学报(英文版)》 |2018年第1期|25-32|共8页
  • 作者单位

    State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Qilian Shan Station of Glaciology and Ecologic Environment, Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Qilian Shan Station of Glaciology and Ecologic Environment, Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Qilian Shan Station of Glaciology and Ecologic Environment, Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Geomatics Center of Gansu Province, Gansu Bureau of Surveying, Mapping and Geoinformation, Lanzhou, Gansu 730000,China;

    Geomatics Center of Gansu Province, Gansu Bureau of Surveying, Mapping and Geoinformation, Lanzhou, Gansu 730000,China;

    State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    Qilian Shan Station of Glaciology and Ecologic Environment, Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

    State Key Laboratory of Cryospheric Science, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 eng
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