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Changes in the glacier extent and surface elevation in Xiongcaigangri region, Southern Karakoram Mountains, China

机译:喀喇昆仑山南部雄蔡岗里地区冰川范围和地表海拔的变化

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摘要

The recent evolution of the Karakoram glaciers, widely acknowledged as peculiar, remains poorly understood. The Xiongcaigangri region is in the south of Karakoram, and its glacial melt water has a significant impact on the local water supply and ecosystem. In this work, glacial changes in the Xiongcaigangri region were detected based on topographic maps and Landsat MSS/TM/ETM+/OLI, SRTM4.1 DEM and Glas/ICESat remote sensing data and GIS techniques. The results show that from 1968 to 2013, the total glacier area decreased from 181.10 km(2) to 178.47 km(2), an overall loss of 2.63 km(2), or 1.45% of the entire 1968 glacial area. The inverse relationship between the retreating area and the change rate indicates that small glaciers may be retreating faster. The main glacial melting occurred below 6500 m a.s.l, and the reduction of 2.62 km(2) accounts for 99.62% of the total glacial retreat in the area studied. The very slight reduction of 0.01 km(2) over 6500 m a.s.l accounts for only for 0.38% of the total glacial retreat in the area studied. The results also show that the glacier areas are decreasing on all slopes, and larger area losses have been observed on smaller slopes, whereas smaller area losses have been observed on the larger slopes. The different aspects of the study all showed glacier retreat taking place between the period from 1968 to 2013. The largest area decrease is in west, and the area lost in the other aspect was comparatively small. Total glacier mass loss in the Xiongcaigangri region is estimated to be (10.97 +/- 22.39) 10(8) m(3) w.e. between 1968 and 2000. The average elevation loss estimated from the ICESat and 2000 SRTM difference was from -4.69-3.40 m per year, and the average elevation loss between SRTM and 1968DEM was from -0.92 to 0.66 m per year. Increasing temperatures along with decreasing precipitation was determined to be the primary factor driving the glacier retreat in the Xiongcaigangri region. (C) 2014 Elsevier Ltd and INQUA. All rights reserved.
机译:喀喇昆仑冰川最近的演变,人们普遍认为它是奇特的,但人们对此知之甚少。雄才岗里地区位于喀喇昆仑山脉的南部,其冰川融水对当地的水供应和生态系统具有重大影响。在这项工作中,根据地形图和Landsat MSS / TM / ETM + / OLI,SRTM4.1 DEM和Glas / ICESat遥感数据和GIS技术,检测了雄彩岗里地区的冰川变化。结果表明,从1968年到2013年,冰川总面积从181.10 km(2)减少到178.47 km(2),总损失为2.63 km(2),占1968年整个冰川面积的1.45%。退缩面积与变化率之间的反比关系表明,小冰川退缩速度可能更快。主要的冰川融化发生在6500 m a.s.l以下,减少的2.62 km(2)占该地区冰川撤退总量的99.62%。在6500 m a.s.l中,0.01 km(2)的极小减小仅占所研究地区冰川退缩总量的0.38%。结果还表明,冰川面积在所有斜坡上都在减少,在较小的斜坡上观察到较大的面积损失,而在较大的斜坡上观察到较小的面积损失。研究的各个方面都显示了在1968年至2013年之间发生了冰川退缩。最大的面积减少出现在西部,而其他方面的损失面积则相对较小。熊蔡岗里地区的冰川总质量损失估计为(10.97 +/- 22.39)10(8)m(3)w.e.在1968年至2000年之间。根据ICESat和2000 SRTM差异估算的平均高程损失为每年-4.69-3.40 m,而SRTM和1968DEM之间的平均高程损失为每年-0.92至0.66 m。确定温度升高和降水减少是导致熊蔡岗里地区冰川退缩的主要因素。 (C)2014 Elsevier Ltd和INQUA。版权所有。

著录项

  • 来源
    《Quaternary International》 |2015年第12期|67-75|共9页
  • 作者单位

    Shangqiu Normal Univ, Coll Environm & Planning, Shangqiu 476000, Peoples R China|Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing, Peoples R China;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Beijing, Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Glacier variations; Remote sensing; Southern Karakoram; Xiongcaigangri region;

    机译:冰川变化遥感喀喇昆仑南部雄才岗里地区;

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