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Changes of six selected glaciers in the Tomor region, Tian Shan, Central Asia, over the past ~ 50 years, using high-resolution remote sensing images and field surveying

机译:使用高分辨率遥感影像和实地调查,在过去〜50年中,中亚天山托莫地区的六个选定冰川的变化

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摘要

As the major water resource of the Tarim River, glaciers in the Tomor region have suffered major losses of ice in the last several decades. Based on topographic maps, high-resolution remote sensing image, field survey data and previous studies, changes of the six selected glaciers in the Tomor region (Qingbingtan Glacier No.72, Qjngbingtan Glacier No.74, Keqikekuzibayi Glacier, Tomor Glacier, Keqikar Glacier and Qiongtailan Glacier) over the past ~50 years were analyzed in this study. Analysis shows that all of the six glaciers showed continuous shrinkage. The reduction rate of Glacier No.72 (terminus retreat of 41 m a~(-1) and area loss of 21.5% during 1964-2009) was higher than the others, with a dramatically increased rate. This dramatic ice thinning, related glacier front retreat and area loss of the six glaciers, suggests that glaciers in the Tomor region might currently be suffering negative mass balance in response to the ongoing temperature rise. Differences in changes of the six glaciers are influenced by debris cover and other topographical factors.
机译:作为塔里木河(Tarim River)的主要水资源,托莫地区的冰川在过去的几十年中遭受了巨大的冰灾。根据地形图,高分辨率遥感影像,野外调查数据和先前的研究,对托莫地区的六个选定冰川(青冰滩72号,青炳潭74号,克基库库兹巴伊冰川,托莫尔冰川,科奇卡卡尔冰川)进行了变化。本研究分析了过去〜50年间的琼斯和琼塔拉扬冰川。分析表明,所有六个冰川都显示出持续的收缩。 No.72冰川(1964-2009年末期退缩量为41 m a〜(-1),面积损失为21.5%)的降低率要比其他冰川高,并且急剧增加。急剧的冰川变薄,相关的冰川前部退缩和六座冰川的面积减少表明,托莫地区的冰川目前可能因温度持续升高而处于负质量平衡状态。六个冰川变化的差异受碎片覆盖和其他地形因素的影响。

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  • 来源
    《Quaternary International》 |2013年第17期|123-131|共9页
  • 作者单位

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute/Tianshan Gladological Station, Chinese Academy of Sciences, Donggang West Road 320#, Lanzhou 730070, China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute/Tianshan Gladological Station, Chinese Academy of Sciences, Donggang West Road 320#, Lanzhou 730070, China,College of Geography and Environment Science, Northwest Normal University, Lanzhou 730070, China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute/Tianshan Gladological Station, Chinese Academy of Sciences, Donggang West Road 320#, Lanzhou 730070, China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute/Tianshan Gladological Station, Chinese Academy of Sciences, Donggang West Road 320#, Lanzhou 730070, China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute/Tianshan Gladological Station, Chinese Academy of Sciences, Donggang West Road 320#, Lanzhou 730070, China;

    State Key Laboratory of Cryospheric Sciences, Cold and Arid Regions Environmental and Engineering Research Institute/Tianshan Gladological Station, Chinese Academy of Sciences, Donggang West Road 320#, Lanzhou 730070, China;

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