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An inventory of glacial lakes in the Third Pole region and their changes in response to global warming

机译:第三极地区冰川湖泊的清单及其对全球变暖的响应

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摘要

No glacial lake census exists for the Third Pole region, which includes the Pamir-Hindu Kush-Karakoram-Himalayas and the Tibetan Plateau. Therefore, comprehensive information is lacking about the distribution of and changes in glacial lakes caused by current global warming conditions. In this study, the first glacial lake inventories for the Third Pole were conducted for similar to 1990, 2000, and 2010 using Landsat TM/ETM + data. Glacial lake spatial distributions, corresponding areas and temporal changes were examined. The significant results are as follows. (1) There were 4602, 4981, and 5701 glacial lakes (> 0.003 km(2)) covering areas of 553.9 +/- 90, 581.2 +/- 97, and 682.4 +/- 110 km(2) in similar to 1990, 2000, and 2010, respectively; these lakes are primarily located in the Brahmaputra (39%), Indus (28%), and Amu Darya (10%) basins. (2) Small lakes (< 0.2 km(2)) are more sensitive to climate changes. (3) Lakes closer to glaciers and at higher altitudes, particularly those connected to glacier termini, have undergone larger area changes. (4) Glacier-fed lakes are dominant in both quantity and area (> 70%) and exhibit faster expansion trends overall compared to non-glacier-fed lakes. We conclude that glacier meltwater may play a dominant role in the areal expansion of most glacial lakes in the Third Pole. In addition, the patterns of the glacier-fed lakes correspond well with warming temperature trends and negative glacier mass balance patterns. This paper presents an important database of glacial lakes and provides a basis for long-term monitoring and evaluation of outburst flood disasters primarily caused by glacial lakes in the Third Pole. (C) 2015 Elsevier B.V. All rights reserved.
机译:第三极地区没有冰川湖普查,包括帕米尔-印度都库什-卡拉科拉姆-喜马拉雅山和青藏高原。因此,缺乏关于由当前全球变暖条件引起的冰川湖的分布和变化的综合信息。在这项研究中,使用Landsat TM / ETM +数据对1990年,2000年和2010年进行了第三极的第一个冰川湖清查。研究了冰川湖的空间分布,相应区域和时间变化。主要结果如下。 (1)与1990年相似,有4602、4981和5701个冰川湖(> 0.003 km(2))覆盖了553.9 +/- 90、581.2 +/- 97和682.4 +/- 110 km(2) ,2000和2010;这些湖泊主要位于布拉马普特拉(39%),印度河(28%)和阿姆达里亚(10%)盆地。 (2)小湖(<0.2 km(2))对气候变化更为敏感。 (3)距冰川较近,海拔较高的湖泊,特别是与冰川终点相连的湖泊,面积变化较大。 (4)与非冰川湖相比,冰川湖在数量和面积上都占主导地位(> 70%),总体上呈现出更快的扩张趋势。我们得出结论,冰川融水可能在第三极大多数冰川湖的面积扩展中起主导作用。此外,冰川湖的格局与温度升高趋势和负的冰川质量平衡格局非常吻合。本文提供了一个重要的冰川湖数据库,并为长期监测和评估主要由第三极冰川湖造成的爆发洪水灾害提供了基础。 (C)2015 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《Global and planetary change》 |2015年第8期|148-157|共10页
  • 作者单位

    Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;

    Univ Texas San Antonio, Lab Remote Sensing & Geoinformat, San Antonio, TX 78249 USA;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China;

    Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China|CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China;

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

    Glacial lake inventory; Glacier-fed lakes; Third Pole; Global warming;

    机译:冰河湖库存;冰河湖;第三极;全球变暖;

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