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乌兹别克斯坦的冰川湖目录和湖涌潜在风险。

Glacial lake inventory and lake outburst potential in Uzbekistan.

机构信息

Institute of Geology and Geophysics, Glacial-geology lab, Olimlar St. 49, 100041 Tashkent, Uzbekistan.

Institute of Geology and Geophysics, Glacial-geology lab, Olimlar St. 49, 100041 Tashkent, Uzbekistan; State University of New York College of Environmental Science and Forestry, Baker 402, 13210 Syracuse, NY, USA.

出版信息

Sci Total Environ. 2017 Aug 15;592:228-242. doi: 10.1016/j.scitotenv.2017.03.068. Epub 2017 Mar 17.

Abstract

Climate change has been shown to increase the number of mountain lakes across various mountain ranges in the World. In Central Asia, and in particular on the territory of Uzbekistan, a detailed assessment of glacier lakes and their evolution over time is, however lacking. For this reason we created the first detailed inventory of mountain lakes of Uzbekistan based on recent (2002-2014) satellite observations using WorldView-2, SPOT5, and IKONOS imagery with a spatial resolution from 2 to 10m. This record was complemented with data from field studies of the last 50years. The previous data were mostly in the form of inventories of lakes, available in Soviet archives, and primarily included localized in-situ data. The inventory of mountain lakes presented here, by contrast, includes an overview of all lakes of the territory of Uzbekistan. Lakes were considered if they were located at altitudes above 1500m and if lakes had an area exceeding 100m. As in other mountain regions of the World, the ongoing increase of air temperatures has led to an increase in lake number and area. Moreover, the frequency and overall number of lake outburst events have been on the rise as well. Therefore, we also present the first outburst assessment with an updated version of well-known approaches considering local climate features and event histories. As a result, out of the 242 lakes identified on the territory of Uzbekistan, 15% are considered prone to outburst, 10% of these lakes have been assigned low outburst potential and the remainder of the lakes have an average level of outburst potential. We conclude that the distribution of lakes by elevation shows a significant influence on lake area and hazard potential. No significant differences, by contrast, exist between the distribution of lake area, outburst potential, and lake location with respect to glaciers by regions.

摘要

气候变化已被证明会增加世界各地不同山脉的高山湖泊数量。然而,在中亚,尤其是在乌兹别克斯坦境内,缺乏对冰川湖及其随时间演变的详细评估。出于这个原因,我们利用 WorldView-2、SPOT5 和 IKONOS 卫星图像(空间分辨率为 2 到 10 米),根据最近(2002-2014 年)的卫星观测,首次详细编制了乌兹别克斯坦的高山湖泊清单。该记录还补充了过去 50 年实地研究的数据。以前的数据大多以苏联档案馆中湖泊清单的形式存在,主要包括局部实地数据。相比之下,这里呈现的高山湖泊清单包括了乌兹别克斯坦领土上所有湖泊的概述。如果湖泊位于海拔 1500 米以上,且面积超过 100 平方米,则被视为湖泊。与世界其他山区一样,空气温度的持续升高导致了湖泊数量和面积的增加。此外,湖溃决事件的频率和总数也在上升。因此,我们还根据当地气候特征和事件历史,利用广为人知的方法,首次对湖溃决事件进行了评估。结果,在乌兹别克斯坦境内确定的 242 个湖泊中,有 15%被认为容易发生湖溃决,其中 10%的湖泊湖溃决潜力较低,其余湖泊的湖溃决潜力平均。我们得出的结论是,按海拔分布的湖泊对湖泊面积和灾害潜力有显著影响。相比之下,湖泊面积、湖溃决潜力和湖泊与冰川位置的分布在区域上没有明显差异。

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