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首页> 外文期刊>Natural hazards and earth system sciences >Assessment of evolution and risks of glacier lake outbursts in the Djungarskiy Alatau, Central Asia, using Landsat imagery and glacier bed topography modelling
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Assessment of evolution and risks of glacier lake outbursts in the Djungarskiy Alatau, Central Asia, using Landsat imagery and glacier bed topography modelling

机译:利用Landsat Imagery和冰川地形建模,评估Djungarskiy Alatau Alatau Alatau Alatau Alatau冰川湖爆发的演变和风险

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Changes in the abundance and area of mountain lakes in the Djungarskiy (Jetysu) Alatau between 2002 and 2014 were investigated using Landsat imagery. The number of lakes increased by 6.2% from 599 to 636 with a growth rate of 0.51% a(-1). The combined areas were 16.26 +/- 0.85 to 17.35 +/- 0.92 km(2) respectively and the overall change was within the uncertainty of measurements. Fifty lakes, whose potential outburst can damage existing infrastructure, were identified. The glacier bed topography version 2 (GlabTop2) model was applied to simulate ice thickness and subglacial topography using glacier outlines for 2000 and SRTM DEM (Shuttle Radar Topography Mission digital elevation model) as input data achieving realistic patterns of ice thickness. A total of 513 overdeepenings in the modelled glacier beds, presenting potential sites for the development of lakes, were identified with a combined area of 14.7 km(2). Morphometric parameters of the modelled overdeepenings were close to those of the existing lakes. A comparison of locations of the overdeepenings and newly formed lakes in the areas deglacierized in 2000-2014 showed that 67% of the lakes developed at the sites of the overdeepenings. The rates of increase in areas of new lakes correlated with areas of modelled overdeepenings. Locations where hazardous lakes may develop in the future were identified. The GlabTop2 approach is shown to be a useful tool in hazard management providing data on the potential evolution of future lakes.
机译:使用Landsat Imagery调查了2002年至2014年间Djungarskiy(Jetysu)Alatau山湖丰富和面积的变化。湖泊的数量从599增加到636增加了6.2%,增长率为0.51%A(-1)。合并区域分别为16.26 +/- 0.85至17.35 +/- 0.92 km(2),整体变化在测量的不确定性范围内。确定了五十湖泊,其潜在的爆发可能会损害现有基础设施。冰川床地形版本2(GLABTOP2)模型应用于使用2000和SRTM DEM(班车雷达形状使命数字高级高级模型的冰川轮廓来模拟冰厚度和沉淀地形,作为实现冰厚度逼真模式的输入数据。建模冰川床上共有513个过度延长,呈现出湖泊发展的潜在地点,鉴定了14.7公里(2)的组合面积。模型过度透过的形态学参数接近现有湖泊的参数。 2000 - 2014年中来地区的过度延长和新成型湖泊的位置比较显示,67%的湖泊在过度透明的地点开发。新湖区地区的增加率与建模过度升高的区域相关。识别有害湖泊可能在未来发展的地方。 Glabtop2方法被证明是危险管理中的有用工具,提供有关未来湖泊的潜在演化的数据。

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