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Hazard assessment of glacial lake outburst floods from Kyagar glacier, Karakoram mountains, China

机译:中国喀喇昆仑山脉喀尔加尔冰川冰川湖爆发洪水的危害评估

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摘要

Kyagar glacier is located in the Chinese Karakoram mountains. The glacier tongue entirely blocks the riverbed in the upper Shaksgam valley and impounds a glacial lake, which was the source of several violent and disastrous glacial lake outburst floods (GLOFs). A GLOF early warning system was implemented between 2011 and 2013. We present an integrative analysis of the hazard potential of Kyagar lake, taking into account the ice flow dynamics of Kyagar glacier as well as the recent surface mass-balance response to climate change. Comparison of two high-resolution digital elevation models (DEMs) for the ice dam shows surface lowering rates of >5 m a–1 between 2002 and 2011, leading to a significant reduction in the maximum potential lake volume. However, two DEMs covering the entire glacier for the period 2000–10 indicate mass gains in its central part, and flow speed measurements show an acceleration in this region. This pattern of local ice-thickness changes combined with varying ice flow velocities is typical for surge-type glaciers. The velocity of the glacier surface and of the ice dam between 2011 and 2012 are analyzed at high temporal and spatial resolution, based on feature tracking of synthetic aperture radar (SAR) images.
机译:Kyagar冰川位于中国喀喇昆仑山脉。冰川的舌头完全堵住了Shaksgam山谷上游的河床,并蓄积了冰川湖,而冰川湖是几次暴力和灾难性的冰川湖爆发洪水(GLOF)的源头。 GLOF预警系统已在2011年至2013年间实施。我们结合Kyagar冰川的冰流动态以及最近对气候变化的地表质量平衡响应,对Kyagar湖的潜在危害进行了综合分析。两种用于冰坝的高分辨率数字高程模型(DEM)的比较显示,在2002年至2011年之间,地表降落率> 5 m a-1,从而导致最大潜在湖泊蓄水量大大减少。但是,在2000-10年期间,覆盖整个冰川的两个DEM指示了其中心部分的质量增加,而流速测量表明该区域的加速度。这种局部冰厚度变化的模式与变化的冰流速度相结合是浪涌型冰川的典型特征。基于合成孔径雷达(SAR)图像的特征跟踪,以高时空分辨率分析了2011年至2012年之间的冰川表面和冰坝的速度。

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