ISSN 1003-8035 CN 11-2852/P

    西藏地区冰崩灾害研究进展

    Advances in the study of glacier avalanches in Tibet

    • 摘要: 随着全球气候的变暖,青藏高原地区冰川消融、退缩加剧,稳定性降低,增加了冰崩灾害的发生频率。西藏地区作为青藏高原的主体部分,其冰川的稳定影响着我国及周边国家的水源及生命财产安全。文章通过梳理国内外冰崩的研究现状,整理了西藏地区冰崩灾害的定义;从地形因素、构造运动和气候作用角度分析了冰崩形成机制;归纳分析了冰崩—冰湖溃决—泥石流链式灾害、冰崩—堵溃—泥石流链式灾害、冰崩—直接型泥石流(山洪)灾害3种类型冰崩灾害链的特征;阐述了目前冰崩灾害监测预警的手段及特点,认为多种监测方式联合是冰崩灾害监测的发展趋势,展望了冰崩灾害的研究体系,以期能为后续的研究工作提供思路。

       

      Abstract: With the global warming, glaciers in the Qinghai-Tibet Plateau are melting and retreating rapidly, and the stability of glaciers are decreasing. As the main part of the Qinghai-Tibet Plateau, stability of glaciers affect the safety of water, life and property in China and neighboring countries. This paper summarized the research status of ice avalanches at home and abroad, and reorganized the definition of ice avalanche disasters in Tibet; Analyzed the formation mechanism of ice avalanche from the topography, tectonic movement and climate; Summarized and analyzed the characteristics of three types of ice avalanche disaster chains. Ice avalanche- glacial lake outburst- debris flow chain disaster, ice avalanche-blocking and outburst - debris flow chain disaster, ice avalanche-debris flow (flash flood) chain disaster; Described the current methods and characteristics of ice avalanche disasters monitoring and warning, and it is believed that the trend is for a combination of multiple monitoring methods for ice avalanche disaster monitoring. The research system of ice avalanche disasters is prospected in order to provide ideas for future research work.

       

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