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Rock glacier inventory, permafrost probability distribution modeling and associated hazards in the Hunza River Basin, Western Karakoram, Pakistan

机译:岩石河流盆地,巴基斯坦西喀拉姆河流域岩石冰川库存,永久冻土概率分布建模与相关危害

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摘要

The destabilization of rock glaciers and permafrost variations is of great importance to the safety of the population and infrastructure in the Karakoram region because of their effects on land stability and river obstructions. In this study, we compiled the first complete rock glacier inventory for the Hunza Basin, western Karakoram, of 616 rock glaciers with an area of 194 km~2 between 2800 and 5700 m a.s.l. We categorized the rock glaciers as intact or relict, and their distributions and destabilization were further analyzed and used along with in situ climate and elevation dataset to model the permafrost probability distribution. The modeled areas where the permafrost zonation index (PZI) is 0.5-1.00 indicate that permafrost occurs over 85% of the catchment area and lies above 3525 m a.s.l., which closely matches the zero-degree isotherm of 3800 m a.s.l. Based on the sensitivity analysis of the independent variables, elevation is the most sensitive variable, followed by net radiation, for predicting the probabilities of the presence and absence of permafrost. The model distributions are quite precise, with median posterior areas under the curve of 0.98 and 0.96 for model training and testing, respectively. We analyzed the rock glacier destabilization for 68 rock glaciers that interacted with river channels, of which 50 blocked or diverted river channels. Destabilized rock glaciers can be closely linked to the 0 °C isotherm between 3400 and 4600 m a.s.l. The significant damage caused by periodic floods from the subsequent blockage of river channels by landslides can be attributed to variations in permafrost. Which demolished infrastructure, including a hydropower plant, suspension bridge and water supply system in Hassan-abad catchment. Quantification of rock glacier dynamics and permafrost in the region can further improve policies related to the reduction in disaster risk and mitigation of associated hazards.
机译:由于它们对土地稳定性和河流障碍物的影响,岩石冰川和永久冻土变化的破坏性非常重视人口和基础设施的安全性。在这项研究中,我们编制了616个岩石冰川的Hunza盆地的第一个完整的岩石冰川库存,其中616个岩石冰川,面积为194公里〜2至2800至5700米A.L.我们将岩石冰川分类为完整或封闭,并进一步分析其分布和稳定化以及原位气候和海拔数据集以模拟永久冻土概率分布。多冻区分区指数(PZI)为0.5-1.00的模型区域表明永久冻坏发生在集水区的85%以上,呈3525米A.L以上,其与3800米A.L的零度等温线相匹配。基于独立变量的敏感性分析,高程是最敏感的变量,其次是净辐射,用于预测存在和不存在永久冻土的概率。模型分布非常精确,分别在0.98和0.96的曲线下的中位后区域,分别用于模型训练和测试。我们分析了与河流渠道互动的68个岩石冰川的岩石冰川稳定化,其中50个被阻挡或转向的河流渠道。不稳定的岩石冰川可以与3400到4600米A.L之间的0°C等温线密切相关。由于山体滑坡随后堵塞河流渠道堵塞的周期性洪水造成的重大损害可归因于永久冻土的变化。其中拆除基础设施,包括哈桑阿巴斯集水区的水电站,悬架桥和供水系统。该地区岩石冰川动态和永久冻土的量化可以进一步改善与减少灾害风险和消除相关危害的政策。

著录项

  • 来源
    《Science of the total environment》 |2021年第15期|146833.1-146833.14|共14页
  • 作者单位

    Key Laboratory of Mountain Hazards and Earth Surface Process. Institute of Mountain Hazards and Environment Chinese Academy of Sciences Chengdu 610041 China University of Chinese Academy of Sciences Beijing 100049 China;

    Key Laboratory of Mountain Hazards and Earth Surface Process. Institute of Mountain Hazards and Environment Chinese Academy of Sciences Chengdu 610041 China CAS Centre for Excellence in Tibetan Plateau Earth Sciences Beijing 100101 China University of Chinese Academy of Sciences Beijing 100049 China;

    International Center for Integrated Mountain Development (ICIM0D) Kathmandu Nepal;

    Key Laboratory of Mountain Hazards and Earth Surface Process. Institute of Mountain Hazards and Environment Chinese Academy of Sciences Chengdu 610041 China University of Chinese Academy of Sciences Beijing 100049 China China-Pakistan Joint Research Center on Earth Science QAU Islamabad Pakistan;

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

    Rock glaciers; Permafrost; Karakoram; Cryospheric hazards; Climate change;

    机译:岩石冰川;永久冻土;喀喇昆仑;低铁危害;气候变化;

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