...
首页> 外文期刊>Geomorphology >Computational experiments on the 1962 and 1970 landslide events at Huascaran (Peru) with r.avaflow: Lessons learned for predictive mass flow simulations
【24h】

Computational experiments on the 1962 and 1970 landslide events at Huascaran (Peru) with r.avaflow: Lessons learned for predictive mass flow simulations

机译:利用r.avaflow对1962年和1970年在Huascaran(秘鲁)发生的滑坡事件进行的计算实验:有关预测质量流量模拟的经验教训

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Mass flow simulations are considered important tools for hazard analysis. For the simulation of single process mass flows such as debris flows, robust tools and reasonable parameter range estimates are available. However, this is much less the case for more complex mass flows, e.g. involving process chains and flow transformation. We explore the challenges of simulating complex flow-dominated landslides by back-calculating the Huascaran events of 1962 and 1970 with r.avaflow, a two-phase mass flow model (Pudasaini, 2012) in a GIS-based open source simulation framework. Both events started as rock-ice falls on the western slope of the north summit of Nevado Huascaran (Cordillera Blanca, Peru) and entrained large volumes of glacial till at lower elevation, resulting in highly mobile debris avalanches. Whereas the 1962 event badly affected the village of Ranrahirca when spreading over a debris cone, the 1970 event overtopped a ridge and led to the complete destruction of the town of Yungay. Well documented in the literature, these events provide an opportunity as a natural laboratory for testing innovative mass flow simulation tools and their features. In a first step, we consider (i) the 1962 event and (ii) the 1970 event separately, for each of them optimizing the key input parameters in terms of empirical adequacy. In a second step, we apply the optimized parameter set for (i) to the 1970 event and the parameter set derived for (ii) to the 1962 event. In a third step, we explore the sensitivity of the model outcomes to selected key parameters (basal friction angle and entrainment coefficient). The results (a) demonstrate the general ability of r.avaflow to reproduce the spatio-temporal evolution of flow heights and velocities as well as travel times and volumes of these complex mass flow events reasonably well; and (b) highlight the challenges and uncertainties involved in predictive simulations with parameter sets obtained from back-calculations. We suggest a strategy to appropriately deal with uncertain outcomes by superimposing the results of multiple simulations. (C) 2018 The Authors. Published by Elsevier B.V.
机译:质量流量模拟被认为是进行危害分析的重要工具。对于单过程质量流(如泥石流)的仿真,可以使用健壮的工具和合理的参数范围估计。但是,对于更复杂的质量流(例如,大流量)而言,情况要少得多。涉及流程链和流程转换。我们通过在基于GIS的开源仿真框架中使用两阶段质量流量模型r.avaflow反向计算1962年和1970年的Huascaran事件,探索了模拟复杂流量为主的滑坡的挑战。这两个事件都是在冰冰从内华达·瓦斯卡兰(Cevillera Blanca,秘鲁)北山顶的西坡上滑落,并夹带大量冰川直到较低海拔,导致高度流动的碎屑雪崩而开始的。 1962年的事件在乱石堆上蔓延时严重影响了Ranrahirca村,而1970年的事件则越过山脊,导致Yungay镇被彻底摧毁。这些事件在文献中有充分的记载,这些活动为自然实验室提供了一个机会来测试创新的质量流模拟工具及其功能。第一步,我们分别考虑(i)1962年事件和(ii)1970年事件,因为它们每个人都根据经验充足性优化了关键输入参数。在第二步中,我们将(i)的优化参数集应用于1970年事件,将(ii)的派生参数集应用于1962年事件。第三步,我们探索模型结果对所选关键参数(基础摩擦角和夹带系数)的敏感性。结果(a)证明了r.avaflow能够很好地再现流高和速度的时空演变以及这些复杂质量流事件的传播时间和体积的一般能力; (b)突出了通过反向计算获得的参数集在预测模拟中所面临的挑战和不确定性。我们建议一种通过叠加多个模拟结果来适当处理不确定结果的策略。 (C)2018作者。由Elsevier B.V.发布

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号