ISSN 1003-8035 CN 11-2852/P

    青藏高原沟槽型雪崩动力学过程RAMMS与R.avaflow模型数值模拟对比分析

    Comparative Numerical Simulation of Gully-Type Avalanche Dynamics on the Tibetan Plateau Using RAMMS and R.avaflow

    • 摘要:
      目的 雪崩灾害严重威胁着青藏高原复杂地形区的工程安全与防灾减灾工作,高精度的数值模拟是进行雪崩灾害风险评估和防治的关键。
      方法 本研究以西藏波密县与墨脱县交界处嘎隆拉山区的某一典型沟槽型雪崩为研究对象,综合利用野外调查、遥感解译数据及高精度的数字高程模型,基于RAMMS和R.avaflow两种雪崩动力学模拟模型,重点分析了雪崩的运动过程、流速、压力和流高等关键动力学特征,并对比分析了在长路径、大高差、沟槽约束显著的场景下2种模型的应用效果与模拟差异。
      结果 结果表明,R.avaflow模拟结果显示的最大流速、流高、压力和总时长普遍高于RAMMS模拟结果;而在空间叠加验证方面,RAMMS模型在堆积区和流通区扩展范围的模拟结果均优于R.avaflow模型。
      结论 本研究通过典型雪崩案例的动力学特征的模拟对比分析,可以为特定场景下选取合适的雪崩模拟评估工具提供了参考,对提升青藏高原地区雪崩灾害的风险管控能力具有一定的理论价值和实际意义。

       

      Abstract:
      Objective Avalanches seriously threaten engineering safety and disaster prevention and mitigation in the complex terrain of the Tibetan Plateau. High-precision numerical simulation is essential for avalanche-hazard risk assessment and prevention.
      Methods This study focuses on a typical gully-type avalanche in the Galongla Mountain area on the border between Bome County and Medog County, Tibet. Field investigation, remote-sensing interpretation, and a high-resolution digital elevation model was integrated, and two avalanche-dynamics simulation models, RAMMS and R.avaflow, were used to analyze key dynamic characteristics, including movement process, flow velocity, pressure, and flow height. The applicability and simulation differences of the two models were compared for a long-runout, large-relief scenario with strong gully confinement.
      Results The results show that R.avaflow generally produces higher maximum velocity, flow height, pressure, and total duration than RAMMS. In spatial overlay validation, however, RAMMS better reproduces the extent of the accumulation and transport zones than R.avaflow.
      Conclusions Through comparative simulation of the dynamic characteristics of a typical avalanche case, this study provides a reference for selecting appropriate avalanche simulation tools under specific scenarios and has theoretical and practical significance for improving avalanche-risk management on the Tibetan Plateau.

       

    /

    返回文章
    返回