ISSN 1003-8035 CN 11-2852/P

    基于时间外推验证的震后泥石流动态易发性评价

    Dynamic susceptibility assessment of post-earthquake debris flows based on temporal extrapolation validation

    • 摘要: 震后山区泥石流孕灾环境呈阶段性演化,传统泥石流易发性评估多依赖随机抽样或交叉验证,难以检验模型的跨期预测能力与可迁移性。对此,本文引入时间外推验证框架,开展震后泥石流动态易发性评估。以四川省汶川县映秀镇为研究区,选取2010年“8•13”、2013年“7•10”和2019年“8•20”三次群发性泥石流事件,构建含稳定因子与时变因子的事件情景型易发性指标体系。采用随机森林模型,并引入特征重要性筛选关键因子,提出融合召回率和精确度的决策阈值优化策略。以2010年和2013年样本训练模型,外推至2019年事件进行独立验证。结果表明,阈值优化后,模型测试集上的性能为:Re=0.90,Pre=0.41,F1=0.56。相比应用原始阈值时,测试集的Pre=0.33,F1=0.48,校正后,Pre提升了24 %,F1提升了17 %。这种策略有效提升了预警信息的可信度,能显著减少不必要的预警和资源消耗。此外,不同时期高与极高易发区域在空间分布上随时间变化显著,实际泥石流多位于该类流域。文章提出的易发性评估框架为震后泥石流存在跨时间尺度的判别提供了可行的技术方案,可为震后泥石流动态易发性评估提供参考。

       

      Abstract: The disaster-forming environment of post-earthquake debris flows in mountainous areas exhibits staged evolution. Traditional debris flow susceptibility assessments mostly rely on random sampling or cross-validation, which is difficult to test the inter-temporal prediction ability and transferability of models. To solve this problem, this paper introduces a temporal-extrapolation validation framework to carry out dynamic susceptibility assessment of post-earthquake debris flows. Taking Yingxiu Town, Wenchuan County, Sichuan Province as the study area, three clustered debris flow events (the “August 13” event in 2010, the “July 10” event in 2013, and the “August 20” event in 2019) were selected to construct an event-scenario susceptibility index system including stable factors and time-varying factors. The Random Forest model was used, and key factors were screened through feature importance. A decision threshold optimization strategy integrating recall and precision was proposed. The model was trained with samples from 2010 and 2013, and extrapolated to the 2019 event for independent validation. The results show that after threshold optimization, the model performance on the test set is: Re =0.90, Pre=0.41, F1 = 0.56. Compared with the original threshold (Pre = 0.33, F1 = 0.48), the Pre is increased by 24 % and F1 by 17 % after calibration. This strategy effectively improves the reliability of early warning information and can significantly reduce unnecessary early warnings and resource consumption. In addition, the spatial distribution of high and very high susceptibility zones varies significantly over time, and actual debris flow are mostly located in such watersheds. The susceptibility assessment framework proposed in this study provides a feasible technical solution for cross-temporal identification of post-earthquake debris flows, and can provide a reference for dynamic susceptibility assessment of post-earthquake debris flows.

       

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