ISSN 1003-8035 CN 11-2852/P

    融合极端降水数据的可解释机器学习在泥石流灾害风险预测中的应用以东川国家级重点泥石流灾害防治区为例

    Debris-Flow hazard prediction using interpretable machine learning integrated with extreme rainfall data: A case study of the national key debris-flow prevention and control area in Dongchuan district

    • 摘要: 针对机器学习模型“黑箱”特性导致地质灾害预测结果难以机理解释的问题,文章旨在融合极端降水数据,构建可解释的泥石流灾害风险预测框架,并定量识别关键致灾因子的敏感阈值。以云南省东川国家级重点泥石流灾害防治区为例,采用遗传算法进行特征筛选,结合孤立森林算法开展样本净化,构建XGBoost、LightGBM和CatBoost 3种梯度提升模型,经过贝叶斯优化确定最优超参数,最后引入SHAP框架进行全局与局部可解释性分析,解析极端降水因子与地形、地表变形因子对泥石流风险的非线性耦合作用。3个模型在测试集上的AUC均超过0.84,其中LightGBM的表现最优(AUC=0.860),XGBoost次之(0.858),CatBoost为0.842。SHAP分析揭示:①降水频率(强降水日数>18 d/a、连续5 d降水次数>28次/a)是首要驱动因子,其边际贡献显著高于降水强度;②坡度22°~28°为重力敏感区间,对高频降水致灾具显著的地形放大效应;③地表形变速率>9 mm/a为物源区失稳的早期预警阈值。本研究将“黑箱”预测模型转化为具有机理解析能力的可解释工具,所提取的长期气候背景阈值可为区域背景风险评估提供量化依据,为构建“背景风险评估+临灾触发预警”的分级防控体系提供方法支撑。

       

      Abstract: To address the limited physical interpretability of black-box machine-learning models in geohazard prediction, this study integrates extreme rainfall data to construct an interpretable debris-flow hazard prediction framework and quantitatively identify sensitive thresholds of key predisposing factors. The national key debris-flow prevention and control area in Dongchuan, Yunnan Province, was selected as the study area. A genetic algorithm was used for feature selection, and the Isolation Forest algorithm was used for sample purification. Three gradient-boosting models (XGBoost, LightGBM, and CatBoost) were constructed, and Bayesian optimization was applied to determine optimal hyperparameters. The SHAP framework was then introduced for global and local interpretability analysis to examine the nonlinear coupling effects of extreme rainfall factors with topographic and surface-deformation factors on debris-flow risk. All three models achieved test-set AUC values above 0.84. LightGBM performed best (AUC = 0.860), followed by XGBoost (0.858) and CatBoost (0.842). SHAP analysis showed that: (1) rainfall frequency (heavy-rainfall days > 18 d/a; consecutive 5-day rainfall events > 28 times/a) is the dominant driver, with a marginal contribution substantially greater than that of rainfall intensity; (2) slope angles of 22°-28° form a gravity-sensitive interval with pronounced topographic amplification under high-frequency rainfall; and (3) a surface deformation rate > 9 mm/a can serve as an early-warning threshold for source-area instability. This study transforms black-box prediction models into mechanism-interpretable tools. The extracted long-term climatic background thresholds provide quantitative support for regional background risk assessment and a methodological basis for building a hierarchical prevention and control system combining "background risk assessment" with "event-triggered early warning".

       

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