基于自适应多尺度传递熵的径流突变智能识别方法

    An intelligent method for runoff mutation detection based on adaptive multi-scale transfer entropy

    • 摘要: 全球气候变化与人类活动加剧背景下,径流系统突变特征日益显著,准确识别径流突变对流域水资源管理具有重要意义。传统Mann-Kendall等统计方法仅基于单变量分析,难以刻画多因子非线性耦合关系。本研究提出基于自适应多尺度传递熵(AMSTE)的径流突变智能识别方法,首次将变分模态分解与传递熵理论相结合,构建多尺度因果关系分析框架。方法采用变分模态分解自动识别流域水文系统特征时间尺度,通过滑动窗口传递熵量化气象因子对径流变化的信息传递强度,集成贝叶斯优化算法实现参数全自动确定,结合改进谱聚类算法精确识别突变时点。以钱塘江流域和长江流域为研究区,基于1961-2020年长序列水文气象数据进行双流域对比验证。结果表明:(1)AMSTE方法成功识别出两流域三次主要突变期(1978-1979年、1997-1998年、2003-2005年),识别置信度达0.85-0.96,与Mann-Kendall检验一致性达78%;(2)小流域以年内尺度为主导(贡献率65.3%),大流域年际尺度贡献显著提升(39.5%),体现明显的流域尺度效应;(3)钱塘江流域气候变化贡献65%,长江流域人类活动贡献55%,揭示不同规模流域驱动机制差异;(4)第三次突变后传递熵显著下降,钱塘江降幅27.6%,长江降幅13.9%,反映大流域具有更强韧性。参数敏感性分析表明方法具有良好稳定性,跨流域参数迁移保持率达77.2%。研究为复杂环境下径流变化分析提供了新的技术手段,对流域水资源管理和气候适应策略制定具有重要科学价值。

       

      Abstract: Under global climate change and intensifying human activities, runoff systems exhibit increasingly pronounced abrupt changes, making accurate mutation detection crucial for basin water resources management. Traditional statistical methods such as the Mann-Kendall test rely on univariate analysis and cannot capture nonlinear multi-factor interactions. We propose an intelligent runoff mutation detection method based on Adaptive Multi-Scale Transfer Entropy (AMSTE), which integrates Variational Mode Decomposition (VMD) with transfer entropy theory for the first time to establish a multi-scale causal analysis framework. VMD automatically identifies characteristic timescales of watershed hydrological systems; sliding-window transfer entropy quantifies information transfer intensity from meteorological factors to runoff; Bayesian optimization enables fully automated parameter determination; and an improved spectral clustering algorithm precisely detects mutation points. Using 1961-2020 hydro-meteorological data from the Qiantang River Basin and Yangtze River Basin, we conducted comparative validation across scales. Key findings include: (1) AMSTE successfully identified three major mutation periods (1978-1979, 1997-1998, 2003-2005) in both basins with confidence levels of 0.85-0.96, achieving 78% consistency with Mann-Kendall tests; (2) intra-annual scales dominate in small basins (65.3% contribution), while inter-annual scales increase significantly in large basins (39.5%), revealing clear scale effects; (3) climate change accounts for 65% of variability in the Qiantang River Basin versus 55% from human activities in the Yangtze River Basin, indicating scale-dependent driving mechanisms; (4) post-third-mutation transfer entropy declined by 27.6% (Qiantang) and 13.9% (Yangtze), demonstrating greater resilience in large basins. Sensitivity analysis confirms robust method stability with 77.2% cross-basin parameter transferability. This study provides a novel analytical tool for runoff change detection in complex environments, offering valuable insights for water resources management and climate adaptation strategies.

       

    /

    返回文章
    返回