| 22 | 0 | 57 |
| 下载次数 | 被引频次 | 阅读次数 |
针对华北半干旱半湿润流域洪水预报中传统概念模型洪峰低估、数据驱动模型物理约束不足的问题,以海河流域大清河水系之阜平流域为研究对象,构建了新安江模型(XAJ)与双向长短期记忆网络(BiLSTM)耦合的洪水预报残差修正模型,并结合SHAP方法揭示模型补偿机理。以XAJ输出的预报流量、三层土壤含水量及径流分量等物理变量为输入,采用递进式特征组合构建BiLSTM残差修正模型,系统评估不同物理信息对预报效果的影响。结果表明:XAJ在阜平流域存在明显洪峰低估和时序偏差;将XAJ输出的基准预报流量作为先验特征输入BiLSTM后,混合模型整体拟合效果显著提升,且物理边界约束可有效抑制纯数据驱动模型在极端条件下的数值失真;进一步引入三层土壤含水量后,模型洪峰捕捉能力最优,平均洪峰相对误差控制在10%以内。SHAP归因分析表明,土壤水分状态变量是驱动残差正向补偿的关键因子,径流分量在本研究样本条件下未表现出稳定增益,其附加信息可能因误差传播和信息冗余削弱模型泛化能力。研究表明,基于关键物理状态约束的XAJ-BiLSTM混合框架能够有效提高北方复杂流域洪峰预报精度,并为物理-数据融合水文模型的可解释构建提供参考。
Abstract:To address the issues of flood forecasting for flood-peak underestimation in traditional conceptual models and insufficient physical constraints in data-driven models for semi-arid and semi-humid catchments in northern China, a residual correction model for flood forecasting was developed by coupling the Xin'anjiang model(XAJ) with a bidirectional long short-term memory network(BiLSTM) for the Fuping Catchment in the Daqing River subsystem of the Haihe River basin. The SHAP method was introduced to interpret the model's compensation mechanism. Physical variables derived from XAJ, including forecasted discharge, three-layer soil moisture, and runoff components, were used as inputs. A progressive feature combination approach was adopted to construct the BiLSTM residual correction model and to evaluate the effects of different physical information on forecasting performance. The results indicate that XAJ exhibits noticeable flood-peak underestimation and temporal deviation in the Fuping catchment. When the baseline forecasted discharge from XAJ is used as a prior input to BiLSTM, the hybrid model achieves significantly improved overall fitting performance, and the physically constrained framework effectively suppresses numerical distortions in purely data-driven models under extreme conditions. After further incorporating the three-layer soil moisture, the model captures flood peaks most accurately, with the mean relative error of flood peaks reduced to within 10%. SHAP attribution analysis reveals that soil moisture state variables are key drivers of positive residual compensation. Runoff component variables do not provide stable additional gains under the current sample conditions, and their inclusion may weaken the model's generalization ability due to error propagation and information redundancy. The research reveals that the proposed XAJ-BiLSTM hybrid framework, constrained by key physical state variables, effectively improves flood-peak forecasting accuracy in complex catchments in northern China and provides a reference for the interpretable construction of physics-data fusion hydrological models.
[1]丁一汇,任国玉,石广玉,等.气候变化国家评估报告(Ⅰ):中国气候变化的历史和未来趋势[J].气候变化研究进展,2006(1):3-8+50.
[2]马强,涂泽辉,李郑淼,等.雨带北移影响下大清河北支防洪情势[J].南水北调与水利科技(中英文),2025,23(5):1127-1133.
[3]ZHAO L,WANG J,XIAO Z,et al. Solar 11-year cycle-modulated north–south contrasting patterns of summer precipitation in China[J]. Journal of Climate,2025,38(14):3277-3294.
[4]刘志雨.雨水情监测预报“三道防线”耦合贯通建设应用与探讨[J].中国水利,2025(10):1-7.
[5]国家防灾减灾救灾委员会办公室.应急管理部发布2025年上半年全国自然灾害情况[J].安全与健康,2025(8):58-59.
[6]REN-JUN Z. The Xin’anjiang model applied in China[J]. Journal of Hydrology,1992,135(1):371-381.
[7]仲志余,张建云,王焰新,等.华北地区深层地下水回补修复试点研究与思考[J].中国水利,2025(15):1-5.
[8]姚成,李致家,张珂,等.基于栅格型新安江模型的中小河流精细化洪水预报[J].河海大学学报(自然科学版),2021,49(1):19-25.
[9]邵景力,白国营,刘翠珠,等.我国地下水管理面临的问题与对策——兼谈地下水“双控”管理[J].水文地质工程地质,2023,50(5):1-9.
[10]晋华.双超式产流模型的理论及应用研究[D].北京:中国地质大学(北京),2006.
[11]魏玉涛.基于新安江-海河模型的漳河流域洪水预报和调度研究[D].济南:济南大学,2022.
[12]钟栗,姚成,李致家,等.应用新安江-海河模型研究下垫面变化对设计洪水的影响[J].湖泊科学,2015,27(5):975-982.
[13]李致家,张心愿,白云鹏,等.海河“23·7”流域性特大洪水复盘模拟[J].河海大学学报(自然科学版),2024,52(5):13-19+92.
[14]李巧玲,李旻喆,李致家,等.新安江-海河模型参数物理意义分析及应用[J].河海大学学报(自然科学版),2025,53(1):1-9.
[15]CHEN X,ZHANG K,LUO Y,et al. A distributed hydrological model for semi-humid watersheds with a thick unsaturated zone under strong anthropogenic impacts:A case study in Haihe River Basin[J].Journal of Hydrology,2023,623:129765.
[16]KRATZERT F,KLOTZ D,BRENNER C,et al.Rainfall-runoff modelling using Long Short-Term Memory(LSTM)networks[J]. Hydrology and Earth System Sciences,2018,22(11):6005-6022.
[17]KRATZERT F,KLOTZ D,SHALEV G,et al.Towards learning universal,regional,and local hydrological behaviors via machine learning applied to large-sample datasets[J]. Hydrology and Earth System Sciences,2019,23:5089-5110.
[18]瞿思敏,余裕,方正,等.机器学习模型与物理机制模型在长诏水库流域实时洪水预报中的比较研究[J].水资源保护,2025,41(5):73-78+88.
[19]王俊,程海云,郭生练,等.智慧流域水文预报技术研究进展与开发前景[J].人民长江,2023,54(8):1-8+59.
[20]张建云,谢康,刘艳丽,等.融合物理机制的机器学习水文模型研究进展[J].人民长江,2025,56(10):37-46.
[21]LI W,LIU C,XU Y,et al. An interpretable hybrid deep learning model for flood forecasting based on Transformer and LSTM[J]. Journal of Hydrology:Regional Studies,2024,54:101873.
[22]CUI Z,ZHOU Y,GUO S,et al. A novel hybrid XAJ-LSTM model for multi-step-ahead flood forecasting[J]. Hydrology Research,2021,52(6):1436-1454.
[23]JIANG H,ZHANG C. A Hybrid XAJ-LSTM-TFM Model for improved runoff simulation in the Poyang Lake basin:integrating physical processes with temporal and lag feature learning[J]. Water,2025,17(14):2146.
[24]张珂,刘杰,王宇昊,等.结合注意力机制的ConvLSTM与新安江模型相融合的混合水文模型[J].水资源保护,2026,42(1):137-143+151.
[25]XIANG X,GUO S,LI C,et al. An explainable deep learning model based on hydrological principles for flood simulation and forecasting[J]. Hydrol. Earth Syst. Sci.,2025,29:7217-7239.
[26]陈暘,雷晓辉,蒋云钟,等.分布式水文模型EasyDHM在海河阜平流域的应用[J].南水北调与水利科技,2010,8(4):111-114+132.
[27]SCHUSTER M,PALIWAL K K. Bidirectional recurrent neural networks[J]. IEEE transactions on Signal Processing,1997,45(11):2673-2681.
[28]LUNDBERG S M,LEE S I. A unified approach to interpreting model predictions[C]//Proceedings of the 31st International Conference on Neural Information Processing Systems. Red Hook:Curran Associates Inc.,2017:4768-4777.
[29]XU Y,LIN K,HU C,et al. Uncovering the dynamic drivers of floods through interpretable deep learning[J]. Earth’s Future,2024,12(10):e2024EF004751.
基本信息:
中图分类号:P338
引用信息:
[1]沈欣怡,史韵琪,张轩,等.基于新安江模型-双向长短期记忆网络与SHAP归因的阜平流域洪水预报残差修正研究[J].中国水利().
基金信息:
国家重点研发计划(2023YFC3006501); 中央级公益性科研院所基本科研业务费专项资金重点基金项目(Y524008、Y525015)
2026-06-04
2026-06-04
2026-06-04