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降雨时间分布对中长期旬极端径流模拟的影响OA

Impact of Rainfall Temporal Distribution on the Simulation for Extreme Runoff in Ten-day Scale

中文摘要英文摘要

在径流中长期预报中,往往忽视预报时间步长内的信息,比如降雨的时间分配.为提高中长期旬尺度极端径流的模拟精度,采用改进的偏最小二乘回归模型 N-PLS和神经网络模型 LSTM 对乌东德水库和向三区间旬还原径流构建模型,并比较旬内降雨分布和温度输入特征及数据处理方式对模型整体、极端旱涝径流模拟性能的影响.结果表明:2 个模型的不同输入方案对乌东德水库旬还原入库径流的整体模型模拟精度R2 和NSE基本都在 0.95~0.98之间,高于向三区间;4 组特征输入方案对 LSTM 模型的影响明显弱于 N-PLS 模型,增加旬内降雨分布和气温特征会微弱提升模型的性能,一定程度上减小了乌东德水库重旱以上径流模拟汛期易偏大的偏差、向三区间重涝以上径流模拟易偏小的偏差;增加旬内降雨分布和气温特征对统计模型 N-PLS性能有明显提升,其中向三区间比乌东德水库表现更明显,显著减小了向三区间重旱以上径流模拟易偏大、重涝以上径流模拟易偏小的偏差;由于 LSTM 模型稳定性更强,因此模型整体精度高于 N-PLS模型,但对于乌东德水库枯期重旱以上极端径流和向三区间汛期重涝以上极端径流,考虑旬内降雨信息、气温特征且非归一化的 N-PLS模型表现更好.总的来说,考虑旬内降雨信息和温度等更多水文特性输入有助于提升旬极端径流的模拟精度.

In long-term runoff forecasting,information within the forecast time step is often overlooked,such as temporal distribution of rainfall.To improve the simulation accuracy of extreme runoff in ten-day scale,an improved partial least squares regression model N-PLS and a neural network model LSTM are used to construct models for Wudongde Reservoir and Xiangsan catchment area,comparing the effects of different input features and data on these two models.The results show that:(a)R2 and NSE of the two models with different input schemes for Wudongde Reservoir are generally between 0.95 and 0.98,which is higher than that of Xiangsan catchment area;(b)the impact of the four sets of feature input schemes on the LSTM model is significantly weaker than that of the N-PLS model,and increasing characteristics within ten-day will slightly improve the performance of the LSTM model,which to some extent reduces the bias of overestimation in severe drought runoff simulation during flood season for Wudongde Reservoir and reduces the bias of underestimation in severe flood runoff simulation for Xiangsan catchment area;(c)adding detailed features can significantly improve the performance of the statistical model N-PLS,with a more pronounced performance in Xiangsan catchment area compared to Wudongde Reservoir,and can significantly reduce the bias of overestimation in severe drought runoff simulation and underestimation in severe flood runoff simulation;and(d)due to the stronger stability of the LSTM model,the overall accuracy of the model is higher than that of the N-PLS model,however,for the severe drought runoff during the dry season of Wudongde Reservoir and severe flood runoff during the flood season of Xiangsan catchment area,the non normalized N-PLS model considering the rainfall information and temperature characteristics within ten-day performs better.Overall,considering more hydrological characteristic inputs such as rainfall information and temperature within the ten-day period can improve the simulation accuracy of extreme runoff during the ten-day period.

吴碧琼;张海荣;曹辉;任玉峰;马一鸣;李曲;张增信

智慧长江与水电科学湖北省重点实验室(中国长江电力股份有限公司),湖北 宜昌 443000智慧长江与水电科学湖北省重点实验室(中国长江电力股份有限公司),湖北 宜昌 443000智慧长江与水电科学湖北省重点实验室(中国长江电力股份有限公司),湖北 宜昌 443000智慧长江与水电科学湖北省重点实验室(中国长江电力股份有限公司),湖北 宜昌 443000智慧长江与水电科学湖北省重点实验室(中国长江电力股份有限公司),湖北 宜昌 443000智慧长江与水电科学湖北省重点实验室(中国长江电力股份有限公司),湖北 宜昌 443000河海大学水文水资源学院,江苏 南京 210024

建筑与水利

中长期径流模拟极端径流LSTM偏最小二乘回归模型降雨分布

medium and long-term runoff simulationextreme runoffLSTMpartial least squares regression modelrainfall distribution

《水力发电》 2026 (2)

13-21,61,10

国家自然科学基金委员会-中华人民共和国水利部-中国长江三峡集团有限公司长江水科学研究联合基金项目(U2240214)中国长江电力股份有限公司科研项目(Z242302054)

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