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      基于ARDL模型的河流径流预测

      River runoff prediction based on ARDL model

      • 摘要: 长江中游复杂的水文过程和频发极端气候事件对径流量预测构成挑战,解析关键水文断面间的流量动态耦合关系并构建径流预测模型,对揭示流域水文响应机制和优化水资源配置具有重要意义。基于长江中游5个关键水文断面(宜昌、沙市、监利、螺山、汉口) 日尺度水文气象数据,通过整合上游来水量、区域降水、气温及断面历史流量数据,构建自回归分布滞后(Autoregressive Distributed Lag,ARDL) 模型,定量解析断面间水流时滞响应特征,对径流进行预测。结果表明:上游来水流量、区域降雨和气温对下游断面日流量的影响存在1~5 d不等的滞后,且不同断面的主导滞后因子各异。在训练期,ARDL模型在5个断面的径流预测中均表现较好,确定系数R2均超过99%,验证期的R2均高于0.93,均方百分比误差均低于5%。该ARDL模型可为长江中游径流预测提供参考。

         

        Abstract: The middle reaches of Changjiang River face challenges in basin flow regulation due to its complex hydrological processes and frequent extreme climate events.Therefore, analyzing the dynamic flow coupling relationships among key hydrological sections and constructing runoff prediction models were crucial for revealing the basin′s hydrological response mechanisms and optimizing water resource allocation.This study utilizes daily-scale hydrometeorological data from five key hydrological cross-sections in the middle reaches of Changjiang River (Yichang, Shashi, Jianli, Luoshan, and Hankou).By integrating upstream inflow, regional precipitation, temperature, and historical flow records at these sections, an Autoregressive Distributed Lag (ARDL) model was constructed to quantitatively analyze inter-section flow lag response characteristics and predict runoff.Results indicated that upstream inflow, regional precipitation, and temperature exhibit lag periods ranging from 1 to 5 days in influencing daily discharge at downstream cross-sections, with lag factors varying across different sections.The ARDL model performed well in predicting the flow volume of all five sections.During the validation period, its coefficient of determination R2 exceeded 99%, and the mean square percentage error (MSPE) was below 5%.The ARDL model can provide a reference for runoff forecasting in the middle reaches of Changjiang River.

         

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