螺山站水位流量关系影响因子及水位预报模型研究

    Research on influencing factors of water level-discharge relationship and water level forecasting model at Luoshan Station

    • 摘要: 螺山水文站水位流量关系复杂,水位预报难度大,如何提高预报精度和有效预见期是亟待解决的问题。基于Spearman相关分析、支持向量回归、水量平衡分析方法,利用2010年至2024年8月螺山站实测水位流量数据及上下游控制节点数据,分析了螺山站水位流量关系和水位预报需考虑的关键影响因子,构建了水位预报模型。结果表明:螺山站水位流量关系关键影响因子为汉口站同时水位落差及陆水水库前1 d出库流量,水位预报影响因子还包括上游干支流来水及前1 d洞庭湖湖区降雨。预报模型在训练期和检验期预见期1~7 d内预报精度较高,R2均在0.97以上,表明模型可在螺山站实际预报中进行应用。研究成果可为城陵矶地区防洪调度提供有力技术支撑,也为复杂河网地区水文预报提供了一种研究思路。

       

      Abstract: The water level-discharge relationship at Luoshan Hydrological Station is complex, which poses challenges for accurate water level forecasting.Enhancing forecast accuracy and extending the effective forecast period are pressing issues that need to be addressed.Based on the measured water level and discharge data and the upstream and downstream control node data from 2010 to August 2024, Spearman correlation analysis, support vector regression and water balance analysis method were used to systematically analyze the key influencing factors for the water level-discharge relationship at Luoshan Station.Based on the analysis results, a water level forecasting model was constructed.Results indicate that the key influencing factors of the water level-discharge relationship at Luoshan Station include simultaneous water level changes between Hankou Station and Luoshan Station, and the discharge from Lushui Reservoir in the previous day.Additionally, factors affecting water level forecasts also involve inflows from upstream tributaries and rainfall in Dongting Lake area in the previous day.The forecasting model demonstrates high accuracy during both the training period and the test period in the 1 to 7-day forecast period, and the R-squared is all above 0.97, indicating that the model can be applied in the actual forecasting at Luoshan Station.The research outcomes provide robust technical support for flood control operations in the Chenglingji area, while also offering a methodological approach for hydrological forecasting in complex river network areas.

       

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