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基于机器学习的广东海域模式风暴潮数据订正及评估OA

Machine learning-based correction and evaluation of storm surge simulation data for Guangdong coastal waters

中文摘要英文摘要

研究基于欧洲中期天气预报中心的ERA5再分析风场与海平面气压数据,驱动ADCIRC模式构建了广东省2024年两次风暴潮过程的逐小时风暴潮数据集.针对ADCIRC模式在广东沿岸模拟存在的系统误差,发展了一种基于随机森林回归的机器学习订正方法.通过构建包含模拟增水、潮位、风增水、风速等17项物理特征及其衍生交互项的特征体系,建立了具有明确物理意义的误差订正模型.训练结果表明:模型在1 377个样本上表现出良好的学习能力,训练集与测试集的R2分别为0.72和0.65,RMSE分别为16.69和21.24,相关系数分别达到0.86和0.81.实例测试显示:模型对2024年9月过程的高风速个例的改进率为11.65%,对2024年11月过程的低风速个例的改进率达48.08%,平均改进率为29.87%.该机器学习订正方法能有效降低ADCIRC模式的系统误差,在低风速条件下订正效果尤为显著.

This study utilized the ERA5 reanalysis wind fields and sea level pressure data from the European Centre for Medium-Range Weather Forecasts(ECMWF)to drive the ADCIRC model,constructing an hourly storm surge dataset for two storm surge processes in Guangdong coastal waters in 2024.To correct the systematic errors in the storm surge simulations,by constructing a feature system comprising 17 physical features including simulated surge,tidal level,wind-induced surge,wind speed,and their derived interaction terms,a machine learning error correction model based on Random Forest regression with clear physical significance was established.Training results demonstrated the model's strong learning capability on 1 377 samples,with an R2 of 0.71 and 0.65,an RMSE of 16.7 and 21.2,and correlation coefficients of 0.86 and 0.81 for the training and test sets,respectively.Case studies showed that the model achieved improvement rates of 11.65%for the high-wind-speed case in September 2024 and 48.08%for the low-wind-speed case in November 2024,with an average improvement rate of 29.87%.The research suggests that this machine learning correction method effectively reduces systematic errors in the ADCIRC model,particularly demonstrating stronger correction capability under low-wind-speed conditions.

俞重阳;张露

河海大学海洋学院,江苏 南京 210098国家海洋环境预报中心,北京 100081

海洋科学

广东海域风暴潮数值模拟机器学习

Guangdong coastal watersstorm surgenumerical simulationmachine learning

《海洋预报》 2026 (3)

31-41,11

国家自然科学基金项目(42425601).

10.11737/j.issn.1003-0239.2026.03.004

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