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基于BO-LSTM神经网络模型的台风浪波高预报方法研究

秦知朋 陈永平 潘毅 徐晓武

秦知朋,陈永平,潘毅,等. 基于BO-LSTM神经网络模型的台风浪波高预报方法研究[J]. 海洋学报,2024,46(10):98–107 doi: 10.12284/hyxb2024089
引用本文: 秦知朋,陈永平,潘毅,等. 基于BO-LSTM神经网络模型的台风浪波高预报方法研究[J]. 海洋学报,2024,46(10):98–107 doi: 10.12284/hyxb2024089
Qin Zhipeng,Chen Yongping,Pan Yi, et al. Research on typhoon wave height prediction method based on BO-LSTM neural network model[J]. Haiyang Xuebao,2024, 46(10):98–107 doi: 10.12284/hyxb2024089
Citation: Qin Zhipeng,Chen Yongping,Pan Yi, et al. Research on typhoon wave height prediction method based on BO-LSTM neural network model[J]. Haiyang Xuebao,2024, 46(10):98–107 doi: 10.12284/hyxb2024089

基于BO-LSTM神经网络模型的台风浪波高预报方法研究

doi: 10.12284/hyxb2024089
基金项目: 国家重点研发计划项目(2023YFC3008100)。
详细信息
    作者简介:

    秦知朋(2000—),男,安徽省舒城县人,主要从事海岸灾害及防灾减灾方面研究。E-mail:2806641744@qq.com

    通讯作者:

    陈永平(1976—),男,江西省万载县人,教授,主要从事海岸灾害与防灾减灾研究。E-mail:ypchen@hhu.edu.cn

Research on typhoon wave height prediction method based on BO-LSTM neural network model

  • 摘要: 随着海平面上升和风暴增强等气候变化的影响,快速准确地预报台风浪波高对于海岸保护和海洋灾害预防显得格外重要。本文首先基于TCWiSE模型生成大量的虚拟台风,利用SWAN数值模式计算台风期间测站处的有效波高,并构建台风浪样本数据库;然后对BO-LSTM神经网络模型的输入因素和超参数进行评估和选取,结合样本数据库对其进行训练和测试。结果表明:所构建的虚拟台风与历史台风具有很好的相似性,可以为台风浪波高智能预报模型的搭建提供充足的数据基础;所搭建的BO-LSTM模型可以快速实现单一站点处的台风浪波高智能预报,并具有媲美SWAN的预报精度,其在长时间预报场景中的预报精度显著优于RF模型和BPNN模型;将预报的未来台风数据添加到BO-LSTM模型的输入中,进一步提高了模型的预报精度和预报未来时长,其预报未来24 h的Bias、RMSE和R2分别为−0.102 m、0.494 m和0.855。研究成果为极端天气下台风浪的智能预报提供一种可行的实现途径。
  • 图  1  1979–2022年西北太平洋地区历史台风路径图

    Fig.  1  Map of historical typhoon tracks in the Northwest Pacific region from 1979 to 2022

    图  2  波浪测站位置、网格范围及水深示意图

    Fig.  2  Schematic diagram of wave measurement station location, grid range, and water depth

    图  3  LSTM单元结构图

    Fig.  3  LSTM unit structure diagram

    图  4  台风浪波高智能预报模型的构建流程图

    虚线框内为贝叶斯优化过程

    Fig.  4  The construction process diagram of an intelligent typhoon wave height prediction model

    图  5  历史台风与随机抽取1128场虚拟台风的起点对比图(a)与终点对比图(b)

    Fig.  5  Comparison diagram of starting point (a) and ending point (b) of historical typhoons and randomly selected 1128 virtual typhoons

    图  6  验证站点位置示意图(a)和影响各站点的历史台风与虚拟台风的参数对比图(b、c)

    Fig.  6  Verification site location diagram (a) and parameter comparison diagram of historical and virtual typhoons affecting each site (b, c)

    图  7  3场典型历史台风期间不同测站处的有效波高验证对比图

    Fig.  7  Comparison chart of significant wave height verification at different stations during three typical historical typhoons

    图  8  输入因素不同前时序条件下各组次的均方根误差

    Fig.  8  Root mean square error of each group under different pre time series conditions of input factors

    图  9  3场典型台风期间不同机器学习模型对舟山站有效波高的预报结果与SWAN模拟结果的对比

    Fig.  9  Comparison between the prediction results of significant wave height at Zhoushan Station using different machine learning models and SWAN simulation results during three typical typhoons

    图  10  BO-LSTM预报有效波高与SWAN模拟有效波高之间的散点密度图

    Fig.  10  Scatter density plot between BO-LSTM predicted significant wave height and SWAN simulated significant wave height

    表  1  输入因素不同种类条件下各组次的均方根误差

    Tab.  1  Root mean square errors of each group under different types of input factors

    输入因素种类验证集RMSE/m
    台风因素0.878
    测站气象因素0.744
    前时序波高0.078
    台风因素+测站气象因素0.687
    台风因素+前时序波高0.066
    测站气象因素+前时序波高0.036
    所有因素0.025
    下载: 导出CSV

    表  2  不同预报时长条件下LSTM最优超参数的选取方案

    Tab.  2  Selection schemes for optimal hyperparameters of LSTM under different forecast duration conditions

    超参数名称 寻优范围 选取方案
    1 h 3 h 6 h 12 h
    神经元个数 (2,512) 214 174 196 272
    丢弃率 (0.01,0.2) 0.05 0.03 0.11 0.08
    批尺寸 (8,32) 12 15 16 8
    迭代次数 (10,100) 34 68 52 76
    下载: 导出CSV

    表  3  不同预报方案条件下BO-LSTM模型在测试集上的Bias、RMSE和R2

    Tab.  3  Bias, RMSE, and R2 of the BO-LSTM model on the test set under different forecasting schemes

    预见期 不添加预报风场 添加预报风场
    Bias/m RMSE/m R2 Bias/m RMSE/m R2
    1 h 0.001 0.017 0.999 0.001 0.012 0.999
    3 h −0.013 0.092 0.997 0.009 0.064 0.998
    6 h 0.018 0.194 0.978 0.014 0.122 0.986
    12 h −0.088 0.425 0.892 −0.063 0.316 0.931
    24 h / / / −0.102 0.494 0.855
    下载: 导出CSV
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出版历程
  • 收稿日期:  2024-01-03
  • 修回日期:  2024-07-15
  • 网络出版日期:  2024-10-18
  • 刊出日期:  2024-10-30

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