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基于卫星资料的西太平洋台风强度监测机器学习方法对比研究

邓子怡 李煜斌 王泓 贾未雨 高志球

邓子怡, 李煜斌, 王泓, 贾未雨, 高志球. 基于卫星资料的西太平洋台风强度监测机器学习方法对比研究[J]. 热带气象学报, 2026, 42(1): 105-121. doi: 10.16032/j.issn.1004-4965.2026.009
引用本文: 邓子怡, 李煜斌, 王泓, 贾未雨, 高志球. 基于卫星资料的西太平洋台风强度监测机器学习方法对比研究[J]. 热带气象学报, 2026, 42(1): 105-121. doi: 10.16032/j.issn.1004-4965.2026.009
DENG Ziyi, LI Yubin, WANG Hong, JIA Weiyu, GAO Zhiqiu. Comparative Study of Machine Learning Methods for Typhoon Intensity Monitoring in the Western Pacific Based on Satellite Data[J]. Journal of Tropical Meteorology, 2026, 42(1): 105-121. doi: 10.16032/j.issn.1004-4965.2026.009
Citation: DENG Ziyi, LI Yubin, WANG Hong, JIA Weiyu, GAO Zhiqiu. Comparative Study of Machine Learning Methods for Typhoon Intensity Monitoring in the Western Pacific Based on Satellite Data[J]. Journal of Tropical Meteorology, 2026, 42(1): 105-121. doi: 10.16032/j.issn.1004-4965.2026.009

基于卫星资料的西太平洋台风强度监测机器学习方法对比研究

doi: 10.16032/j.issn.1004-4965.2026.009
基金项目: 

国家自然科学基金面上项目 42075072

详细信息
    作者简介:

    李煜斌,男,江西省人,教授,主要从事大气边界层和热带气旋动力学研究。E-mail: liyubin@nuist.edu.cn

  • 中图分类号: P444

Comparative Study of Machine Learning Methods for Typhoon Intensity Monitoring in the Western Pacific Based on Satellite Data

  • 摘要: 台风是严重影响沿海地区的自然灾害,准确监测其强度对于防灾减灾具有重要意义。基于卫星观测结合深度学习技术已成为台风强度监测的新一代方法,然而不同深度学习方法的准确度并不明确。因此,本文评估了六种基于深度学习的卷积神经网络模型在西太平洋台风强度监测中的表现。本研究利用2015—2024年Himawari-8/9卫星云产品数据和中国气象局台风最佳路径数据,对比分析了LeNet-5、AlexNet、DenseNet-121、VGG-16、ResNet-50以及GoogleNet-InceptionV3等模型的计算效果。本文不仅探讨了这些模型在不同强度台风场景下的适用性和性能表现,还对模型的特征提取步骤进行可视化,旨在更清晰地说明模型之间的差异以及模型工作原理。结果表明,LeNet-5与AlexNet在极弱(TD)和极强(SuperTY)级别下偏差最大;DenseNet-121在各强度下Bias分布较为平均;ResNet-50、VGG-16和GoogleNet-InceptionV3则在中等强度范围(TS、STS、TY、STY)内表现较为稳定。总体来看,GoogleNet-InceptionV3模型估计准确度最高(R2=0.89),但ResNet-50运行速度更快(R2=0.87)。

     

  • 图  1  六个模型在测试集上的估计结果

    灰色虚线表示1:1线,黑色实线为真实值与模型估计结果拟合线,色标表示预测值与观测值在二维空间中的样本密度,采用对数尺度(log10),颜色越暖表示该区间内样本数量越多。

    图  2  六个模型在测试集下强度估计偏差(Bias)的频率分布图

    图  3  六个模型的均方误差空间分布

    所有模型采用统一色标范围。当RMSE大于10 m·s-1时,统一归并至最高色阶(>10)。

    图  4  六个模型下的测试集估计结果的Bias与强度变化关系

    图  5  六个模型估计结果中台风快速增强时刻(RI)、快速减弱时刻(RW)、非快速增强减弱时刻(NRIRW)的(a)Bias、(b)MAE、(c)RMSE对比

    图  6  RI和RW阶段样本对应的原始云产品

    上排为RI阶段样本,下排为RW阶段样本;从左至右各列依次为云顶亮温(CLTT)、云光学厚度(CLOT)、云顶高度(CLTH)和云有效半径(CLER)。同一变量在RI与RW阶段采用统一色标范围,不同变量之间色标独立设置。

    图  7  早期层(上)与后期层(下)中提取的RI与RW特征图

    颜色表示特征响应强度,色标为对应特征图的归一化激活值。

    表  1  六个模型架构

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出版历程
  • 收稿日期:  2024-08-22
  • 修回日期:  2025-08-25
  • 网络出版日期:  2026-03-14
  • 刊出日期:  2026-02-20

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