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基于观测和再分析数据的LSTM深度神经网络沿海风速预报应用研究

王国松 王喜冬 侯敏 齐义泉 宋军 刘克修 吴新荣 白志鹏

王国松,王喜冬,侯敏,等. 基于观测和再分析数据的LSTM深度神经网络沿海风速预报应用研究[J]. 海洋学报,2020,42(1):67–77,doi:10.3969/j.issn.0253−4193.2020.01.008
引用本文: 王国松,王喜冬,侯敏,等. 基于观测和再分析数据的LSTM深度神经网络沿海风速预报应用研究[J]. 海洋学报,2020,42(1):67–77,doi:10.3969/ j.issn.0253−4193.2020.01.008
Wang Guosong,Wang Xidong,Hou Min, et al. Research on application of LSTM deep neural network on historical observation data and reanalysis data for sea surface wind speed forecasting[J]. Haiyang Xuebao,2020, 42(1):67–77,doi:10.3969/j.issn.0253−4193.2020.01.008
Citation: Wang Guosong,Wang Xidong,Hou Min, et al. Research on application of LSTM deep neural network on historical observation data and reanalysis data for sea surface wind speed forecasting[J]. Haiyang Xuebao,2020, 42(1):67–77,doi:10.3969/j.issn.0253−4193.2020.01.008

基于观测和再分析数据的LSTM深度神经网络沿海风速预报应用研究

doi: 10.3969/j.issn.0253-4193.2020.01.008
基金项目: 国家重点研发计划(2016YFC1401903);国家自然科学基金(41776004);河海大学中央高校基本科研业务费(2016B12514)。
详细信息
    作者简介:

    王国松(1987—),男,天津市人,助研,主要从事数值模拟与资料处理研究。E-mail:xifengbishu2110@163.com

    通讯作者:

    侯敏,工程师,主要从事海洋气象预报业务。E-mail:ande0604@163.com

  • 中图分类号: P732.4

Research on application of LSTM deep neural network on historical observation data and reanalysis data for sea surface wind speed forecasting

  • 摘要: 基于海洋气象历史观测资料和再分析数据等,利用LSTM深度神经网络方法,开展在有监督学习情况下的海面风场短时预报应用研究。以中国近海5个代表站为研究区域,通过气象台站观测数据和ERA-Interim 6 h再分析数据构建数据集。选取21个变量作为预报因子,分别构建两个LSTM深度神经网络框架(OBS_LSTM和ALL_LSTM)。经与2017年WRF模式6 h预报结果对比分析,得出如下结论:构建的两个LSTM风速预报模型可以大幅降低风速预报误差,RMSE分别降低了41.3%和38.8%,MAE平均降低了43.0%和40.0%;风速误差统计和极端大风分析发现,LSTM模型能够抓住地形、短时大风和台风等敏感信息,对于大风过程预报结果明显优于WRF模式;两种LSTM模型对比发现,ALL_LSTM模型风速预报误差最小,具有很好的稳定性和鲁棒性,OBS_LSTM模型应用范围更广泛。
  • 图  1  气象观测台站分布(蓝点)与WRF模式嵌套区域

    黑红点线为2017年影响汕头和西沙两站的台风最佳路径

    Fig.  1  Locations of meteorological observation stations (blue points) and nested domain of WRF model

    Black dot line is the best track of typhoon affecting Shantou and Xisha stations in 2017

    图  2  预处理后测试集主要变量序列分布

    Fig.  2  Time series of main variable of the test set after preprocessing

    图  3  西沙站与观测风速相关性最高的9个变量热力图

    Fig.  3  The heat map of highest correlation between 9 variables and observed wind speed at Xisha Station

    图  4  ALL_LSTM预报模型结构图

    Fig.  4  ALL_LSTM prediction model structure diagram

    图  5  ALL_LSTM,OBS_LSTM和WRF模式日平均风速预报结果与台站观测资料对比

    Fig.  5  Comparison of daily mean wind speed forecast results of ALL_LSTM, OBS_LSTM and WRF models with observational data

    表  1  中国近海5个气象台站基本信息

    Tab.  1  Basic information of the five meteorological stations in China offshore

    站号站名缩写站类纬度经度观测场海拔高度/m
    54662大连DL基准站38°54'N121°38'E91.5
    54857青岛QD基本站36°04'N120°20'E76.0
    58265吕泗LS基准站32°04'N121°36'E 5.5
    59316汕头ST基准站23°24'N116°41'E 2.9
    59981西沙XS基准站16°50'N112°20'E 4.7
    下载: 导出CSV

    表  2  WRF模式设置

    Tab.  2  Specification of the WRF model

    区域与选项具体设置
    区域与分辨率三重嵌套,Lambert conformal投影,中心点(42°N,115°E)
    D01:水平分辨率
    30 km
    D02:水平分辨率
    10 km
    D03:水平分辨率
    3.3 km
    D04:水平分辨率
    3.3 km
    D05:水平分辨率
    3.3 km
    垂直分辨率44η层
    输出时间间隔6 h
    边界层方案Lin et al. scheme方案
    积云方案Kain-Fritsch方案
    微物理方案WSM 5-class 方案
    辐射方案长短波辐射方案:RRTMG方案
    陆面过程Noah陆面模式
    背景误差CV5
    热启动
    下载: 导出CSV

    表  3  验证集风速误差统计

    Tab.  3  Compare the performance of 6 h wind speed on validation sets

    站位误差统计ALL_LSTM
    模型
    OBS_LSTM
    模型
    WRF
    模型
    大连均方根误差/m·s−11.441.511.87
    绝对误差/m·s−11.091.171.43
    相关系数0.550.480.70
    青岛均方根误差/m·s−11.471.533.00
    绝对误差/m·s−11.101.152.33
    相关系数0.600.530.11
    吕泗均方根误差/m·s−11.151.211.17
    绝对误差/m·s−10.900.940.93
    相关系数0.640.580.73
    汕头均方根误差/m·s−10.740.771.13
    绝对误差/m·s−10.580.610.85
    相关系数0.550.500.51
    西沙均方根误差/m·s−11.161.202.99
    绝对误差/m·s−10.880.922.44
    相关系数0.730.710.70
    各地平均均方根误差/m·s−11.191.242.03
    绝对误差/m·s−10.910.961.60
    相关系数0.610.560.55
      注:最小均方根误差、最小绝对误差和最大相关系数分别用粗体表示。
    下载: 导出CSV
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  • 收稿日期:  2019-01-15
  • 修回日期:  2019-06-22
  • 网络出版日期:  2021-04-21
  • 刊出日期:  2020-01-25

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