Hu Yingying, Pang Lin, Wang Qiguang. Application of deep learning bias correction method to temperature grid forecast of 7-15 days. J Appl Meteor Sci, 2023, 34(4): 426-437. DOI:  10.11898/1001-7313.20230404.
Citation: Hu Yingying, Pang Lin, Wang Qiguang. Application of deep learning bias correction method to temperature grid forecast of 7-15 days. J Appl Meteor Sci, 2023, 34(4): 426-437. DOI:  10.11898/1001-7313.20230404.

Application of Deep Learning Bias Correction Method to Temperature Grid Forecast of 7-15 Days

DOI: 10.11898/1001-7313.20230404
  • Received Date: 2023-03-10
  • Rev Recd Date: 2023-06-06
  • Publish Date: 2023-07-31
  • The forecast error of numerical weather forecasting is inevitable, and there are still difficulties in temperature forecast of 7-15 days. To improve forecast accuracy and timeliness, the deviation correction technique is often used in operation. In recent years, deep learning methods have shown great potential in statistical post-processing of model forecasts. To improve the accuracy of Global Ensemble Prediction System of China Meteorological Administration (CMA-GEPS) for 7-15 days, error characteristics of 2 m temperature and 10 m wind products of CMA-GEPS control forecast provided by TIGGE data center from 25 December 2018 to 5 July 2022, and ERA5 data provided by ECMWF are analyzed. The U-Net model and residual connection model is used to conduct 2 m temperature lattice forecast error revision experiment for the lead time of 168-360 h in the region 15.75°-55.25°N, 73°-136.5°E. The experiments are designed with various data features to explore differences of the deep learning methods for longer lead time with different sample characteristics and model parameters, and performances of models are examined by comparing the bias, mean absolute bias and root mean square error. The results show that 2 m temperature forecast errors of 7-15 days become larger as the lead time increases. The model forecast skill gradually decreases, and in the target area, performance in eastern and southern marine and offshore areas is better than in western and northern the plateaus and mountains. The differences in the spatial distribution of errors are more prominent. Among the revised models, the effect of the U-Net model is better than that of the U-Net residual connection model, and adding the initial 2 m temperature data of ERA5 can greatly improves the performance, but the effect of adding CMA-GEPS control forecast 10 m wind product of CMA-GEPS control forecast is not apparent. For 9 lead times, the revised root mean square errors are reduced by 10%-25%, and the model can effectively reduce the large forecast errors for the northern Mongolian Plateau and the western Tibetan Plateau, and some mountainous areas in the target area.
  • Fig. 1  Root mean square error of CMA-GEPS model control forecast for 2 m temperature with different lead times from 8 Apr to 5 Jul in 2022

    Fig. 2  Root mean square error of different lead times for 2 m temperature in the target area from 8 Apr to 5 Jul in 2022

    Fig. 3  Average absolute errors of 2 m temperature for CMA-GEPS model control forecast and U-Net model correction

    the line denotes average absolute error reduction rate of U-Net model correction based on dataset Ⅱ relative to CMA-GEPS control forecast

    Fig. 4  The same as in Fig. 3, but for root mean square error

    the line denotes root mean square error reduction rate of U-Net model correction based on dataset Ⅱ relative to CMA-GEPS control forecast

    Fig. 5  Daily root mean square error of 2 m temperature for 168 h lead time from 8 Apr to 5 Jul in 2022 by CMA-GEPS control forecast and U-Net model correction

    Fig. 6  The same as in Fig. 5, but for 360 h lead time

    Fig. 7  Root mean square error of 2 m temperature in the target area for 360 h lead time by CMA-GEPS control forecast and U-Net model correction

    Table  1  Evaluation indicaters of CMA-GEPS model control forecast of 2 m temperature for 240 h lead time and deep learning model correction based on dataset Ⅰ (unit:℃)

    预报与订正结果 评价指标
    偏差 平均绝对偏差 均方根误差
    CMA-GEPS控制预报产品 0.41 2.57 3.56
    U-Net模型订正 0.51 2.40 3.16
    U-Net残差连接模型订正 0.10 2.73 3.68
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    Table  2  The same as in Table 1, but based on dataset Ⅱ (unit:℃)

    预报与订正结果 评价指标
    偏差 平均绝对偏差 均方根误差
    CMA-GEPS控制预报产品 0.41 2.57 3.56
    U-Net模型订正 -0.21 1.67 2.29
    U-Net残差连接模型订正 -0.03 1.77 2.44
    DownLoad: Download CSV
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    • Received : 2023-03-10
    • Accepted : 2023-06-06
    • Published : 2023-07-31

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