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一种针对模式预报场的精细化插值新方法

A New Fast Refinement Interpolation Method for Model Forecasting

  • 摘要: 随着智能网格预报业务的深入发展,为了不断提高网格预报产品的时空精度和准度,同时让网格和站点预报产品保持一致性,通过研究提出一种既考虑了静态真实地形又考虑了大气动态垂直变率的快速插值方法(Fast Refinement Interpolation, 简称FRI),并选择2022年1月1日到2022年3月31日的ECMWF和CMA-GFS、CMA-MESO三个模式的3~36 h预报产品作为试验数据,开展了个例天气过程试验、FRI参数选取试验和长期插值检验对比。从长期插值检验和个例试验来看,FRI方法相对双线性插值方法具有明显优势,空间上,FRI方法能提高近地面2 m气温的空间插值精度,插值结果更加符合地形变化情况,时间上,FRI方法较双线性插值方法的2 m气温插值结果准确率明显提高,特别是在具有复杂下垫面的中西部地区。方法中的修正参数还能被作为检验模式三维预报场垂直变率的一种指标。FRI方法插值快速高效,具有明确的物理解释意义,它的提出为更精准的预报近地面气象要素提供了重要理论支撑。

     

    Abstract: With the continuous development of grid forecasting operations with higher resolution and more accuracy, the spatial and temporal accuracies and precision of grid forecast products need to be continuously improved. To maintain compatibility between the grid and site forecasts, FRI (fast refinement interpolation) method was explored, which considers the static real-terrain and dynamic atmospheric vertical variation process. In this study, 3–36-h forecast products for three models (ECMWF, CMA-GFS, and CMA-MESO) from 1 January 2022 to 31 March 2022, were selected as the experimental data. Further, the results of individual weather process tests, FRI parameter selection tests, and long-term interpolation tests were compared. The results of long-term interpolation tests and individual case trials showed that the FRI method has a clear advantage over the bilinear interpolation method. From a spatial perspective, the FRI method can improve the spatial interpolation accuracy of 2-m temperature near the ground, and the results are more consistent with topographic variations. From a temporal perspective, the FRI method significantly improves the accuracy of the 2-m temperature interpolation results compared with the bilinear interpolation method, especially in the western region with complex subsurface. Additionally, the loss parameter in the proposed method can be used as an indicator to check the three-dimensional atmospheric vertical variability of the model product. The FRI method is fast and efficient and offers a clear physical meaning, which provides important theoretical support for the more accurate reflection of near-surface meteorological forecast information.

     

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