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基于DETR模型的欧亚大陆温带气旋冷暖锋自动识别研究

Automatic Identification of Cold and Warm Fronts in Extratropical Cyclones over the Eurasian Continent Based on the DETR Model

  • 摘要: 温带气旋是中纬度地区重要的天气系统,对全球天气及气候均具有深远影响。锋面系统是温带气旋的关键结构,其精准识别对于提高天气预报的准确性至关重要。近两年来,深度学习方法开始在锋面自动识别领域得到应用,然而针对欧亚大陆的锋面自动识别研究较少,并且多集中于单类锋面的检测,实现冷锋和暖锋的同步识别与分类仍然存在较大困难。因此本文提出了一种基于DETR(Detection Transformer)模型的冷暖锋同步识别方法DETR-FRO。该方法利用海平面气压、850 hPa的温度平流、温度及相对湿度等气象变量构建RGB特征图像,并结合人工冷暖锋标签集训练DETR模型,实现了冷暖锋自动同步识别与分类。DETR-FRO改进了原DETR模型的输送通道,引入多个气象变量构建RGB特征图像以提升锋面特征表达能力,使得冷暖锋均有较好的识别效果。多维度验证结果表明,该方法能够同步识别欧亚大陆温带气旋的冷暖锋,并且具有较高的准确性和稳定性。在典型暴雪个例的应用中,DETR-FRO模型能够准确还原冷锋、暖锋及其演变过程,且识别结果与动力、热力要素场有较好的匹配,进一步验证了该模型的泛化能力与气象可解释性。这一改进也为天气预报和温带气旋的研究提供了新的技术支持。

     

    Abstract: A temperate cyclone is an important weather system in the mid-latitude regions and has a profound impact on global weather and climate. The frontal system is a key structure of a temperate cyclone, and its accurate identification is crucial for improving weather forecast accuracy. In recent years, deep learning methods have been applied in the field of frontal automatic recognition, but research on frontal identification over the Eurasian continent has been limited, often focusing on detecting single-type fronts. Achieving simultaneous recognition and classification of cold and warm fronts still presents significant challenges. Therefore, this paper proposes a cold and warm front synchronous recognition method based on the DETR (Detection Transformer) model, called DETR-FRO. The method constructs RGB feature images using meteorological variables such as sea-level pressure, temperature advection at 850 hPa, temperature, and relative humidity, and trains the DETR model with an artificial cold and warm front label set to achieve automatic synchronous recognition and classification of cold and warm fronts. DETR-FRO improves the original DETR model’s transmission channel by incorporating multiple meteorological variables to construct RGB feature images, enhancing the ability to express frontal features, resulting in good recognition performance for both cold and warm fronts. Multi-dimensional validation results show that the method can simultaneously identify the cold and warm fronts of temperate cyclones over the Eurasian continent with high accuracy and stability. In the application to a typical snowstorm case, the DETR-FRO model accurately restores the cold front, warm front, and their evolution process, and the recognition results align well with dynamic and thermodynamic fields, further verifying the model"s generalization ability and meteorological interpretability. This improvement also provides new technical support for weather forecasting and the study of temperate cyclones.

     

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