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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(DETR-FRONT)。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。此外,基于DETR-FRO构建的1995~2024年长时间序列锋面数据集,从气候尺度揭示了欧亚大陆温带气旋冷暖锋频率的季节分布特征,有利于加深温带气旋冷暖锋气候特征研究的理解。

     

    Abstract: A extratropical cyclone is an important weather system in mid-latitude regions and has a profound impact on global weather and climate. The frontal system is a key component of the cyclone, and its accurate identification is crucial for improving the accuracy of weather forecasts. In recent years, deep learning methods have been applied to automatic frontal recognition, but research on frontal identification over the Eurasian continent has been limited, with a focus on detecting single-type fronts. Achieving simultaneous recognition and classification of cold and warm fronts remains a major challenge. Therefore, this paper proposes a method for the synchronous recognition of cold and warm fronts based on the Detection Transformer (DETR) model called DETR-FRONT (DETR-FRO). This method constructs RGB feature images using meteorological variables, such as sea level pressure, temperature advection, temperature, and relative humidity at 850 hPa. The DETR model is trained using an artificially created cold and warm front label set, enabling automatic synchronous recognition and classification of both types of fronts. DETR-FRO improves the original DETR model by enhancing its transmission channel and incorporating multiple meteorological variables to construct RGB feature images. This modification strengthens the ability of the model to capture and express frontal features, leading to improved recognition performance for cold and warm fronts. Multidimensional validation results show that DETR-FRO can simultaneously identify cold and warm fronts in extratropical cyclones over the Eurasian continent with high accuracy and stability. In a typical snowstorm case study, the DETR-FRO model accurately reconstructs the cold and warm fronts and their evolution processes. The recognition results are consistent with dynamic and thermodynamic fields, further confirming the model’s generalization ability and meteorological interpretability. This improvement provides new technical support for weather forecasting and the study of extratropical cyclones. In addition, the long-term frontal dataset created using DETR-FRO, covering the period from 1995 to 2024, reveals the seasonal distribution characteristics of cold and warm front frequencies in extratropical cyclones over the Eurasian continent at the climate scale. This information contributes to a deeper understanding of the climatic characteristics of cold and warm fronts in extratropical cyclones.

     

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