Journal of Computer Applications ›› 2026, Vol. 46 ›› Issue (3): 980-992.DOI: 10.11772/j.issn.1001-9081.2025020184
• Frontier and comprehensive applications • Previous Articles Next Articles
Min CHEN1,2,3, Xiaolin QIN1,2(
), Shaohan LI3, Hao YANG3, Taohong LI3
Received:2025-03-03
Revised:2025-04-18
Accepted:2025-04-28
Online:2026-03-16
Published:2026-03-10
Contact:
Xiaolin QIN
About author:CHEN Min, born in 1989, Ph. D. candidate. Her research interests include spatio-temporal prediction, data mining, smart meteorology.Supported by:
陈敏1,2,3, 秦小林1,2(
), 李绍涵3, 杨昊3, 李韬弘3
通讯作者:
秦小林
作者简介:陈敏(1989—),女,四川乐山人,博士研究生,主要研究方向:时空预测、数据挖掘、智慧气象基金资助:CLC Number:
Min CHEN, Xiaolin QIN, Shaohan LI, Hao YANG, Taohong LI. Review of deep learning applications in severe convective weather prediction[J]. Journal of Computer Applications, 2026, 46(3): 980-992.
陈敏, 秦小林, 李绍涵, 杨昊, 李韬弘. 深度学习应用于强对流天气预测的综述[J]. 《计算机应用》唯一官方网站, 2026, 46(3): 980-992.
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URL: https://www.joca.cn/EN/10.11772/j.issn.1001-9081.2025020184
| 类别 | 指标 |
|---|---|
| 全局精度 | MAE, MSE,RMSE, PCC |
| 二值精度 | CSI, Accuracy, FSS, F1-score, POD, Precision, HSS, Recall,FAR |
| 降尺度精度 | CSI-neighborhood, FSS, Pooled CRPS |
| 清晰度精度 | GDL, LPIPS, PSNR, SSIM |
Tab. 1 Commonly used evaluation metrics in weather prediction
| 类别 | 指标 |
|---|---|
| 全局精度 | MAE, MSE,RMSE, PCC |
| 二值精度 | CSI, Accuracy, FSS, F1-score, POD, Precision, HSS, Recall,FAR |
| 降尺度精度 | CSI-neighborhood, FSS, Pooled CRPS |
| 清晰度精度 | GDL, LPIPS, PSNR, SSIM |
| 方法类别 | 代表模型 | 优势 | 劣势 |
|---|---|---|---|
循环 方法 | ConvLSTM | 结合CNN和LSTM结构,捕捉空间和时间依赖关系,适用于短时天气预测。ConvLSTM在气象数据集(如 Radar Echo、ERA5、GFS、ClimateNet)上能有效捕捉降水、温度、风场等时空依赖关系,适用于短期天气预测 | 计算成本高,对长期趋势(如ERA5的长期气候模式)捕捉较弱,易受累积误差影响,在GFS这样的数值天气预报数据上可能不及传统物理模型精确 |
| MotionRNN | 采用时间-空间变换机制,提升对运动信息的建模能力,适用于复杂天气场景 | 计算复杂度较高,对长时间序列预测仍有误差累积问题 | |
| SwinLSTM | 结合Swin Transformer进行局部和全局信息交互,提高时序预测精度 | 结构复杂,对计算资源需求较高,训练难度比较大 | |
非循环 方法 | SimVP | 采用ETD架构,实现端到端多步预测,计算效率高 | 主要依赖CNN,难以捕捉长时间依赖关系 |
| MIMO-VP | 采用Transformer实现MIMO,提高长时序预测能力 | 计算量大,训练难度较大 | |
| TAU | 通过静态注意力和动态注意力优化特征提取,提升计算效率 | 对数据量依赖较高,对不同天气类型的适应性有待提升 | |
生成 模型 | MoCoGAN | 采用运动-内容解耦,增强降水等天气场景的时空一致性 | 生成结果受随机性影响,存在模式崩溃风险 |
| PreDiff | 结合扩散模型进行天气预测,生成效果稳定,适用于不确定性建模 | 计算量大,训练和推理开销较高 | |
| DiffCast | 结合全局UNet,增强降水预测的细节保留能力 | 对高分辨率天气场景的泛化能力有待提升 | |
| 大模型 | GraphCast | 采用GNN进行全球天气预测,具备良好的泛化能力 | 对超长时间尺度的预测仍存一定误差 |
| FourCastNet | 结合Transformer提高天气预测效率,计算速度快 | 需要高质量数据支持,缺乏物理约束 | |
| Pangu-Weather | 端到端建模全球天气,精度超过部分NWP方法 | 训练数据和计算资源需求极大 |
Tab. 2 Comparison of advantages and disadvantages of weather prediction models of various representative method
| 方法类别 | 代表模型 | 优势 | 劣势 |
|---|---|---|---|
循环 方法 | ConvLSTM | 结合CNN和LSTM结构,捕捉空间和时间依赖关系,适用于短时天气预测。ConvLSTM在气象数据集(如 Radar Echo、ERA5、GFS、ClimateNet)上能有效捕捉降水、温度、风场等时空依赖关系,适用于短期天气预测 | 计算成本高,对长期趋势(如ERA5的长期气候模式)捕捉较弱,易受累积误差影响,在GFS这样的数值天气预报数据上可能不及传统物理模型精确 |
| MotionRNN | 采用时间-空间变换机制,提升对运动信息的建模能力,适用于复杂天气场景 | 计算复杂度较高,对长时间序列预测仍有误差累积问题 | |
| SwinLSTM | 结合Swin Transformer进行局部和全局信息交互,提高时序预测精度 | 结构复杂,对计算资源需求较高,训练难度比较大 | |
非循环 方法 | SimVP | 采用ETD架构,实现端到端多步预测,计算效率高 | 主要依赖CNN,难以捕捉长时间依赖关系 |
| MIMO-VP | 采用Transformer实现MIMO,提高长时序预测能力 | 计算量大,训练难度较大 | |
| TAU | 通过静态注意力和动态注意力优化特征提取,提升计算效率 | 对数据量依赖较高,对不同天气类型的适应性有待提升 | |
生成 模型 | MoCoGAN | 采用运动-内容解耦,增强降水等天气场景的时空一致性 | 生成结果受随机性影响,存在模式崩溃风险 |
| PreDiff | 结合扩散模型进行天气预测,生成效果稳定,适用于不确定性建模 | 计算量大,训练和推理开销较高 | |
| DiffCast | 结合全局UNet,增强降水预测的细节保留能力 | 对高分辨率天气场景的泛化能力有待提升 | |
| 大模型 | GraphCast | 采用GNN进行全球天气预测,具备良好的泛化能力 | 对超长时间尺度的预测仍存一定误差 |
| FourCastNet | 结合Transformer提高天气预测效率,计算速度快 | 需要高质量数据支持,缺乏物理约束 | |
| Pangu-Weather | 端到端建模全球天气,精度超过部分NWP方法 | 训练数据和计算资源需求极大 |
| 模型 | MSE | MAE | RMSE |
|---|---|---|---|
| ConvLSTM | 1.521 4 | 0.794 9 | 1.233 5 |
| PredRNN | 1.331 1 | 0.724 6 | 1.153 7 |
| MAU | 1.251 4 | 0.703 6 | 1.118 7 |
| Swin Transformer | 1.142 9 | 0.673 5 | 1.069 1 |
| HorNet | 1.201 4 | 0.690 6 | 1.096 1 |
| TAU | 1.161 9 | 0.670 7 | 1.077 9 |
Tab. 3 Evaluation metrics of different models for 2-meter air temperature prediction (t2m) on WeatherBench dataset
| 模型 | MSE | MAE | RMSE |
|---|---|---|---|
| ConvLSTM | 1.521 4 | 0.794 9 | 1.233 5 |
| PredRNN | 1.331 1 | 0.724 6 | 1.153 7 |
| MAU | 1.251 4 | 0.703 6 | 1.118 7 |
| Swin Transformer | 1.142 9 | 0.673 5 | 1.069 1 |
| HorNet | 1.201 4 | 0.690 6 | 1.096 1 |
| TAU | 1.161 9 | 0.670 7 | 1.077 9 |
| 模型 | MSE | MAE | RMSE |
|---|---|---|---|
| ConvLSTM | 1.897 6 | 0.921 5 | 1.377 5 |
| PredRNN | 1.881 0 | 0.906 8 | 1.371 5 |
| MAU | 1.900 1 | 0.919 4 | 1.378 4 |
| Swin Transformer | 1.499 6 | 0.814 5 | 1.224 6 |
| HorNet | 1.553 9 | 0.825 4 | 1.246 6 |
| TAU | 1.592 5 | 0.842 6 | 1.261 9 |
Tab. 4 Evaluation metrics of different models for 10-meter wind components prediction (uv10) on WeatherBench dataset
| 模型 | MSE | MAE | RMSE |
|---|---|---|---|
| ConvLSTM | 1.897 6 | 0.921 5 | 1.377 5 |
| PredRNN | 1.881 0 | 0.906 8 | 1.371 5 |
| MAU | 1.900 1 | 0.919 4 | 1.378 4 |
| Swin Transformer | 1.499 6 | 0.814 5 | 1.224 6 |
| HorNet | 1.553 9 | 0.825 4 | 1.246 6 |
| TAU | 1.592 5 | 0.842 6 | 1.261 9 |
| 模型 | MSE | MAE | RMSE |
|---|---|---|---|
| ConvLSTM | 0.049 4 | 0.154 2 | 0.222 3 |
| PredRNN | 0.055 0 | 0.158 8 | 0.234 6 |
| MAU | 0.049 5 | 0.151 6 | 0.222 6 |
| Swin Transformer | 0.046 4 | 0.147 3 | 0.215 4 |
| HorNet | 0.046 9 | 0.147 5 | 0.216 6 |
| TAU | 0.047 2 | 0.146 0 | 0.217 3 |
Tab. 5 Evaluation metrics of different models for total cloud cover (tcc) prediction on WeatherBench dataset
| 模型 | MSE | MAE | RMSE |
|---|---|---|---|
| ConvLSTM | 0.049 4 | 0.154 2 | 0.222 3 |
| PredRNN | 0.055 0 | 0.158 8 | 0.234 6 |
| MAU | 0.049 5 | 0.151 6 | 0.222 6 |
| Swin Transformer | 0.046 4 | 0.147 3 | 0.215 4 |
| HorNet | 0.046 9 | 0.147 5 | 0.216 6 |
| TAU | 0.047 2 | 0.146 0 | 0.217 3 |
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