用分层噪声注入让天气模型低成本生成可调控的概率预测
Controllable Probabilistic Forecasting with Stochastic Decomposition Layers
- 通过三层解码器级联注入可学习噪声,实现多尺度不确定性建模
- 仅需基线2%计算量,5MB隐空间编码即可复现并调节预测不确定度
- 适合需要可解释性与可控性的气象预报及气候分析场景
基于潜在噪声注入并以连续排名概率评分(CRPS)优化的AI天气集合预测,在计算成本远低于扩散模型的前提下,实现了高精度与良好校准。然而现有CRPS集合方法在训练策略和噪声注入机制上差异显著,多数采用条件归一化全局注入噪声,增加训练开销并降低随机扰动的物理可解释性。本文提出随机分解层(SDL),将确定性机器学习天气模型转化为概率集合系统。受StyleGAN层级噪声注入启发,SDL通过潜变量调制、逐像素噪声和通道缩放,在三个解码器尺度上施加学习到的扰动。应用于WXFormer时,只需基线模型2%的计算成本。每个集合成员由紧凑的隐向量(5 MB)生成,支持完美复现及推理后通过隐空间重缩放调节预测范围。在2022年ERA5再分析数据上的评估显示,集合的展布-技能比接近1,排序直方图随中期预报逐步趋于均匀,校准性能媲美业务运行的IFS-ENS。多尺度实验揭示层次化不确定性:粗粒度层调控大尺度环流,细粒度层控制中尺度变化。显式的潜在参数化为业务预报与气候应用提供了可解释的不确定性量化。
原文摘要 · Abstract (English)
AI weather prediction ensembles with latent noise injection and optimized with the continuous ranked probability score (CRPS) have produced both accurate and well-calibrated predictions with far less computational cost compared with diffusion-based methods. However, current CRPS ensemble approaches vary in their training strategies and noise injection mechanisms, with most injecting noise globally throughout the network via conditional normalization. This structure increases training expense and limits the physical interpretability of the stochastic perturbations. We introduce Stochastic Decomposition Layers (SDL) for converting deterministic machine learning weather models into probabilistic ensemble systems. Adapted from StyleGAN's hierarchical noise injection, SDL applies learned perturbations at three decoder scales through latent-driven modulation, per-pixel noise, and channel scaling. When applied to WXFormer via transfer learning, SDL requires less than 2\% of the computational cost needed to train the baseline model. Each ensemble member is generated from a compact latent tensor (5 MB), enabling perfect reproducibility and post-inference spread adjustment through latent rescaling. Evaluation on 2022 ERA5 reanalysis shows ensembles with spread-skill ratios approaching unity and rank histograms that progressively flatten toward uniformity through medium-range forecasts, achieving calibration competitive with operational IFS-ENS. Multi-scale experiments reveal hierarchical uncertainty: coarse layers modulate synoptic patterns while fine layers control mesoscale variability. The explicit latent parameterization provides interpretable uncertainty quantification for operational forecasting and climate applications.
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