arXiv:2605.16163physics.ao-phcs.LG2026-05

针对全球气象模型降水预报的时效依赖偏差,提出新方法实现瑞士千米级精准降尺度。

SwAIther-Precip: Lead-Time-Aware Bias Correction Enables Kilometer-Scale Downscaling of Global AI Precipitation Forecasts over Switzerland

论文配图:SwAIther-Precip: Lead-Time-Aware Bias Correction Enables Kilometer-Scale Downscaling of Global AI Precipitation Forecasts over Switzerland
图 1 · 摘自论文原文
  • 用时序条件调制的U-Net先修正预报偏差,再用扩散模型生成精细空间细节。
  • 相比原始AI模型,预报误差降低48%,小尺度空间结构匹配度达0.88。
  • 适合需要高精度短临降水预报的气象灾害预警与基础设施规划者使用。

在复杂地形区域,实现千米级中程降水预报仍具挑战性,因降水涉及多尺度非线性过程,全球模式难以以合理成本显式解析。尽管全球人工智能天气模型可生成有效中程预报,但其0.25度分辨率限制了本地灾害应用。统计降尺度虽可弥补差距,但现有方法常受状态依赖及尤其时效依赖偏差影响。本文提出SwAIther-Precip框架,将粗分辨率AIFS预报转化为瑞士区域概率性千米级降水场。首先,通过特征线性调制的U-Net基于预报时效修正系统性偏差;此校正使后续超分辨率阶段仅需处理降水场本身,可直接基于观测数据训练。接着,扩散模型独立生成细尺度空间变异性。基于AIFS预报与CombiPrecip雷达-雨量计观测数据,该方法使CRPS降低48%。生成场在大尺度与小尺度上的谱保真度分别高于0.85与0.88,对应1公里网格下约4公里的有效分辨率,适用于长达5天的预报。跨时效训练进一步提升远期性能,在第6天实现相对分时段模型13%的CRPS降低。结果表明,生成前显式纠正时效依赖偏差是高效千米级概率降尺度的关键。

原文摘要 · Abstract (English)

Skillful medium-range precipitation forecasting at kilometer scale remains challenging over complex terrain because precipitation arises from multiscale nonlinear processes that global models cannot explicitly resolve at affordable cost. Global AI weather models can produce skillful medium-range forecasts, but their native 0.25 degrees resolution limits direct use for local hazard applications. Statistical downscaling can help bridge this gap, yet existing approaches often struggle with state-dependent, and especially lead-time-dependent, biases in global forecasts. We introduce SwAIther-Precip, a lead-time-aware downscaling framework that converts coarse-resolution AIFS forecasts into probabilistic km-scale precipitation fields over Switzerland. First, a U-Net conditioned on lead time via feature-wise linear modulation deterministically corrects systematic biases at coarse resolution. This targeted correction enables a cheaper super-resolution stage conditioned only on corrected precipitation, allowing direct training on observations rather than on the full atmospheric state. A diffusion-based model then generates fine-scale spatial variability independently of lead time. Using AIFS forecasts and CombiPrecip radar-gauge observations, SwAIther-Precip reduces CRPS by 48% relative to raw AIFS. The generated fields reproduce observed spatial variability with spectral fidelity above 0.85 at large scales and 0.88 at small scales, corresponding to an effective resolution of approximately 4 km on a 1 km grid for lead times up to 5 days. Training across lead times further improves long-range performance, yielding a 13% CRPS reduction at 6 days relative to lead-time-specific models. These results show that explicitly correcting lead-time-dependent biases before generative super-resolution is key to efficient km-scale probabilistic downscaling of global AI precipitation forecasts.

降水预报降尺度扩散模型时空建模

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