This post reviews a quantitative benchmark study on whether AI weather models can predict beyond the well-known two-week limit of weather forecasting.
Key points
The experiment
- ETH Zurich researchers ran 9 top AI weather models (Pangu-Weather, GraphCast, FourCastNet, Aurora, SFNO, AIFS, DLESyM, etc.) in autoregressive rollouts of up to two years — 14,600 steps at 6-hour intervals.
- Only three models (Aurora, SFNO, DLESyM) completed the full rollout; six failed along the way.
- *Blow-up*: exponential divergence from physical reality. FourCastNet collapsed after ~8 days; GraphCast diverged after ~300 days.
- *Drift*: slow bias accumulation — seasonal structure persists, but temperatures shift year over year.
- *Loss of seasonality*: Pangu "froze" after ~180 days, producing a time-invariant climate. The cause: Pangu has no time embedding, so it cannot know the calendar date and loses the seasonal signal over long rollouts.
- Adding Gaussian noise to inputs showed Aurora and SFNO progressively remove noise, converging toward physically plausible states — while GraphCast and AIFS amplify noise.
- Aurora produced seasonal, physically realistic weather trajectories from pure white-noise initialization, and even "denoised" an image of a cat mapped onto atmospheric variables back into winter — evidence of an implicit climate attractor.
- Distance-ratio tests show outputs are not memorized training samples: nearest and second-nearest training neighbors are nearly equidistant.
- Attention window size, patch size, normalization type, number of vertical levels, and static variables do not determine stability.
- Time embedding controls seasonality; removing it removes seasons but not stability.
- Spatiotemporal resolution is the key stability factor: coarse resolution (1.5°, 24-hour steps) is more stable than fine resolution (0.25°, 6-hour steps), because fine scales contain high-frequency energy that amplifies during autoregression.
- Ten-year rollouts captured the shape of extreme-event statistics but not magnitudes: Aurora and DLESyM underestimated extreme heat by several degrees; SFNO overestimated extreme cold in some regions.
Three failure modes
Stable models are denoisers
Ablation findings
Extreme weather
Implications
The study frames a fundamental trade-off: short-range precision (fine resolution, short steps) reduces long-range stability, and vice versa — the same tension exists in classical numerical models, but AI models make it visible. AI models trained on historical data may also face untested distribution shifts under climate change. The post argues that AI weather forecasting and AI climate emulation are diverging into two distinct technical paths with different requirements.
References
1. Lehmann et al., "Can AI Weather Models Predict Beyond Two Weeks? A Quantitative Benchmark and Analysis of Long Rollouts", arXiv:2605.30184, 2026. 2. Bodnar et al., "Aurora: A Foundation Model for the Earth System", Nature, 2025. 3. Bonev et al., "Spherical Fourier Neural Operators", ICML 2023. 4. Kochkov et al., "Neural General Circulation Models for Weather and Climate", Nature, 2024. 5. Bi et al., "Pangu-Weather", Nature, 2023.