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REVIEW 4 major objections 5 minor 8 cited by

FourCastNet 3: A geometric approach to probabilistic machine-learning weather forecasting at scale

T0 review · 4 major / 5 minor · reviewed 2026-08-06 · deepseek-v4-flash

Pith's one-line read FourCastNet 3 claims a purely convolutional, one-step probabilistic model can match diffusion-based ensemble skill while keeping 60-day power spectra realistic.

desk verdict A serious contender with credible medium-range skill; the 60-day spectral evidence is internally inconsistent and must be fixed before the subseasonal claim ships. read the letter →

arxiv 2507.12144 v2 pith:7UQORXY5 submitted 2025-07-16 cs.LG physics.ao-ph

classification cs.LGphysics.ao-ph
keywords probabilisticweatherforecastingsphericalneuraloperatorensembleCRPSlossspectralfidelityhiddenMarkovmodelsubseasonalpredictionmachinelearning
verification ladder T0 review T1 audit T2 compute T3 formal

The pith

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The reading

FourCastNet 3 (FCN3) is a probabilistic machine-learning weather model built as a hidden Markov model: at each 6-hour step it maps the current atmospheric state plus a stochastic latent noise vector to the next state, so sampling the noise generates an ensemble. The paper's central claim is that this one-step scheme, trained end-to-end with a spatial and spectral CRPS objective, beats the standard physics-based ensemble on probabilistic skill, nearly matches the leading diffusion-based probabilistic model, and stays well calibrated with spread-skill ratios near one. Its distinctive claim is spectral fidelity: individual ensemble members keep the correct angular power-spectrum slopes for rollouts of 30 to 60 days, where competing probabilistic ML models show blurring or high-frequency buildup. Training on reanalysis data through 2016, a 50-member 15-day forecast costs about 60 seconds on one GPU, roughly 8 times faster than the diffusion baseline and 60 times faster than the conventional ensemble, which the authors argue makes large subseasonal ensembles practical.

What carries the argument

The load-bearing machinery is the combined objective and noise model. Stochasticity enters through a hidden Markov latent variable $z_n$ sampled from a spherical diffusion process parameterized in spectral space, with eight fixed length scales $k_T$, $\lambda=1$, and $\sigma=1$; this is meant to supply spatio-temporally correlated uncertainty. The loss is a composite of a spatially averaged ensemble CRPS and a spectral CRPS over spherical-harmonic coefficients $\hat{u}^m_\ell$, which the paper argues prevents the pointwise-CRPS failure mode in which shuffled but unrealistic members still score perfectly. The architecture carries the claim through spherical group convolutions: global filters parameterized by the convolution theorem on the sphere, $(\widehat{u\star k})^m_\ell = \hat{u}^m_\ell \hat{k}^0_\ell$, and local discrete-continuous spherical convolutions with Morlet-type wavelet filter bases.

What would settle it

Run the trained 50-member model on out-of-distribution initial conditions, for example the years after the training period or a cluster of heatwaves and cyclones, and compare each ensemble member's angular power spectral density to the reanalysis at 30- and 60-day leads. If the relative spectral error leaves the stated −0.2 to 0.2 band, or spread-skill ratios depart from one, the calibration and spectral-fidelity claims are falsified. A second, cheaper check: retrain with the spectral CRPS term removed; if the power-spectrum slopes remain correct, the paper's causal story about the loss is wrong.

Watch

Extended reading notes

Core claim

FCN3's discovery claim is that probabilistic weather forecasting does not need iterative diffusion sampling: a purely convolutional spherical neural operator, conditioned on noise from a spherical diffusion process, can produce calibrated ensembles in one forward pass per member. The architecture combines eight local discrete-continuous spherical convolutions for every one global spectral convolution, omits layer normalization, and predicts the next state directly rather than a residual tendency; the paper finds this suppresses high-frequency artifact buildup. The training objective couples a pointwise, spatially averaged CRPS with a spectral CRPS that scores the predictive distribution of each spherical-harmonic coefficient, weighted by mode multiplicity; the authors argue this is what keeps spatial correlations and power spectra physically realistic. Evaluated on 50-member ensembles over the out-of-sample year 2020, FCN3 outperforms the conventional physics ensemble and matches the leading diffusion model on 15 of 16 scoring channels at short lead times, at double the temporal resolution; spread-skill ratios approach one, rank histograms flatten, and the angular power spectral density matches the reanalysis ground truth with relative error between −0.2 and 0.2 at a 15-day lead.

Load-bearing premise

The paper's probabilistic claims rest on the assumption that eight hand-chosen spherical-diffusion noise scales, with fixed parameters $\lambda=1$ and $\sigma=1$, adequately represent the atmosphere's true correlated forecast uncertainty; if that noise is misspecified, the ensemble could appear calibrated under the CRPS loss without carrying physical uncertainty, and the 60-day spectral stability need not survive outside the reanalysis distribution.

Editorial extensions

If this is right

  • If the claims hold, operational centers could replace CPU-heavy ensemble weather prediction with one-GPU ML ensembles for medium-range and early-warning products.
  • A 60-day forecast at 0.25° and 6-hourly resolution in under 4 minutes on a single GPU makes subseasonal ensemble studies no longer compute-bound.
  • The spectral-stability claim implies the model can be autoregressed for 240 steps without the small-scale noise buildup that precedes blow-up in other probabilistic ML models.
  • The paper's success with a 50-member ensemble, larger than the 16 members used in training, indicates ensemble size can be scaled up without losing calibration.

Reading between the lines

Editorial extensions of the paper, not claims the author makes directly.

  • Inference: the eight fixed noise scales are the fragile part; if the real forecast-error covariance is dominated by scales outside the chosen $k_T$ set, CRPS calibration could be achieved by construction rather than by physical representativeness. Adding data-assimilation perturbations to the noise would test this.
  • Inference: the speed comparison is at double temporal resolution, so the per-step cost advantage over the diffusion baseline is real but the wall-clock comparison partly reflects this resolution difference.
  • Inference: scoring each spectral mode's distribution instead of only pointwise marginals is a general principle that could transfer to any spatial probabilistic forecaster, including climate emulators and precipitation nowcasters.
  • Inference: the paper lists precipitation output and assimilation-uncertainty coupling as future work; those additions would test whether the spectral fidelity survives a moisture cycle and realistic initial-condition spread.
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Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, and a circularity audit.

Referee Report

4 major / 5 minor

Summary. The manuscript presents FourCastNet 3 (FCN3), a probabilistic machine-learning weather forecasting system built from spherical convolutions, a hidden-Markov formulation with stochastic noise inputs, and a combined spatial-plus-spectral CRPS training objective. The authors report that FCN3 outperforms IFS-ENS, is competitive with GenCast, is well calibrated at 50 ensemble members, preserves angular power spectra up to 60-day lead times, runs 8–60× faster than the compared baselines, and can be trained at scale using a new domain-decomposition-based model/data parallelism scheme. Evaluation follows WeatherBench 2 practice on the out-of-sample year 2020, including CRPS, RMSE, ACC, spread-skill ratio, rank histograms, case studies, bias maps, and spectral diagnostics. The paper also documents the open-source Makani and torch-harmonics software.

Significance. If the claims hold, FCN3 is a significant advance: it demonstrates that a purely convolutional spherical architecture can match diffusion-based probabilistic skill at a fraction of the inference cost, and it reports spectral and rollout stability at subseasonal lead times that most ML weather models lack. The manuscript is commendably thorough in its evaluation: it uses a 50-member ensemble over the full year 2020, reports both aggregate scores and physical-fidelity diagnostics, includes case studies and bias maps, and makes training and inference code publicly available. The distributed-training contribution (spatial model parallelism with ensemble and batch parallelism) is also noteworthy and well documented. The main reservations concern the evidence for the headline 60-day spectral-stability claim and the interpretation of spectral fidelity given that the training loss directly optimizes it.

major comments (4)
  1. [Appendix F.7, Figure 23] The text and caption of Figure 23 contradict each other: the body text states that the figure shows 'four FCN3 forecast members initialized at 2018-01-01 00:00:00 UTC', while the caption says the angular PSD is 'averaged over daily initial conditions at 00:00:00 UTC and 12:00:00 UTC over the year 2020'. This is load-bearing because the abstract's claim of 'realistic spectra ... at extended lead times of up to 60 days' rests on the 1440-hour (60-day) panel of this figure. If the text is correct, the 60-day evidence is a single-initialization anecdote; if the caption is correct, the paper provides no sampling uncertainty for the 1440-hour PSD, unlike the 360-hour panel in Figure 5 which shows relative-error bounds. Please resolve the inconsistency and, in either case, provide a quantitative comparison with sampling uncertainty (e.g., relative-error bounds over initializations and ensemble members) at the 1440-hour lead time.
  2. [Section 5, Appendix E.1 (Eq. 51)] The spectral-fidelity result is partly by construction: the training objective includes a spectral CRPS term (Eq. 51) that directly encourages the spherical-harmonic coefficients of individual ensemble members to match the ground-truth distribution. The paper acknowledges this in Section 2 and Appendix E.1, and the acknowledgment is welcome. However, the abstract and Section 5 present spectral fidelity as an emergent advantage of the method ('retains perfectly the correct slopes'), which overstates the case for a quantity that is explicitly optimized. Please either temper these claims or provide an evaluation metric that is not a direct training target, such as spectral spread-skill or the spectral CRPS of a model ablated without the spectral loss term, to demonstrate that the 60-day spectral stability is not merely a re-statement of the loss function.
  3. [Abstract and Section 5 (speed comparisons)] The speed-up claims of '8x over GenCast' and '60x over IFS-ENS' compare inference on an NVIDIA H100 with GenCast on a Cloud TPU v5 and IFS on 96 AMD Epyc Rome CPUs, at different temporal resolutions. The paper acknowledges 'barring the differences in hardware and resolution' in Section 5, but the abstract states the speed-ups without qualification. Since speed is a central advertised advantage, please report at least one controlled comparison (same hardware, matched resolution) or clearly attach the hardware caveat to the abstract's speed figures.
  4. [Appendix B.7, Table 1, Figures 15–16] The ensemble's physical uncertainty representation depends on the hand-specified spherical diffusion noise with fixed parameters (eight length scales kT, lambda=1, sigma=1; Table 1, Eq. 27–28). The paper shows good aggregate calibration via spread-skill ratio and rank histograms, but it does not report scale-dependent or spatially resolved verification of ensemble spread, such as spread-skill as a function of spherical harmonic degree or lead-time-dependent spectral spread. Given that the 60-day spectral-stability claim concerns the behavior of individual members, please add a scale-resolved diagnostic (e.g., spectral spread-skill or banded rank histograms) to demonstrate that the ensemble represents uncertainty at the relevant wavelengths rather than only matching marginal pointwise distributions.
minor comments (5)
  1. [Figure 18 caption] The caption for Figure 18 (anomaly correlation coefficient, ACC) states 'Lower scores indicate better skill', but for ACC higher values indicate better skill; this is inconsistent with the caption of Figure 14. Please correct.
  2. [Section 3] In the paragraph describing the decoder, the sentence 'Both encoder and decoder encode do not perform any channel mixing' is grammatically broken; please rephrase, for example as 'Neither the encoder nor the decoder performs any channel mixing'.
  3. [Section G (Scaling FourCastNet 3)] At the end of the introductory paragraph, the sentence 'This is inspired from' is incomplete; please finish the sentence or delete the fragment.
  4. [Throughout] The model name is written inconsistently as 'FCN3' and 'FCN 3' (e.g., 'FCN 3 ensemble', 'FCN3' in captions); please use a single consistent abbreviation.
  5. [Appendix F.2] The text says FCN3 'outperforms IFS-ENS' on probabilistic and deterministic scores; Figure 12 and Figure 13 appear to support this for most channels and lead times, but the claim is made without a statistical significance test. A brief statement on the number of initializations (about 730 per year) and, if possible, confidence intervals for the score differences would strengthen the claim.

Circularity Check

0 steps flagged · score 0.0 of 10

No circularity: skill and calibration are out-of-sample against external baselines; spectral fidelity is an explicit training objective, and the 60-day claim is an evidentiary gap (Fig. 23 caption/text conflict), not a circular reduction.

full rationale

The derivation chain is self-contained: FCN3 is an autoregressive hidden Markov model with explicit stochastic forcing sampled from a published diffusion process (Appendix B.7, Eqs. 27-28, citing Palmer et al. [30]) and trained with a composite CRPS objective (Eqs. 48-51). The headline skill and calibration numbers are evaluated on out-of-sample 2020 initial conditions against independent external baselines (IFS-ENS and GenCast via WeatherBench 2), so they are not fitted inputs renamed as predictions. Self-citations to SFNO [10], Huge Ensembles [7,8], and DISCO [32] provide architectural lineage and context rather than load-bearing reductions, and no uniqueness theorem is imported from the authors' prior work to forbid alternatives. The one near-circular element is spectral fidelity: Eq. 51 computes CRPS per spherical-harmonic coefficient, and the reported angular PSD (Eq. 53) is the squared sum of those same coefficients, so matching the spectrum is explicitly optimized rather than emergent; the paper itself acknowledges this ('the combined CRPS loss function which enforces the correct local and global distribution'). However, the 60-day spectral claim goes beyond the 8-step autoregressive training horizon, so it is extrapolation rather than a by-construction result, and it is evaluated on held-out 2020 data. I also flag an evidence gap that is not circularity: Appendix F.7 text says Figure 23 shows 'four FCN3 forecast members initialized at 2018-01-01 00:00:00 UTC,' while the caption says 'averaged over daily initial conditions at 00:00:00 UTC and 12:00:00 UTC over the year 2020'; under either reading no sampling uncertainty is provided for the 1440-hour PSD, which weakens the abstract's 60-day spectral claim as a correctness matter, not as a circular one.

Assumptions & free parameters 4 free parameters · 6 assumptions · 0 invented entities

No new physical entities are introduced; the latent noise is a standard stochastic parameterization (Palmer et al. [30]). The free parameters are mostly loss weights and noise scales, some unreported (lambda_spectral), that the central spectral-fidelity and calibration claims depend on.

free parameters (4)
  • lambda_spectral = not reported
    Weight of the spectral CRPS term in Eq. (48); central to the spectral-fidelity claim, yet no value or tuning procedure is given in the text.
  • noise process parameters (kT, lambda, sigma) = kT in {3.08e-5,...,5.05e-1}, lambda=1, sigma=1
    Hand-selected in Table 1 / Eq. (28); define the distribution of the latent stochastic variable that drives the ensemble, so calibration depends on their adequacy.
  • local-to-global block ratio = 4 local : 1 global
    Chosen 'through experimentation' (Appendix C.5); affects skill and spectral behavior.
  • channel weights wc and temporal weights w_dt_c = defined in Table 4 and Eq. (49)
    Data-derived from ERA5 statistics; they shape the loss, but are not fitted to the target metric.
assumptions (6)
  • standard math Spherical harmonic transform and convolution theorems are accurate for the grids used.
    Used throughout the architecture (Appendix B).
  • domain assumption ERA5 reanalysis is a valid ground truth for the atmosphere and its spectrum.
    Training target and evaluation reference; spectral fidelity is defined relative to ERA5's T639 spectrum.
  • domain assumption The atmosphere can be modeled as a first-order Markov process on 6-hourly states with an additive latent noise.
    Hidden Markov formulation in Section 2 / Appendix A.2.
  • domain assumption Rotation-equivariant spherical convolutions are appropriate inductive biases for global weather.
    Section 3; assumes no preferred coordinate system beyond zonal/meridional anisotropy captured by kernels.
  • ad hoc to paper Direct state prediction (not tendency) is more stable in rollout; layer normalization should be omitted.
    Appendix C.5 and C.7; empirical, not theoretically justified.
  • ad hoc to paper Noise-centering (sign-flipping paired ensemble members) improves performance.
    Appendix E.3; unexplained and specific to this model.

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Cite this review

Pith. "Pith review of FourCastNet 3: A geometric approach to probabilistic machine-learning weather forecasting at scale." pith.science (2026). https://pith.science/paper/7UQORXY5

@misc{pith2026250712144,
  author       = {Pith},
  title        = {Pith review of: FourCastNet 3: A geometric approach to probabilistic machine-learning weather forecasting at scale},
  year         = {2026},
  howpublished = {\url{https://pith.science/paper/7UQORXY5}},
  note         = {Machine review of arXiv:2507.12144}
}
read the original abstract

FourCastNet 3 advances global weather modeling by implementing a scalable, geometric machine learning (ML) approach to probabilistic ensemble forecasting. The approach is designed to respect spherical geometry and to accurately model the spatially correlated probabilistic nature of the problem, resulting in stable spectra and realistic dynamics across multiple scales. FourCastNet 3 delivers forecasting accuracy that surpasses leading conventional ensemble models and rivals the best diffusion-based methods, while producing forecasts 8 to 60 times faster than these approaches. In contrast to other ML approaches, FourCastNet 3 demonstrates excellent probabilistic calibration and retains realistic spectra, even at extended lead times of up to 60 days. All of these advances are realized using a purely convolutional neural network architecture tailored for spherical geometry. Scalable and efficient large-scale training on 1024 GPUs and more is enabled by a novel training paradigm for combined model- and data-parallelism, inspired by domain decomposition methods in classical numerical models. Additionally, FourCastNet 3 enables rapid inference on a single GPU, producing a 60-day global forecast at 0.25{\deg}, 6-hourly resolution in under 4 minutes. Its computational efficiency, medium-range probabilistic skill, spectral fidelity, and rollout stability at subseasonal timescales make it a strong candidate for improving meteorological forecasting and early warning systems through large ensemble predictions.

Figures

Figures reproduced from arXiv: 2507.12144 by the authors.

Figure 1
Figure 1. Schematic of the FourCastNet 3 model. The model predicts the state of the atmosphere at the [PITH_FULL_IMAGE:figures/full_fig_p002_1.png] view at source ↗
Figure 2
Figure 2. Illustration of model- and data-parallelism for training of FourCastNet 3. In the given example, [PITH_FULL_IMAGE:figures/full_fig_p005_2.png] view at source ↗
Figure 3
Figure 3. Probabilistic skill of FourCastNet 3 relative to the ERA5 ground truth. Continuously ranked [PITH_FULL_IMAGE:figures/full_fig_p006_3.png] view at source ↗
Figures from the paper (23 more)
Figure 4
Figure 4. Figure 4: FourCastNet 3 prediction of storm Dennis initialized on 2020-02-11 at 00:00:00 UTC. The [PITH_FULL_IMAGE:figures/full_fig_p007_4.png]
Figure 5
Figure 5. Figure 5: Comparison of angular power spectral densities of a single FourCastNet 3 ensemble member at [PITH_FULL_IMAGE:figures/full_fig_p008_5.png]
Figure 6
Figure 6. Figure 6: Illustration of the equiangular (lat/lon-) grid in blue and a Gaussian grid in red. Both grids [PITH_FULL_IMAGE:figures/full_fig_p018_6.png]
Figure 7
Figure 7. Figure 7: Depiction of random filters k(x) resulting from the filter parametrization. The spectral filter on the left is parameterized as a linear combination of globally supported spherical harmonics, whereas the local filter on the right is parameterized as a linear combinatio…
Figure 8
Figure 8. Figure 8: Illustration of the Morlet-type wavelet filter basis, used to represent localized filters on the [PITH_FULL_IMAGE:figures/full_fig_p020_8.png]
Figure 9
Figure 9. Figure 9: FourCastNet 3 encoder and decoder. Atmospheric, surface and auxiliary channels are all encoded [PITH_FULL_IMAGE:figures/full_fig_p023_9.png]
Figure 10
Figure 10. Figure 10: Illustration of a single processor block. Green blocks indicate convolutions which take spatial [PITH_FULL_IMAGE:figures/full_fig_p023_10.png]
Figure 11
Figure 11. Figure 11: Mean and variance of activations for 8 randomly initialized instances of FourCastNet 3 and [PITH_FULL_IMAGE:figures/full_fig_p025_11.png]
Figure 12
Figure 12. Figure 12: Continuously ranked probability scores (CRPS) averaged over initial conditions at 00:00:00 [PITH_FULL_IMAGE:figures/full_fig_p031_12.png]
Figure 13
Figure 13. Figure 13: Ensemble-mean root mean squared errors (RMSE), averaged over initial conditions at 00:00:00 [PITH_FULL_IMAGE:figures/full_fig_p031_13.png]
Figure 14
Figure 14. Figure 14: Ensemble-mean anomaly correlation coefficient (ACC), averaged over initial conditions at [PITH_FULL_IMAGE:figures/full_fig_p032_14.png]
Figure 15
Figure 15. Figure 15: Spread-skill ratios (SSR), averaged over initial conditions at 00:00:00 UTC and 12:00:00 UTC [PITH_FULL_IMAGE:figures/full_fig_p033_15.png]
Figure 16
Figure 16. Figure 16: Rank histograms of the ERA5 ground truth within the 50-member FourCastNet 3 ensemble at [PITH_FULL_IMAGE:figures/full_fig_p034_16.png]
Figure 17
Figure 17. Figure 17: Root mean squared errors (RMSE) of a single ensemble member, averaged over initial conditions [PITH_FULL_IMAGE:figures/full_fig_p035_17.png]
Figure 18
Figure 18. Figure 18: Single member anomaly correlation coefficient (ACC), averaged over initial conditions at [PITH_FULL_IMAGE:figures/full_fig_p036_18.png]
Figure 19
Figure 19. Figure 19: Depiction of a single 6-hour forecast initialized at 2018-01-01 00:00:00 UTC compared to the [PITH_FULL_IMAGE:figures/full_fig_p037_19.png]
Figure 20
Figure 20. Figure 20: Depiction of a single 6-hour forecast initialized at 2018-01-01 00:00:00 UTC compared to the [PITH_FULL_IMAGE:figures/full_fig_p038_20.png]
Figure 21
Figure 21. Figure 21: Depiction of a single 60-day forecast initialized at 2018-01-01 00:00:00 UTC compared to the [PITH_FULL_IMAGE:figures/full_fig_p039_21.png]
Figure 22
Figure 22. Figure 22: Bias of a single FourCastNet 3 ensemble member relative to the ERA5 ground truth averaged [PITH_FULL_IMAGE:figures/full_fig_p040_22.png]
Figure 23
Figure 23. Figure 23: Angular power spectral density of FCN3 forecasts at lead times of 6, 360 and 1440 hours, [PITH_FULL_IMAGE:figures/full_fig_p041_23.png]
Figure 24
Figure 24. Figure 24: Zonal power spectral density of ML weather forecasts at the 60 [PITH_FULL_IMAGE:figures/full_fig_p042_24.png]
Figure 25
Figure 25. Figure 25: Communicator hierarchy used in training and inference. To enable multiple forms of parallelism, [PITH_FULL_IMAGE:figures/full_fig_p042_25.png]
Figure 26
Figure 26. Figure 26: Illustration of domain decomposition within Makani for an azimuth group of 4 and a polar [PITH_FULL_IMAGE:figures/full_fig_p043_26.png]

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Forward citations

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Pith tools

Reviewed August 6, 2026 · model on record in the stance chip above.