WeatherNext 3 was published as a technical report - "WeatherNext 3: Increasing resolution and performance of global weather models with raw observations" (arXiv 2609.03582) - released alongside the September 3, 2026 launch. It is long and dense, so this page distills what it documents, the numbers to look for and the caveats to keep in mind. The paper remains the authority; treat this as a map, not a substitute. For the product view, see the release timeline and the model overview.
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Each figure below is traceable to the paper. The commentary is ours.
New forecasts every hour instead of every six, by ingesting low-latency geostationary satellite mosaics - the most recent frame arrives with under an hour of latency.
Single-level variables such as solar radiation and cloud cover resolve at 0.1 degree on hourly time steps, on par with physics-based global models. WeatherNext 2 ran at 0.25 degrees.
Forecasts run as 15-day, 64-member ensembles, with members sampled by injecting noise into the model and skill scored with CRPS across the members.
Four threads carry most of the report. Understanding them is most of understanding the paper.
The model ingests geostationary satellite mosaics - infrared and visible bands covering water vapor, temperature and clouds - plus tropical cyclone fixes and station observations, instead of relying only on analysis fields.
Beyond classic analysis variables, it learns satellite-derived precipitation products at 0.1 degree, including IMERG-based estimates and a product the team calls PARDIG that its internal checks rank closer to independent observations.
Modelling sparse station data lets 2 m temperature and dewpoint be predicted at any location, conditioned on local geography, with reported error substantially lower than competing global models - including at stations never seen in training.
Headline scores use CRPS, the standard probabilistic metric, measured against named references and ensemble baselines such as ECMWF ENS and AIFS ENS, with scorecards comparing model generations at matched resolution.
The report rewards a specific route more than a linear read.
The abstract names the three headline claims - hourly cadence, on-par resolution, raw-observation training. Go straight to the scorecards before the method.
Captions say what the model was compared against and at which resolution. A score without its reference tells you little, especially where older forecasts were interpolated for the comparison.
Skill differences shift with forecast horizon. Look for how far ahead an improvement holds, not just the best row of the best table.
The paper itself flags where evidence is not independent - for example, precipitation verifies partly against products the model also trained on. Read those lines before quoting numbers.
Knowing the edges of a result is as useful as knowing the result.
The reported improvements are strongest where forecasting was historically weakest. Your local baseline may already be strong, so judge the paper by its regional detail, not its headlines.
Where generations are compared at 0.1 degree, the older model's forecasts were interpolated upward. That is stated in the paper, but easy to miss in a skim.
Nothing in the paper changes who owns warnings: national meteorological agencies remain the source for safety decisions, wherever the forecast comes from.
Evaluation continues after publication, including live leaderboards that rescore model runs as new observations arrive. Treat published numbers as a snapshot.
Short answers about the report, its numbers and how to use it.
Related reading: the model overview and accuracy, explained.
The paper explains the machine; the workspace shows you its output for your own coordinates. Start the 7-day free trial, or read how to sanity-check accuracy first.