Weather markets look like the cleanest systematic category on Kalshi: the data is public, the models are well-studied, and most traders just glance at a phone weather app. That pull is real โ€” but the honest operator's version of this guide has to start with the part the hype skips. Most of the "edge" you will compute is your model disagreeing with the market, and the market is frequently right for reasons a single forecast cannot see.

Updated May 2026. This page was rewritten after we built and ran the model end to end, so the framing below is what the data actually showed โ€” not what makes the best sales pitch.

What We Actually Built โ€” And What It Showed

We ran a real, no-cost model against live markets: Kalshi's KXHIGH* daily-high contracts for seven cities (their structured strike fields, not scraped titles) priced against a free Open-Meteo high-temperature forecast, converted to a probability with a normal-CDF model. Real data on both sides, $0 in API spend.

In a representative scan it scored 84 live contracts across the seven cities. The single biggest "edge" it flagged was a New York "high above 84ยฐF" contract: the model said ~98% while the market sat near 81%, a ~17-point gap that looks enormous. It is not free money. It is a multi-day-out forecast combined with an assumed error band, and the market's lower number was pricing uncertainty the model was told to ignore. That gap is the single most important lesson in weather trading: a large model-vs-market disagreement is a question to investigate, not a guarantee of profit.

Why The Naive Edge Is Mostly A Mirage

Three structural traps turn most computed "edges" into noise. A real strategy is mostly about respecting them.

1. Settlement station โ‰  the city

Kalshi settles each market on one specific weather station, not "the city." A forecast pulled for the city center can sit roughly 1ยฐF off the settlement station โ€” and because the brackets settle to an integer ยฐF, ~1ยฐF is often enough to flip which side of the contract wins. If you do nothing else from this guide, map the exact settlement station for every market you trade and forecast that point.

2. Your sigma is unfitted

Turning a forecast into a probability requires a forecast-error distribution. Assuming one (we used โ‰ˆ2.7ยฐF) is a guess, not a measurement โ€” and every probability, and therefore every "edge," is only as good as that number. Real work here is fitting the error band empirically, per station and per forecast horizon, from forecast-vs-actual history. An unfitted sigma is the difference between a concept demo and a strategy.

3. Same-day markets out-know your forecast

By midday the day's high is already partly realized, so a same-day market is pricing information a morning forecast does not have. Trade future days. And note the uncomfortable corollary: model skill decays as the horizon grows, which is exactly where the naive edge looks biggest. The fattest apparent edges live where your model is weakest.

The Honest Method

  1. Use a distribution, not a point. The GFS ensemble (GEFS, 30 members) or ECMWF gives you a spread, not a single number โ€” that spread is the probability.
  2. Map the exact settlement station and forecast that location, not the metro.
  3. Fit your error band empirically per station and horizon. Re-fit it; model bias drifts by season.
  4. Exclude same-day markets by default; trade future days where a forecast genuinely knows more than the tape.
  5. Treat model โˆ’ market as a disagreement to investigate. Size small, expect the market to win more often than your gut wants, and only scale where a real, fitted, station-correct model still disagrees.

The Data Sources

Open-Meteo

Free, no API key, returns a daily high per location. It is what our model used and it is the lowest-friction way to get a real forecast into a bot. It is a point forecast, so pair it with an explicit, fitted error band rather than trusting the single number.

GFS / GEFS (Global Forecast System)

Free via NOAA, updated every 6 hours. The GEFS ensemble runs 30 perturbation members, giving you the probability distribution directly instead of a synthetic one.

ECMWF (European Model)

Generally more accurate than GFS at the 3โ€“7 day range. Some data is free; high-resolution data is subscription. When GFS and ECMWF agree, your error band can tighten; when they diverge, that disagreement is itself the signal that the market may be right to be uncertain.

HRRR (High-Resolution Rapid Refresh)

Hourly, 3 km resolution, best for next-day forecasts. Useful for tracking how the forecast โ€” and your fitted uncertainty โ€” moves as an event approaches.

Automating It Properly

Automation helps here, but not for the reason the hype implies. It is not about firing on raw divergence faster than everyone else. It is about doing the disciplined version consistently: the same station mapping every time, a fitted error band instead of a guessed one, future-day markets only, and small position sizing on genuine disagreements.

Build that with our Python tutorial or our no-code builder with weather signals โ€” and wire in the guardrails above, not a bare model-minus-market trigger.

Automate The Disciplined Version

Our signal system can connect weather data feeds to your bots โ€” so the station mapping, the future-day filter, and your position sizing run the same way every time.

Build a Weather Bot โ†’

MR

Marcus Rivera

Head of Quantitative Strategy

Marcus Rivera is Head of Quantitative Strategy at Bot for Kalshi. A former prop trader with a background in financial engineering, he now focuses exclusively on prediction market alpha. He's traded over $2M in prediction market volume across Kalshi and legacy futures exchanges.