An ensemble forecast is a set of model forecasts valid for the same time, each started from slightly different initial conditions or run with different versions of a model. Instead of one answer, it shows a range of plausible outcomes and how closely they agree.
Why one run is not enough
The atmosphere is never measured perfectly, and small errors in a model's starting data grow over time. Models also cannot represent processes smaller than their grid or capture every physical process.
An ensemble samples those uncertainties by nudging, or perturbing, the starting data and sometimes by swapping in different physics packages.
Spread, mean and probability
Spread is how far the members fan out from each other. Wide spread points to lower predictability, while tight clustering suggests more confidence in that part of the forecast.
The ensemble mean averages the members, which filters out small, uncertain features and gives a smoother picture. A probability counts how many members meet a threshold, such as an inch of rain, and divides by the total number of members.
Examples as of October 2026
NOAA's Global Ensemble Forecast System (GEFS) has 31 members, one unperturbed control and 30 perturbed runs, at about 25 km. It runs four times a day out to 16 days, with the 00 UTC run extended to 35 days, and a June 2026 bug-fix upgrade brought it to version 12.3.20.
For storm-scale detail, the High Resolution Ensemble Forecast (HREF) combines several models at about 3 km. HREF and the Short-Range Ensemble Forecast (SREF) are scheduled to retire on 10/14/26, replaced by the Rapid Refresh Forecast System and its ensemble.
What an ensemble cannot do
Every member inherits its model's grid, so a 25-km ensemble cannot show individual thunderstorms no matter how many members it has. An 80 percent ensemble probability means 80 percent of members agree, and it needs a forecaster's judgment before it becomes a real-world chance.
