Numerical weather prediction
Builds on Initial value problemPrimitive equationsData assimilationNumerical analysisButterfly effect
Definition
Let be a numerical model of the atmosphere. It is a discretisation in space and time, by the methods of numerical analysis, of partial differential equations for the atmospheric state. Typical equations are the primitive equations, together with parametrisations of unresolved processes. The model state is a vector of grid-point or spectral values, and one step of the model maps to . Numerical weather prediction is the forecasting of the weather by the following procedure.
- An analysis of the current state is computed from observations and a previous forecast by data assimilation.
- The initial value problem is solved forward: with , up to the forecast range.
- The forecast fields are converted into weather variables at the times and places of interest.
Remarks
The procedure is repeated in cycles, typically every or hours, and the short-range forecast of one cycle is the background for the next analysis. In ensemble prediction, step 2 is repeated from several perturbed analyses, and the spread of the forecasts estimates their uncertainty.
Example: the first successful numerical forecast, in 1950, used the barotropic vorticity equation on a grid over North America and was computed on the ENIAC computer.
Non-example: a statistical forecast that predicts tomorrow's temperature by regression on past observations, without integrating equations of motion, is not numerical weather prediction in this sense.
Because the atmosphere is chaotic, errors in grow with time, the butterfly effect, and this limits the useful range of deterministic forecasts to about two weeks.
Reading path
To understand this page from the ground up, read these 6 pages in order. The foundations come first.
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- no evidence level
- Butterfly effect concept
- Data assimilation concept
- Initial value problem concept
- Numerical analysis concept
- Primitive equations concept
- Numerical weather prediction definition
Further reading
About this page
| Tag | ED6Q47PKTG |
|---|---|
| URI | m2://ED6Q47PKTG |
| Kind | definition |
| Writing | W0 stub |
| MSC | 86A10, 65M06, 35Q86 |
| Defines | Numerical weather prediction |
| Uses | Initial value problem, Primitive equations, Data assimilation, Numerical analysis, Butterfly effect |
| Changed | 3 November 2026 |
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