Climate model
Builds on Navier–Stokes equationsRadiative transfer equationPartial differential equationOrdinary differential equation
Definition
A climate model is a mathematical model of the climate system, given by:
- state variables, such as temperature, velocity, humidity, salinity and ice cover, for one or more components (atmosphere, ocean, land, ice, biosphere);
- ordinary or partial differential equations for these variables, from conservation of mass, momentum and energy, with radiation to space;
- prescribed external forcings, such as the incoming solar radiation and the atmospheric concentrations of greenhouse gases, or equations for them.
The climate predicted by the model is the statistics of its solutions over long times, rather than a single trajectory.
Remarks
Example: a general circulation model of the atmosphere solves the primitive equations on a grid over the globe. These approximate the Navier–Stokes equations for a thin layer on a rotating sphere, and are coupled with the radiative transfer equation. It meets clause 1 with fields on the grid, clause 2 with the primitive equations and the energy equation, and clause 3 with the solar input and the gas concentrations.
Non-example: a statistical fit of observed temperatures against time is not a climate model, since it has no evolution equations derived from conservation laws (clause 2 fails).
Processes too small for the grid, such as clouds and turbulence, enter through parameterisations, which express their average effect in terms of the resolved variables.
Reading path
To understand this page from the ground up, read these 5 pages in order. The foundations come first.
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- no evidence level
- Navier–Stokes equations concept
- Ordinary differential equation concept
- Partial differential equation concept
- Radiative transfer equation example
- Climate model definition
Further reading
About this page
| Tag | 54FR8EYWZ6 |
|---|---|
| URI | m2://54FR8EYWZ6 |
| Kind | definition |
| Writing | W0 stub |
| MSC | 86A08, 86A10, 35Q86 |
| Defines | Climate model |
| Uses | Navier–Stokes equations, Radiative transfer equation, Partial differential equation, Ordinary differential equation |
| Changed | 3 November 2026 |
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