Fluid mechanics Turbulence Concept
Turbulence
Summary
Turbulence is the irregular, chaotic state of fluid motion that occurs at high Reynolds number. A turbulent flow has eddies over a wide range of sizes, and it mixes and dissipates energy far faster than a smooth flow. Its details are unpredictable, while its averages are reproducible. It is described by the Navier–Stokes equations, but no general theory derives its statistics from them. Most flows in nature and engineering, from rivers to jet engines, are turbulent.
Where this leads
15 pages build on this one.
- Law of the wall
- Kolmogorov 1941 theory
- Monin–Obukhov similarity theory
- Large eddy simulation
- Kraichnan's inverse cascade in two-dimensional turbulence
- Laminar–turbulent transition
- Reynolds decomposition
- Intermittency in turbulence
- Energy cascade
- Reynolds stress
- Planetary boundary layer
- Kolmogorov four-fifths law
- Taylor microscale
- Kolmogorov microscales
- Kármán–Howarth equation
Further reading
About this page
| Tag | VY307F8Z0S |
|---|---|
| URI | m2://VY307F8Z0S |
| Kind | concept |
| Writing | W0 stub |
| MSC | 76F02 |
| Same as | |
| Changed | 3 November 2026 |
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Results about this
- Law of the wall
- Turbulence closure problem
- Kolmogorov 1941 theory
- Kolmogorov four-fifths law
- Kármán–Howarth equation
Used by
- Law of the wall
- Kolmogorov 1941 theory
- Monin–Obukhov similarity theory
- Large eddy simulation
- Kraichnan's inverse cascade in two-dimensional turbulence
- Laminar–turbulent transition
- Reynolds decomposition
- Intermittency in turbulence
- Energy cascade
- Reynolds stress
- Planetary boundary layer
- Kolmogorov four-fifths law
- Taylor microscale
- Kolmogorov microscales
- Kármán–Howarth equation