Kolmogorov Microscale Calculator

Find the Kolmogorov length, time, and velocity microscales, the smallest eddies where turbulent kinetic energy dissipates into heat.

🌀 Kolmogorov Microscale Calculator
m²/s
m²/s³
Kolmogorov length η (mm)
Kolmogorov time τη (ms)
Kolmogorov velocity vη (mm/s)
Step-by-step working

🌀 What is the Kolmogorov Microscale Calculator?

This Kolmogorov microscale calculator finds the three smallest scales of turbulence, the length scale η, the time scale τ_η, and the velocity scale v_η, from just two inputs: the fluid's kinematic viscosity ν and the turbulent kinetic energy dissipation rate ε. These scales mark the bottom of the turbulent energy cascade, the point where the smallest eddies stop breaking into smaller ones and instead dissipate their kinetic energy into heat through molecular viscosity.

Turbulence researchers, mechanical and aerospace engineers, and meteorologists use Kolmogorov microscales constantly. They set the required grid resolution for Direct Numerical Simulation (DNS) of turbulent flow, since a simulation grid coarser than η cannot capture the full energy cascade. They also help estimate mixing efficiency in chemical reactors, the size of the smallest droplets a turbulent spray can produce, and the finest structures visible in atmospheric or oceanic turbulence.

A common misconception is that the Kolmogorov length scale is a fixed physical size. It is not, it depends entirely on the local dissipation rate ε and the fluid's viscosity ν, so it varies from millimeters in gentle atmospheric turbulence down to fractions of a millimeter in intense turbulence such as inside a jet engine or a high-speed mixing tank. Another useful fact: the Kolmogorov microscale Reynolds number, Re_η = v_η·η/ν, always equals exactly 1, by the very definition of the scale as the point where inertial and viscous forces balance.

This calculator is useful for anyone studying fluid dynamics, computational fluid dynamics (CFD) mesh design, atmospheric science, or turbulent mixing who needs a fast, reliable Kolmogorov microscale estimate without deriving the exponents by hand.

📐 Formula

η  =  (ν³ / ε)1/4
η = Kolmogorov length scale, m
ν = kinematic viscosity, m²/s
ε = turbulent kinetic energy dissipation rate, m²/s³ (equivalently W/kg)
τη = (ν / ε)1/2, the Kolmogorov time scale in seconds
vη = (ν×ε)1/4, the Kolmogorov velocity scale in m/s
Example: air at 20°C (ν=1.5×10-5, ε=1×10-3): η ≈ 1.3554 mm, τη ≈ 122.4745 ms, vη ≈ 11.0668 mm/s.

📖 How to Use This Calculator

Steps

1
Pick a preset or enter kinematic viscosity - Choose air or water to auto-fill a typical kinematic viscosity, or enter your own value in m²/s.
2
Enter the dissipation rate - Enter the turbulent kinetic energy dissipation rate ε in m²/s³ (equivalently W/kg).
3
Calculate the microscales - Click Calculate to get the Kolmogorov length, time, and velocity microscales.
4
Read the results and chart - See η in millimeters, τη in milliseconds, vη in millimeters per second, and how η shrinks as dissipation rate rises.

💡 Example Calculations

Example 1 - Air, moderate atmospheric turbulence

1
ν=1.5×10-5 m²/s (air), ε=1×10-3 m²/s³ (typical atmospheric boundary layer)
2
η = (ν³/ε)1/4 = 1.3554 mm, τη = (ν/ε)1/2 = 122.4745 ms, vη = (ν×ε)1/4 = 11.0668 mm/s
3
The smallest atmospheric eddies are on the order of a millimeter, well below anything visible to the eye
η = 1.3554 mm, τη = 122.4745 ms, vη = 11.0668 mm/s
Try this example →

Example 2 - Water, turbulent mixing tank

1
ν=1.0×10-6 m²/s (water), ε=1×10-2 m²/s³ (stirred tank turbulence)
2
η = (ν³/ε)1/4 = 0.1000 mm, τη = (ν/ε)1/2 = 10.0000 ms, vη = (ν×ε)1/4 = 10.0000 mm/s
3
Water's lower viscosity gives a smaller Kolmogorov length than air even though ε is ten times higher here
η = 0.1000 mm, τη = 10.0000 ms, vη = 10.0000 mm/s
Try this example →

Example 3 - Air, intense turbulence

1
ν=1.5×10-5 m²/s (air), ε=0.1 m²/s³ (intense turbulence, e.g. near a jet)
2
η = (ν³/ε)1/4 = 0.4286 mm, τη = (ν/ε)1/2 = 12.2474 ms, vη = (ν×ε)1/4 = 34.9964 mm/s
3
A 100× jump in dissipation rate over Example 1 shrinks η by only about 3.2×, since η scales with ε-1/4
η = 0.4286 mm, τη = 12.2474 ms, vη = 34.9964 mm/s
Try this example →

❓ Frequently Asked Questions

What is the Kolmogorov microscale?+
The Kolmogorov microscale is the smallest length scale in a turbulent flow, the size of the smallest eddies, where turbulent kinetic energy is dissipated into heat by molecular viscosity. Below this scale, turbulence smooths out into laminar, viscosity-dominated motion.
What is the formula for the Kolmogorov length scale?+
η = (ν³/ε)^(1/4), where ν is kinematic viscosity in m²/s and ε is the turbulent kinetic energy dissipation rate in m²/s³ (equivalently W/kg). It is one of three Kolmogorov microscales, alongside a time scale and a velocity scale.
What are the Kolmogorov time and velocity scales?+
The Kolmogorov time scale is τ_η = (ν/ε)^(1/2) and the Kolmogorov velocity scale is v_η = (νε)^(1/4). Together with the length scale η, they describe the smallest, fastest-dissipating eddies in a turbulent flow, all three combine so that η/τ_η = v_η exactly.
Why is the Kolmogorov microscale Reynolds number always 1?+
By definition, the Kolmogorov scale is the point in the turbulent energy cascade where inertial forces and viscous forces are equal in magnitude, so Re_η = v_η·η/ν = 1 always, regardless of the values of ν and ε. This is the defining property of the scale, not a coincidence.
How does dissipation rate ε affect the Kolmogorov length scale?+
Higher dissipation rate ε produces a smaller Kolmogorov length scale, since η = (ν³/ε)^(1/4) decreases as ε increases. More intense turbulence cascades energy down to progressively finer eddies before viscosity converts it to heat.
What is a typical Kolmogorov length scale for atmospheric turbulence?+
For air (ν ≈ 1.5×10⁻⁵ m²/s) with a typical atmospheric dissipation rate of ε ≈ 10⁻³ m²/s³, the Kolmogorov length scale works out to roughly 1.36 mm. Stronger turbulence, higher ε, pushes this down to a fraction of a millimeter.
Why does water have a smaller Kolmogorov length scale than air at the same dissipation rate?+
Water's kinematic viscosity (ν ≈ 1.0×10⁻⁶ m²/s) is about 15 times smaller than air's, and η scales with ν^(3/4), so at the same dissipation rate water's smallest turbulent eddies are markedly finer than air's.
Why do Kolmogorov microscales matter for turbulence simulation?+
Direct Numerical Simulation (DNS) of turbulence must resolve the computational grid down to roughly the Kolmogorov length scale η to capture the full energy cascade without a turbulence model, which is why DNS grids for high-Reynolds-number flows require enormous numbers of grid points.
What units are used for the dissipation rate ε?+
The turbulent kinetic energy dissipation rate ε is measured in m²/s³, which is dimensionally identical to W/kg (watts of dissipated power per kilogram of fluid mass). Both units describe the same physical quantity.
Is the Kolmogorov length scale the same as the boundary layer thickness?+
No. The Kolmogorov length scale η describes the smallest eddies in fully developed turbulence anywhere in a flow, while boundary layer thickness describes the wall-normal extent of the velocity profile near a solid surface. They are related but answer different questions.
Who introduced the Kolmogorov microscales?+
Soviet mathematician Andrey Kolmogorov introduced these scales in his 1941 theory of turbulence, which describes how kinetic energy cascades from large, energy-containing eddies down through the inertial subrange to the smallest, viscosity-dominated eddies at the Kolmogorov scale.

What is the Kolmogorov microscale?

The Kolmogorov microscale is the smallest length scale in a turbulent flow, the size of the smallest eddies, where turbulent kinetic energy is dissipated into heat by molecular viscosity. Below this scale, turbulence smooths out into laminar, viscosity-dominated motion.

What is the formula for the Kolmogorov length scale?

η = (ν³/ε)^(1/4), where ν is kinematic viscosity in m²/s and ε is the turbulent kinetic energy dissipation rate in m²/s³ (equivalently W/kg). It is one of three Kolmogorov microscales, alongside a time scale and a velocity scale.

What are the Kolmogorov time and velocity scales?

The Kolmogorov time scale is τ_η = (ν/ε)^(1/2) and the Kolmogorov velocity scale is v_η = (νε)^(1/4). Together with the length scale η, they describe the smallest, fastest-dissipating eddies in a turbulent flow, all three combine so that η/τ_η = v_η exactly.

Why is the Kolmogorov microscale Reynolds number always 1?

By definition, the Kolmogorov scale is the point in the turbulent energy cascade where inertial forces and viscous forces are equal in magnitude, so Re_η = v_η·η/ν = 1 always, regardless of the values of ν and ε. This is the defining property of the scale, not a coincidence.

How does dissipation rate ε affect the Kolmogorov length scale?

Higher dissipation rate ε produces a smaller Kolmogorov length scale, since η = (ν³/ε)^(1/4) decreases as ε increases. More intense turbulence cascades energy down to progressively finer eddies before viscosity converts it to heat.

What is a typical Kolmogorov length scale for atmospheric turbulence?

For air (ν ≈ 1.5×10⁻⁵ m²/s) with a typical atmospheric dissipation rate of ε ≈ 10⁻³ m²/s³, the Kolmogorov length scale works out to roughly 1.36 mm. Stronger turbulence, higher ε, pushes this down to a fraction of a millimeter.

Why does water have a smaller Kolmogorov length scale than air at the same dissipation rate?

Water's kinematic viscosity (ν ≈ 1.0×10⁻⁶ m²/s) is about 15 times smaller than air's, and η scales with ν^(3/4), so at the same dissipation rate water's smallest turbulent eddies are markedly finer than air's.

Why do Kolmogorov microscales matter for turbulence simulation?

Direct Numerical Simulation (DNS) of turbulence must resolve the computational grid down to roughly the Kolmogorov length scale η to capture the full energy cascade without a turbulence model, which is why DNS grids for high-Reynolds-number flows require enormous numbers of grid points.

What units are used for the dissipation rate ε?

The turbulent kinetic energy dissipation rate ε is measured in m²/s³, which is dimensionally identical to W/kg (watts of dissipated power per kilogram of fluid mass). Both units describe the same physical quantity.

Is the Kolmogorov length scale the same as the boundary layer thickness?

No. The Kolmogorov length scale η describes the smallest eddies in fully developed turbulence anywhere in a flow, while boundary layer thickness describes the wall-normal extent of the velocity profile near a solid surface. They are related but answer different questions.

Who introduced the Kolmogorov microscales?

Soviet mathematician Andrey Kolmogorov introduced these scales in his 1941 theory of turbulence, which describes how kinetic energy cascades from large, energy-containing eddies down through the inertial subrange to the smallest, viscosity-dominated eddies at the Kolmogorov scale.