What Reynolds number measures
The Reynolds number is the ratio of inertial to viscous forces in a flow:
Re = ρ V L / μ = V L / ν
Two geometrically similar bodies at the same Reynolds number have the same relative balance of those forces, which is why a wind-tunnel model is tested at a Reynolds number as close as possible to the full-size airplane. Laminar-to-turbulent transition, skin friction, and the behavior of a high-lift system all depend on Re.
Air properties
For atmospheric flight the density ρ and the dynamic viscosity μ come from the ambient air. This page can take them from the U.S. Standard Atmosphere 1976 at a geopotential altitude (Sutherland’s law for μ), or from a pressure and temperature, or from values you type. At sea-level ISA, ρ = 1.225 kg/m³ and μ ≈ 1.7894×10−5 Pa·s, so a 1 m chord at 50 m/s has Re ≈ 3.42×106.
A rough sea-level rule of thumb is Re ≈ 10,735 × Vkt × Lft. Use the calculator, not the thumb rule, when altitude or temperature matters.
Sources
NASA Glenn Beginner’s Guide to Aeronautics (Reynolds number); U.S. Standard Atmosphere 1976 (Sutherland constants); Anderson, Fundamentals of Aerodynamics.
Frequently asked questions
What length should I use for a wing Reynolds number?
The reference chord — typically the mean aerodynamic chord for a whole wing, or the local chord at a span station. For a fuselage or a boom, use a length; for a circular cylinder or a landing-gear leg, use the diameter.
Does Reynolds number change with altitude?
Yes. Density falls faster than viscosity, so Re at a given true airspeed and length is lower at altitude than at sea level. That is one reason high-altitude cruise and low-Reynolds-number UAV work need care with transition and flap effectiveness.
What viscosity law is used with the ISA option?
Sutherland’s law as in the U.S. Standard Atmosphere 1976, μ = β T3/2/(T+S), with the same constants as the standard-atmosphere calculator on this site.