True Airspeed Calculator
Use the true airspeed calculator to calculate the true airspeed (referred to as TAS) for all aircraft.
The formula
p = p₀(T/T₀)^5.2559 below the tropopause
Density altitude is what an aircraft feels
Aerodynamic performance depends on air density, and density falls with both altitude and temperature while humidity lowers it further. Density altitude is the altitude at which the standard atmosphere would have the density you actually have — so an aircraft at a 1,500 m airfield on a hot day may be performing as though it were at 3,000 m. "Hot and high" is the classic accident setup, and humidity makes it slightly worse still.
Moisture reducing density surprises people. Water's molar mass is 18 against nitrogen's 28, so vapour displacing air makes the mixture lighter. It is a small effect but it goes the opposite way to intuition.
An airspeed indicator measures dynamic pressure, ½ρv², so in thin air it under-reads the true airspeed. True airspeed grows as the inverse square root of density — roughly 2% per thousand feet, which is the standard mental correction. Indicated airspeed is nonetheless the right thing to fly by, since stall and structural limits also depend on dynamic pressure.
The 5.2559 exponent in the barometric formula is not a fit: it is gM/RL for the standard 6.5 K/km lapse rate. The model is therefore exact within its own assumptions, and departs from reality only where the real lapse rate does.