Standard sea level
110 kt EAS, 0 ft and 15 °C: 110.0 kt TAS.
Turn air density into a clearer picture of your airspeed.
An estimate for dry air using the standard pressure-altitude model.
Describe what you expected. This creates a report you can send to the site maintainer; it does not submit anything automatically.
Estimate true airspeed from equivalent airspeed, pressure altitude and outside air temperature.
Enter equivalent airspeed (EAS), pressure altitude in feet and outside air temperature in Celsius. CAS is only an approximation for EAS at low Mach.
TAS = EAS / √σ · σ = (1 − 6.87535 × 10⁻⁶ × h)^5.2561 × 288.15 / (T + 273.15)θ is wind direction minus runway heading or course, normalized to −180° to 180°. V is wind speed. Results round to one decimal; calculations use full precision. Speed units are converted through knots.
110 kt EAS, 0 ft and 15 °C: 110.0 kt TAS.
110 kt EAS, 5,000 ft and 5 °C: approximately 118.3 kt TAS.
First correct IAS for instrument and position errors to CAS. At low Mach, CAS approximates EAS; otherwise apply compressibility correction.
At lower density, a higher true speed is needed to produce the same dynamic pressure.
Dry-air tropospheric model only, −2,000 to 36,000 ft. Humidity and compressibility corrections are not included; this is not a high-speed air-data computer. This tool does not replace your aircraft operating handbook, official weather, regulations or pilot judgement.
Updated 11 September 2026. Automated checks cover the mathematical model; an independent aviation review is pending.
Reference: FAA aviation handbooks · Models and limitations