Density altitude is the altitude in the ISA that has the same air density as the
actual conditions. It is calculated by applying the ISA temperature deviation to
pressure altitude: density altitude = pressure altitude + (ISA deviation × 120),
where ISA deviation is the difference between actual temperature and the ISA
standard temperature for that pressure altitude (15°C minus 1.98°C per 1,000 ft).
Every 1,000-foot increase in density altitude reduces piston engine power by
approximately 3 percent, propeller efficiency by approximately 1–2 percent, and
increases true airspeed at a given indicated airspeed — meaning the aircraft
lifts off at a higher groundspeed, further extending the takeoff roll.
Example Calculation
Field elev: 5,000 ft | QNH: 1010 hPa | OAT: 33°C | Pressure alt: 5,260 ft | Density alt: 8,420 ft
- ISA standard temp at sea level: 15°C, decreasing 1.98°C per 1,000 ft
- Each 1°C above ISA raises density altitude by approximately 120 ft
- Humidity increases density altitude further — often overlooked
- Full-power run-up before departure cannot reveal high density altitude
- Turbine engines are less affected than piston engines but still impacted
Density Altitude Calculator →