Density altitude is the altitude the airplane “feels”: the height in the standard atmosphere where the air is as thin as it is today. Hot days, high airports and low pressure all raise it, which means a longer takeoff roll and a slower climb.
For learning only. This lesson is for studying and ground-school work, not for planning a real flight. Use official weather, charts and flight-planning tools, and the numbers in your aircraft’s handbook (POH).
Try it with your own problem ↓An airport sits at 3,500 ft. The altimeter setting is 30.12 inHg and the temperature is 25 °C. Find the density altitude.
The density altitude is about 5,292 ft: the airplane will perform as if the field were nearly 1,800 ft higher. (The full standard-atmosphere formula gives about 5,193 ft.)
Air gets thinner as you climb, and it also gets thinner as it warms, because warm air expands. The standard atmosphere is a table that pairs each altitude with a standard pressure and temperature. Pressure altitude fixes the pressure; then each degree warmer than standard thins the air about as much as climbing another 120 feet would.
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Work it out: elevation 3,500 ft, altimeter 30.12, 25 °COpens The Flight Computer with this exampleOr try these
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ISA at 5,000 ft is 15 − 10 = 5 °C, so it is 25 °C warmer than standard: 5,000 + 120 × 25 = 8,000 ft.
Thin air gives the engine less power, the propeller less bite and the wings less lift. A takeoff that is easy at sea level can need much more runway on a hot day at a high airport.
No. It is the rule of thumb in the FAA’s handbooks and is close for light airplanes. Flight computers and performance charts use the full standard-atmosphere formula.
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