Density altitude

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Density Altitude Computation Chart.

Density altitude is the altitude in the International Standard Atmosphere at which the air density would be equal to the actual air density at the place of observation. "Density Altitude" is the pressure altitude adjusted for non-standard temperature.

Both an increase in temperature and humidity will cause a reduction in air density. Thus, in hot and humid conditions, the density altitude at a particular location may be significantly higher than the true altitude.

Air density is perhaps the single most important factor affecting airplane performance. It has a direct bearing on:[1]

  • The lift generated by the wings — reduction in air density reduces the wing's lift.
  • The efficiency of the propeller — which for a propeller (effectively an airfoil) behaves similarly to lift on wings.
  • The power output of the engine — power output depends on oxygen intake, so the engine output is reduced as the equivalent "dry air" density decreases and produces even less power as moisture displaces oxygen in more humid conditions.

As a result of a density altitude that is higher than the actual physical altitude, the following effects are observed:[1]

  • The aircraft will accelerate more slowly down the runway as a result of reduced power production.
  • The aircraft will need to achieve a higher true airspeed to attain the same lift - this implies both a longer roll down the runway before liftoff and a higher true airspeed which must be maintained when airborne to avoid stalling.
  • The aircraft will climb more slowly as the result of reduced power production and lift.
  • The aircraft service ceiling (maximum altitude which can be attained) will be lower due to both lower power output and reduced lift, reducing the ability to fly above obstacles such as mountains

Density altitude can be calculated from atmospheric pressure and temperature (assuming dry air).


\mathrm{DA} = 145426 \left[1-\left(\frac{P_0/P_{SL}}{\mathrm{T}/T_{SL}}\right)^b\right]

where

DA = density altitude in feet
P0 = atmospheric (static) pressure
PSL = standard sea level atmospheric pressure (101.325 kPa)
T = true (static) air temperature in kelvins (K) [add 273.15 to the Celsius (°C)] figure
TSL = standard sea level air temperature (288.15 K)
b = 0.235

Easy formula to calculate density altitude from pressure altitude

This is an easier formula to calculate (with great approximation) density altitude from pressure altitude and International Standard Atmosphere temperature deviation

Density altitude in feet = pressure altitude in feet + (120 x (OAT - ISA_temperature))

Where:

OAT = Outside air temperature in °C
ISA_temperature = 15 °C - (1.98 °C/1000 ft × pressure altitude in feet)

  1. ^ a b AOPA Flight Training, Volume 19, Number 4; April 2007; Aircraft Owners and Pilots Association; ISSN 1047-6415

This article incorporates text from Pilot's Handbook of Aeronautical Knowledge, a public domain work of the United States Government.

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