Joseph R. Badick

Flight Theory and Aerodynamics


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measures dynamic pressure and is calibrated for sea level standard day density. As altitude increases, the density ratio decreases and a correction must be made. The correction factor is images:

      Due to the decrease in air density with an increase in altitude, for any given TAS, CAS will decrease as altitude increases. As higher altitudes are attained, the aircraft must fly faster to obtain the same pressure differential. For a given CAS, as an aircraft increases in altitude, the TAS will increase. The higher the aircraft travels in altitude, the greater the difference between CAS and TAS.

Schematic illustration of altitude and EAS to TAS correction chart.

      EXAMPLE

equation

      Understanding the relationship between the speeds above, and the calculation of each one, can be facilitated by remembering “ICE‐T.” IAS is read off the airspeed indicator, CAS is IAS corrected for installation/position errors, EAS is CAS corrected for compressibility, and finally TAS is EAS corrected for temperature and pressure.

      Source: U.S. Department of Transportation Federal Aviation Administration (2013).

      Mach

      The Mach number is found by comparing TAS to the speed of sound for a given set of conditions at a specific altitude. The speed of sound is an important factor in the study of high‐speed flight and is discussed in depth in Chapter 14. Because the aircraft’s speed in relation to the speed of sound is so important in high‐speed flight, airspeeds are usually measured as Mach number (named after the Austrian physicist Ernst Mach). Mach number is the aircraft’s true airspeed divided by the speed of sound (in the same atmospheric conditions):

      (2.13)equation

      where

       M = Mach number

       V = true airspeed (kts.)

       a = local speed of sound (kts.)

      EXAMPLE

      Using the TAS from the previous example (518.6 kts.), when a = 607.3 kts., calculate the Mach number for the aircraft.

equation

      Groundspeed

      Groundspeed (GS) is the actual speed of the aircraft over the ground, either calculated manually or more commonly nowadays read off the GPS (Global Positioning Satellite) navigational unit. The GS increases with a tailwind and decreases with a headwind, and is TAS adjusted for the wind. Groundspeed equals true airspeed in a no wind situation. Consider an airplane that has departed an airport located at sea level, then lands on a runway located at 5000 ft. Even though the IAS on approach will remain the same as if the airplane was landing at sea level, the TAS (and GS) will be higher at the airport with the higher elevation, thus more runway will be utilized during the landing.



a Speed of sound (local for a given condition)
A Area (ft2)
AGL Above ground level
CAS Calibrated airspeed (kts.)
°C Celsius temperature (°)
DA Density altitude
EAS Equivalent airspeed
°F Fahrenheit temperature
GS Groundspeed
H Total pressure(head) (psf)
IAS Indicated airspeed
°K Kelvin temperature
MSL Mean sea level
M Mach number (ratio)
P Static pressure
PA Pressure altitude
P 0 Sea level standard pressure
q Dynamic pressure
R Universal gas constant