Joseph R. Badick - Flight Theory and Aerodynamics

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FLIGHT THEORY
AERODYNAMICS
GET A PILOT’S PERSPECTIVE ON FLIGHT AERODYNAMICS FROM THE MOST UP-TO-DATE EDITION OF A CLASSIC TEXT Flight Theory and Aerodynamics
Flight Theory and Aerodynamics
Flight Theory and Aerodynamics

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Indicated Airspeed

Indicated airspeed (IAS) is the direct reading of the airspeed indicator, and is uncorrected for errors related to installation or nonstandard atmospheric density. If there are any errors in the instrument, they may be shown on an instrument error card located near the instrument and/or in the AFM.

Calibrated Airspeed

Calibrated airspeed (CAS) is obtained when the necessary corrections have been made to the IAS for installation error and instrument error. These position errors are especially prevalent at lower airspeeds, and the IAS may be “indicating” slower than the CAS. Most of the time in non‐pressurized aircraft operating at lower altitudes, the CAS can be assumed to be within several knots of the IAS.

Equivalent Airspeed

Equivalent airspeed (EAS) results when the CAS has been corrected for compressibility effects. Figure 2.12shows a compressibility correction chart. In general, if flying above 10 000 ft and 200 kts., the compressibility correction should be made. Unlike the instrument and position error charts, which vary with different aircraft, this chart is good for any aircraft.

EAS is not a significant factor in airspeed computations when aircraft fly at relatively low speeds and altitudes, but at higher speeds and altitudes, the compressibility correction must be taken into account. For example, if an aircraft is flying at a pressure altitude of 20 000 ft at a CAS of 400 kts., Figure 2.12indicates a compressibility correction of −17.5 kts. The EAS for this example is 382.5 kts.

Figure 212 Compressibility correction chart True Airspeed True airspeed - фото 76

Figure 2.12 Compressibility correction chart.

True Airspeed

True airspeed (TAS) is obtained when EAS has been corrected for density ratio, the airspeed indicator 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 Flight Theory and Aerodynamics - изображение 77:

(2.12) Flight Theory and Aerodynamics - изображение 78

Values of картинка 79can be found in the ICAO Standard Altitude Chart ( Table 2.1); values of 1/ картинка 80can be found in Figure 2.13.

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.

Figure 213 Altitude and EAS to TAS correction chart EXAMPLE Using our - фото 81

Figure 2.13 Altitude and EAS to TAS correction chart.

EXAMPLE

Using our example from the CAS discussion, EAS was determined to be 382.5 kts. If the outside air temperature at a pressure altitude of 20 000 ft is −30 °C, we can utilize Eq. 2.12to find the TAS. From Table 2.1, the pressure ratio ( δ ) is 0.4595.

Figure 214depicts the change in TAS between sea level and 15 000 ft when the - фото 82

Figure 2.14depicts the change in TAS between sea level and 15 000 ft when the IAS remains constant. For the respective IAS, the CAS calibration has been applied. As the aircraft climbs, the TAS increases as the air density decreases. The aircraft must travel at 130 kts. TAS to register 100 kts. on the airspeed indicator.

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

Figure 214 IAS CAS and TAS comparison Source US Department of - фото 83

Figure 2.14 IAS, CAS, and TAS comparison.

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) картинка 84

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.

Groundspeed Groundspeed GS is the actual speed of the aircraft over the - фото 85

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.

SYMBOLS

a Speed of sound (local for a given condition)
A Area (ft 2)
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
°R Rankine temperature
TAS True airspeed
T Absolute temperature
T 0 Sea level standard temperature
V Velocity (fps)
V k Velocity (kts.)
δ (delta) Pressure ratio
θ (theta) Temperature ratio
ρ (rho) Density
σ (sigma) Density ratio

KEY TERMS

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