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MACH NUMBER and AIRSPEED vs. ALTITUDE MACH NUMBER
MACH NUMBER is defined as a speed ratio, referenced to the speed of sound, i.e.
MACH NUMBER = [1] (at the given atmospheric conditions)
Since the temperature and density of air decreases with altitude, so does the speed of sound, hence a given true velocity results
in a higher MACH number at higher altitudes.
AIRSPEED is a term that can be easily confused.
The unqualified term airspeed can mean any of the following:
a. Indicated airspeed (IAS)  the airspeed shown by an airspeed indicator
in an aircraft. Indicated airspeed is expressed in knots and is abbreviated KIAS.
b. Calibrated airspeed (CAS)  indicated airspeed corrected
for static source error due to location of pickup sensor on aircraft. Calibrated airspeed is expressed in knots and is abbreviated KCAS. Normally
it doesn't differ much from IAS.
c. True airspeed (TAS)  IAS corrected for instrument installation error, compressibility error, and
errors due to variations from standard air density. TAS is expressed in knots and is abbreviated KTAS. TAS is approximately equal to CAS at
sea level but increases relative to CAS as altitude increases. At 35,000 ft, 250 KIAS (or KCAS) is approximately 430 KTAS.
IAS
(or CAS) is important in that aircraft dynamics (such as stall speed) responds largely to this quantity. TAS is important for use in navigation
(True airspeed ± windspeed = groundspeed).
Figures 1 and 2 depict relations between CAS and TAS for various altitudes and nonstandard
temperature conditions. The first graph depicts lower speed conditions, the second depicts higher speeds.
As an example of use, consider
the chart on the next page. Assume we are in the cockpit, have read our IAS from the airspeed indicator, and have applied the aircraft specific
airspeed correction to obtain 370 KCAS. We start at point "A" and go horizontally to our flight altitude at point "B" (25,000 ft in this case).
To find our Mach, we go down vertically to point "C" to obtain 0.86 Mach. To get our TAS at our actual environmental conditions, we go from
point "B" vertically until we hit the Sea Level (S.L.) reference line at point "D", then travel horizontally until we reach our actual outside
air temperature (20°C at altitude) at point "E", then go up vertically to read our actual TAS from the scale at point "F" (535 KTAS). If we
wanted our TAS at "standard" temperature and pressure conditions, we would follow the dashed lines slanting upward from point "B" to point "G"
and read 515 KTAS from the scale. Naturally, we could go into the graph at any point and go "backwards" to find CAS from true Mach or TAS.
Figure 3 shows a much wider range of Mach numbers. It contains only TAS and Mach, since aircraft generally do not fly above Mach 2, but
missiles (which don't have airspeed indicators) do. The data on this graph can be obtained directly from the following formula for use at altitudes
of 36,000 ft and below:
[2]
The speed of sound calculated from this formula can be used with the equation on the first page to obtain Mach number. This equation
uses the standard sea level temperature of 59E F and a lapse rate of 3.57°/1000 ft altitude. Temperature stabilizes at 69.7° F at 36,000 ft
so the speed of sound stabilizes there at 573 knots. See the last page of this section for a derivation of equation [2].
Figure 1. TAS and CAS Relationship with Varying Altitude and Temperature
Figure 2. TAS and CAS Relationship with Varying Altitude and Temperature
(Continued)
Figure 3. Mach Number vs TAS Variation with Altitude
The following is a derivation of equation [2] for the speed of sound:
Given: p = pressure (lb/ft^{2})
T = absolute temperature (°Rankine) = °F + 459.7 v = specific volume
(ft^{3}/lb) w = specific weight (lb/ft^{3}) =
1/ν R = a constant (for air: R = 53.3)
ρ = density = w/g = 1/gν ? ν = 1/gρ
From Boyle's law of gasses: pν = RT , therefore we have: p/ρ = gRT = (32.2)(53.3)T =
1718 T [3]
It can also be shown that: p/ρ^{γ}
= constant; for air γ = 1.4 [4]
From the continuity equation applied
to a sound wave: ρAVa = (ρ+dρ)A(V_{a} + dV_{a})
[5]
Expanding and dropping insignificant terms gives: dV_{a} = V_{a} dρ/ρ [6]
Using Newton's second law (p + ρV_{a}/2
= a constant) and taking derivatives: dp = ρV_{a}dV_{a}
substituting into [6] gives: V_{a}^{2}
= dp/dρ [7] 2 Then taking derivatives of [4] and substituting in [7] gives:
[8]
Then using [3] gives: [9]
Using a "Standard" atmosphere of 59° F @ Sea Level (S.L.)
and a lapse rate of 3.57°/1000 ft altitude:
which is equation [2]
Table of Contents
for Electronics Warfare and Radar Engineering Handbook
Introduction 
Abbreviations  Decibel  Duty
Cycle  Doppler Shift  Radar Horizon / Line
of Sight  Propagation Time / Resolution  Modulation
 Transforms / Wavelets  Antenna Introduction
/ Basics  Polarization  Radiation Patterns 
Frequency / Phase Effects of Antennas 
Antenna Near Field  Radiation Hazards 
Power Density  OneWay Radar Equation / RF Propagation
 TwoWay Radar Equation (Monostatic) 
Alternate TwoWay Radar Equation 
TwoWay Radar Equation (Bistatic) 
Jamming to Signal (J/S) Ratio  Constant Power [Saturated] Jamming
 Support Jamming  Radar Cross Section (RCS) 
Emission Control (EMCON)  RF Atmospheric
Absorption / Ducting  Receiver Sensitivity / Noise 
Receiver Types and Characteristics 
General Radar Display Types 
IFF  Identification  Friend or Foe  Receiver
Tests  Signal Sorting Methods and Direction Finding 
Voltage Standing Wave Ratio (VSWR) / Reflection Coefficient / Return
Loss / Mismatch Loss  Microwave Coaxial Connectors 
Power Dividers/Combiner and Directional Couplers 
Attenuators / Filters / DC Blocks 
Terminations / Dummy Loads  Circulators
and Diplexers  Mixers and Frequency Discriminators 
Detectors  Microwave Measurements 
Microwave Waveguides and Coaxial Cable 
ElectroOptics  Laser Safety 
Mach Number and Airspeed vs. Altitude Mach Number 
EMP/ Aircraft Dimensions  Data Busses  RS232 Interface
 RS422 Balanced Voltage Interface  RS485 Interface 
IEEE488 Interface Bus (HPIB/GPIB)  MILSTD1553 &
1773 Data Bus  This HTML version may be printed but not reproduced on websites.
