(aerospace engineering) The airspeed as read from a differential-pressure airspeed indicator which has been corrected for instrument and installation errors; equal to true airspeed for standard sea-level conditions.
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(aerospace engineering) The airspeed as read from a differential-pressure airspeed indicator which has been corrected for instrument and installation errors; equal to true airspeed for standard sea-level conditions.
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Calibrated airspeed (CAS) is the speed shown by a conventional airspeed indicator after correction for instrument error and position error. Most EFIS displays also show CAS. At high speeds and altitudes, calibrated airspeed is further corrected for compressibility errors and becomes equivalent airspeed (EAS).
When flying at sea level under International Standard Atmosphere conditions (15°C, 1013 hPa, 0% humidity) calibrated airspeed is the same as equivalent airspeed and true airspeed (TAS). If there is no wind it is also the same as ground speed (GS). Under any other conditions, CAS may differ from the aircraft's TAS and GS.
Calibrated airspeed in knots is usually abbreviated as KCAS, while indicated airspeed is abbreviated as KIAS.
CAS has two primary applications in aviation:
With the widespread use of GPS and other advanced navigation systems in cockpits, the first application is rapidly decreasing in importance – pilots are able to read groundspeed (and often true airspeed) directly, without calculating calibrated airspeed as an intermediate step. The second application remains critical, however – for example, at the same weight, an aircraft will rotate and climb at approximately the same calibrated airspeed at any elevation, even though the true airspeed and groundspeed may differ significantly. These V speeds are usually given as IAS rather than CAS, so that a pilot can read them directly from the airspeed indicator.
Since the airspeed indicator capsule responds to impact pressure, CAS is defined as a function of impact pressure alone. Static pressure and temperature appear as fixed coeficients defined by convention as standard sea level values. It so happens that the speed of sound is a direct function of temperature, so instead of a standard temperature, we can define a standard speed of sound.
In a spreadsheet CAS can be computed as: ![CAS=a_{sl}\sqrt{5\left[\left(\frac{q_c}{P_{sl}}+1\right)^\frac{2}{7}-1\right]}](http://wpcontent.answers.com/math/2/7/1/2719270f408faf26c0f16ace49e78027.png)
where:
The above is based on the Saint-Venant formula for subsonic airspeeds. For supersonic airspeeds, where a normal shock forms in front of the pitot probe, the Rayleigh formula applies:
![CAS=a_{sl}\left[\left(\frac{q_c}{P_{sl}}+1\right)\times\left(7\left(\frac{CAS}{a_{sl}}\right)^2-1\right)^{2.5} / \left(6^{2.5} \times 1.2^{3.5} \right) \right]^{(1/7)}](http://wpcontent.answers.com/math/0/c/3/0c3bfd9e7f0ed597bf0cbdf5ff631885.png)
The supersonic formula must be solved iteratively, by assuming an initial value for CAS equal to asl.
The formula works in any units, just select the appropriate values for Psl and asl. For example Psl = 1013.25 hPa, asl = 661.48 knots.
This can then be used to calibrate an airspeed indicator when impact pressure (qc) is measured using a water manometer or accurate pressure gauge. If using a water manometer to measure millimeters of water the reference pressure (Psl) may be entered as 10333 mm H20.
At higher altitudes CAS can be corrected for compressibility error to give equivalent airspeed (EAS). In practice compressibility error is negligible below about 10,000 feet and 200 knots.
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
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