Pressure altitude
Pressure altitude within the atmosphere is the altitude in the International Standard Atmosphere (ISA) with the same atmospheric pressure as that of the part of the atmosphere in question.
The National Oceanic and Atmospheric Administration (NOAA) has published the following formula[1] for directly converting atmospheric pressure in millibars (mb{displaystyle mathrm {mb} }) to pressure altitude in feet (ft{displaystyle mathrm {ft} }
):
- 145366.45[1−(Station pressure in millibars1013.25)0.190284].{displaystyle 145366.45left[1-left({frac {text{Station pressure in millibars}}{1013.25}}right)^{0.190284}right].}
In aviation, the pressure altitude is the indicated altitude obtained when an altimeter is set to an agreed baseline pressure under certain circumstances in which the aircraft’s altimeter would be unable to give a useful readout of the altitude. Examples would be landing at a very high altitude or near sea level under conditions of exceptionally high air pressure. Old altimeters were typically limited to displaying the altitude when set between 950 mb{displaystyle 950~mathrm {mb} } and 1030 mb{displaystyle 1030~mathrm {mb} }
. Standard pressure, the baseline used universally, is 1013.25{displaystyle 1013.25}
hectopascals (hPa{displaystyle mathrm {hPa} }
), which is equivalent to 1013.25 mb{displaystyle 1013.25~mathrm {mb} }
or 29.92{displaystyle 29.92}
inches of mercury (inHg{displaystyle mathrm {inHg} }
). This setting is equivalent to the atmospheric pressure at mean sea level (MSL) in the ISA. Pressure altitude is primarily used in aircraft-performance calculations and in high-altitude flight (i.e., above the transition altitude).
- QNE
QNE is an aeronautical code Q code. The term QNE refers to the indicated altitude at the landing runway threshold when 1013.25 mb{displaystyle 1013.25~mathrm {mb} }or 29.92 inHg{displaystyle 29.92~mathrm {inHg} }
is set in the altimeter’s Kollsman window. In other words, it is the pressure altitude at the landing runway threshold.
Most aviation texts for PPL and CPL exams describe a process for finding the pressure altitude (in feet) using the following formula:
- Pressure altitude (PA)=Elevation+1000×(29.92−Altimeter setting).{displaystyle {text{Pressure altitude (PA)}}={text{Elevation}}+1000times (29.92-{text{Altimeter setting}}).}
For example, if the airfield elevation is 500 ft{displaystyle 500~mathrm {ft} } and the altimeter setting is 29.32 inHg{displaystyle 29.32~mathrm {inHg} }
, then
- PA=500+1000×(29.92−29.32)=500+1000×0.6=500+600=1100.{displaystyle {begin{aligned}{text{PA}}&=500+1000times (29.92-29.32)\&=500+1000times 0.6\&=500+600\&=1100.end{aligned}}}
Alternatively,
- Pressure altitude (PA)=Elevation+30×(1013−QNH).{displaystyle {text{Pressure altitude (PA)}}={text{Elevation}}+30times (1013-{text{QNH}}).}
For example, if the airfield elevation is 500 ft{displaystyle 500~mathrm {ft} } and the QNH is 993 mb{displaystyle 993~mathrm {mb} }
, then
- PA=500+30×(1013−993)=500+30×20=500+600=1100.{displaystyle {begin{aligned}{text{PA}}&=500+30times (1013-993)\&=500+30times 20\&=500+600\&=1100.end{aligned}}}
Aircraft Mode “C” transponders report the pressure altitude to air traffic control; corrections for atmospheric pressure variations are applied by the recipient of the data.
The relationship between static pressure and pressure altitude is defined in terms of properties of the ISA.
See also
- QNH
- Flight level
- Density altitude
- Standard conditions for temperature and pressure
- Barometric formula
References
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External links
Newbyte Atmospheric Calculator, Android Version
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