where
.
where Rd is the gas constant for dry air (= 287.04
J kg-1 K-1)
where g is the acceleration due to gravity (= 9.801 m s-2)
and is a constant if z is the geopotential height.
the pressure altitude is the altitude in the standard atmosphere at which a given pressure (pstn) will be observed.
For standard atmosphere, the height-pressure relationship is (derivation using hydrostatic equation can be found at http://hurri.kean.edu/~yoh/calculations/standatm/StdAtm.html ),
![]()
For standard atmosphere, the height-density relationship is (derivation
using hydrostatic equation can be found at http://hurri.kean.edu/~yoh/calculations/standatm/StdAtm.html
),
and
the pressure value to which an aircraft altimeter scale is set, so it will indicate the altitude above mean sea level of the aircraft on the ground at the location for which the pressure was determined.
The altimeter setting is the pressure "reduced" to sea level using the temperature profile of the "standard" atmosphere without regard to water vapor.
For standard atmosphere, the height-pressure relationship is (derivation using hydrostatic equation can be found at http://hurri.kean.edu/~yoh/calculations/standatm/StdAtm.html ),
![]()
where po is 1013.25mb and To is 288.15 K.This equation of height-pressure relationship is modified if the aircraft altimeter scale is set at pas (altimeter setting) instead of standard pressure po :
![]()
where Tas is the corresponding temperature reading when the altimeter scale is set at pas. Since altimeter is calibrated according to the standard atmosphere, we also have that Tas and pas must be related by :
![]()
In order to show the height of the plane above the runway, it is important to choose the altimeter setting (pas) such that the altimeter should indicate station/runway elevation (zstn) at observed station pressure (pstn). According to the modified height-pressure relationship,
![]()
Eliminating Tas from the two equations above, we get
![]()
The stations elevation (zstn) usually is about 0.3 m above the official station elevation since there is the typical location of the altimeter of the plane.