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→Simplified model
\[p= p_{ground} -\rho_{air} g H\]
Where \(p_{ground}\) is the static pressure on the ground. This simple formula allows us to relate the decrease in static pressure to the altitude we are at, if we know the density of air and the gravitational acceleration (which we do). If we note down the ground pressure and continuously monitor the static pressure as we fly, it is possible to work out the altitude of the aeroplane. This is the fundamental principle of an altimeter.
=== Compressible effects ===