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The Barometric Formula,sometimes called the exponential atmosphere, is a formula used to model how the pressure (or density) of the air changes with altitude. It is based on the simplifying (not very realistic) assumption that the temperature does not depend on altitude. However, this formula agrees reasonably well with the actual pressure and density variations above the earth's surface up to a height of about 450,000 ft.
or
where h is the scale height, ρ (rho) is density, P is pressure, M = 0.029 kg (the mass of 1 mole of air), R = 8.314 J K-1 mol-1 is the molar gas constant, T is temperature, is gravity and z is the vertical height above the earth's surface.
I.e., going up the pressure decreases roughly 1% every 80 metre.
Exponentials
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