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The relationship between elevation and atmospheric oxygen content is not a simple linear one. It's actually exponential with multiple variables. The oxygen concentration as a function of elevation can be calculated from the Barometric formula: P = P0 exp(-M g z / RT) where P0 = sea level Pressure (~1000 hPa), M = mass of 1 mol of air (~0.029 kg mol-1), g = gravity (9.8 ms-2), z = elevation (m), R = gas constant (8.314 J K-1 mol-1) and T = temperature (K). However, for the first 2 km (~6500 ft) above sea level the relationship can be approximated as linear. In this case, at a constant temperature, the rate at which oxygen decreases with elevation is about 10% per km.

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Q: Oxygen content decreases at what rate with increased elevation?
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