eotfofylgg

eotfofylgg t1_jclfjlr wrote

The atmosphere is full of wind, which keeps things pretty well mixed, at least in the troposphere.

In a hypothetical perfectly still atmosphere, the heavier molecules would tend to settle to the bottom. Even then, the air wouldn't be perfectly stratified like a layer cake, because there is enough thermal energy to mix the layers. But you would observe that, as the elevation increased, the concentration of heavier molecules dropped off faster than the concentration of lighter molecules.

1