sophiecentaur
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That's a familiar phenomenon that you can see with bonfire smoke and, indeed it's similar with cumulus clouds over warm ground. I'm not too sure how it relates to the humidity / temperature distribution, though. It tells you when the extra thermal energy of the smoke runs out as it gains gpe. Would the smoke stop at the interface between dry and damp air?256bits said:Is this anything like smoking a cigarette and watching smoke rise and roil, until it stabilizes ( in altitude ) somewhere above.
Heat rises the smoke at the beginning and then it spreads out.
Perhaps the guy could have a smoke box set above his chest(at the chest temperature) , release some smoke and see what happens. An instant visual.
Some effects as in post 9 from @Lnewqban might come into play.
I think the OP's question is actually a big one and needs to be 'trimmed' if we want an actual answer. Is the air near the ceiling always warmer and / or is it always damper? In a black metal vertical column (equal temperature all the way up), could we measure a humidity difference as we go up?
The walls would maintain a 'zero' temperature gradient so there would be a steady change in the mixture of molecules on the way up, depending on density.
remember that most of our experiences involve a heat source somewhere and a heat sink. How much and where are very important factors.DaveC426913 said:Hot air will generally rise to the ceiling.
Moisture will generally diffuse throughout the room.
Diffusion will be affected by molecular mass, too.