Schematic diagram showing that some of the air above the tropopause
forms multimers, while below the tropopause the air is in the normal monomer form.
Not exact matches
This means that when oxygen and / or nitrogen molecules join together to
form larger
multimer molecules, the average amount of latent energy they can store will decrease.
We suggest that most of the ozone in the ozone layer is actually
formed by the splitting up of oxygen
multimers!
So, if
multimers rapidly
form in one part of the atmosphere, the average molar density will rapidly decrease.