I'm hoping that someone may be able to explain the relationship between
Temperature inversion, dew point/cloud production and High Pressure (and
it's effect on cloud). High pressure (and its associated stability) is a
cloud killer, but why when all a parcel of air has to do is rise and
condense? Where is the lower layer of an inversion in relation to cloud
production or condensation? Above cloud base? I've seen various diagrams
in relation to temperature inversion and they're pretty vague about where
the inversion is in relation to cloud.

Dave
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