Question:
An atmospheric temperature inversion happens when warm air
settles in a layer above cold air. When this condition occurs over
cities, it can create a very stable air mass that traps pollution
near the Earth's surface. Why is the air mass in a temperature
inversion so stable?
Replies:
Kay,
"Stable" is the word used to describe the atmospheric
stability when warmer air overlies cooler air (this is
called a temperature inversion). The word inversion is
used because the air temperature generally decreases
with height; but in the case of an inversion, the
temperature gradient (change of temperature with height)
is inverted, or reversed from normal. This typically
The inversion is meta-stable -- it really is not stable. There are a lot
of reasons why/how this can happen. Two common ones are slow moving warm air
that "rides up" of colder air because there is not adequate turbulence for
the two air masses to mix. The other is a result of mountains forming a
'bowl' trapping the cold air near the ground. Here too the lack of air
turbulence is at fault. You can find a detailed description at:
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