INVERSION

INVERSION

Because of the fire (Phoenix): INVERSION
Usually, within the lower atmosphere (the troposphere) the air near the surface of the Earth is warmer than the air above it, largely because the atmosphere is heated from below as solar radiation warms the earth’s surface, which in turn then warms the layer of the atmosphere directly above it.
Consequences of a thermal inversion
With the ceasing of convection, which is normally present in the atmosphere, a number of phenomena are associated with a temperature inversion. The air becomes stiller, hence the air becomes murky because dust and pollutants are no longer lifted from the surface.

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