Clouds and often precipitation occur on the poleward sides of both warm and stationary fronts and whenever tropical air reaching the latitude of the polar front is forced upward over
the colder air near the surface.
Not exact matches
A low - altitude flow of warm, moist
air from an ocean area combined with a flow of
cold, dry polar
air high up creates maximum instability, which means that parcels of
air heated
near the
surface rise rapidly, creating powerful updrafts.
This means that as the dense
cold air flows towards the low spot and pools there the influence of the large scale wind decreases to zero in a shallow layer
near the
surface.
(1) Most of the warming would actually occur
near the
surface in areas with shallow
cold dry
air masses, such as in Siberia and northern Canada where it would not have a large effect.
Cold - cloud rain occasionally will refreeze if a layer of subfreezing
air exists
near Earth's
surface.
In other words, UHI * is the value of the urban - heat - island effect if wind were not reducing it by replacing warmer
air with
colder; and NSTI * is the effect of the
near -
surface temperature inversion if the wind were not mixing up the
air near the ground with the
air a little higher up.
There is also an increased upwelling of deep
cold ocean waters and more intense uprising of
surface air near South America, resulting in increasing numbers of drought occurrences, although fishermen reap benefits from the more nutrient - filled eastern Pacific waters.
... bodies situated on or
near to the
surface of the earth become, under certain circumstances,
colder than the neighbouring
air, by radiating more heat to the heavens than they receive in every way...