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 The side of the front which has the
'humps' or 'triangles' indicates the direction in which
the front is moving.
Warm front
Ahead of the warm front is a belt of thickening
cloud, gradually developing into moderate rain and
cloud. The belt of rain extends 100-200 miles ahead of
the front. Behind the front the rain usually becomes
lighter, or ceases, but the weather remains cloudy. The
warm front does not necessarily bring higher
temperatures. This is particularly so in summer, when
the cloudy weather behind the front cuts off the heat
from the sun. In winter, however, the south-westerly
winds that usually blow after a warm front has moved
through bring milder conditions. The advance of a warm
front is usually the way in which a cold winter spell is
broken down. Ahead of a warm front pressure falls
steadily, and sometimes very rapidly. After the passage
of the front the barometer usually steadies, or falls
less rapidly.
Cold front
This usually brings a narrower belt of cloud and
rain. It is called a cold front because the moist
south-westerly winds ahead of it are replaced by cooler,
drier north-westerly winds. When a cold front moves
through an area it usually brings brighter, clearer
weather behind it, but this brighter weather is
sometimes mixed with showers. Pressure falls ahead of
the cold front, but usually rises after its passage and
the veer of the wind.
Occluded front or occlusion
The characteristics of an occlusion are similar to
those of a cold front in that the rain belt is narrow,
and the winds generally veer to the north-west behind
it. There is usually a clearance to the west after the
front has moved through.
Sometimes fronts do not bring much in the way of rain
or cloud, and are then known as 'weak'. Thunderstorms
can occur with all three types of front, but are most
likely to accompany a cold front. However, many
thunderstorms are not linked with frontal activity.
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