Passage of a Front

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Passage of a Front
The picture on the left hand side of this page shows the passage of a front. The
text on the right hand side of the page describes the different steps involved. Add
the missing words to the text.
Cold Front
Cold fronts occur when a COLDER air
mass replaces a WARMER air mass.
In a cold front the COLD air follows the
warm air and, because COLD air is more
dense, it pushes the WARM air out of
its way, forcing it to rise.
As the warm air rises, it becomes
COOLER and CLOUDS start to form.
Precipitation at cold fronts is usually
heavier although less geographically
extensive (50-70 km) and less
prolonged than rainfall associated
with warm fronts.
The reason for this is that the uplift of
the warm air is stronger due to the
undercutting of cold air, so TOWERING
clouds form, and RAIN,
THUNDERSTORMS, hail and tornados
can occur.
The air behind a cold front is noticeably
COLDER and DRIER than the air ahead
of it.
When the cold front passes through,
temperatures can drop more than 15
DEGREES in the first hour.
Missing words:
15 degrees,
drier,
towering,
colder,
clouds, warmer,
colder,
warm,
rain,
cold,
cold,
cooler,
thunderstorms
Warm Front
Warm fronts occur, when a WARM air
mass approaches a COLD air mass. The
warmer air LIFTS up and over the colder
air.
WARM fronts are usually more gentle
than COLD fronts, they move SLOWLY.
They move gently settling over the cold
front and moving it out of the way.
Precipitation at warm fronts are usually
less heavy although more extensive
(300-400 km), than at the cold fronts.
The AIR behind a warm front is warmer
and moister than the air ahead of it.
Warm fronts bring more STEADY lighter
rain or snow in FRONT of them, which
can last from a few hours to several
days. When a warm front passes
through, the air becomes noticeably
warmer and more HUMID than it was
before.
The first signs of the warm front are the
cirrus clouds.
Missing words:
humid,
slowly,
warm,
steady,
colder,
front,
warmer,
lifts,
air
cold,
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