Frontal Systems
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Transcript Frontal Systems
Frontal Systems
&
High and Low Pressure
Science 10
Frontal Systems
Fronts are created when one air mass
overtakes another
They will typically be classified into two
categories:
– Warm front – when warm air runs into cold air
– Cold front – when cold air runs into warm air
Warm Front
Warm Front
The warm air gradually climbs over the colder air
Typical clouds associated with a warm front are:
–
–
–
–
–
Cirrus
Cirrostratus
Altostratus
Nimbostratus
Stratus
Associated with periods of steady precipitation
May exist over 50-100km
Cold Front
Cold Front
Occurs when warm air is violently pushed
up by advancing cold air
Cumulus clouds are associated with a cold
front
Can result in cumulonimbus clouds
Short periods of heavy precipitation
Covers a small geographical area (2-5km)
Weather Map
High Pressure
High pressure has
“more” air above it
It is pulled down by
gravity
Due to Coriolis Effect,
it spins clockwise and
out in the Northern
Hemisphere
Clear skies
Light winds
Low Pressure
Low pressure has “less” air
above it
Air from a high pressure
flows towards a low
pressure
Due to Coriolis Effect, it
spins counter clockwise
and in in the Northern
Hemisphere
Clouds
Strong winds
High and Low Pressures
Questions Pg. 32 9-12
Pg. 34 13-16
Pg. 32
9. Spherical Earth makes
Sun’s more or less
concentrated.
10. Air Mass- a very large mass of air that has nearly uniform
properties such as temperature, humidity, and pressure.
-arctic (cold, dry)
- continental polar (cool, dry)
- continental tropical (hot, dry)
- maritime polar (cool, humid)
- maritime tropical (hot, humid)
11.
12. Coriolis Effect
Pg. 34
13. Jet streams are fast flowing, narrow air currents found in
the atmosphere, usually between the Troposphere and the
Stratosphere.
14. A Front is a zone that develops as a result of the meeting
of two air masses with different characteristics.
15. A Stationary Front- is when two air masses meet but neither
advances.
16. When cold air replaces warm air we have a Cold Front.
Cold fronts usually bring short periods of heavy precipitation.