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Global Atmosphere Circulation
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Definition of Global Atmosphere Circulation
Global atmospheric circulation is a worldwide system of
winds.
This transports
heat
from
tropical
to
polar
latitudes.
In each hemisphere, air circulates in
cells.
When hot air rises, driven by the equator?
Low
pressure
Draws moisture from the ground
Creating
clouds
, rain and storms
When cool air sinks?
High
pressure
Brings
fine
weather
How is wind caused?
Air moves from
high
atmospheric pressure to
low
atmospheric pressure
Three cells in each hemisphere?
Hadley
Cell
Ferrel
Cell
Polar
cell
Describe function of Hadley Cell : Low pressure belt
Heat
of the sun concentrated at the
equator
causes air to
rise.
Forms a
low
pressure belt.
Huge
rain clouds
formed.
Ecosystems
like
tropical
rainforests form here.
Describe function of Hadley cell : High pressure belt
Cool air
sinks
, towards the earth at
30
degrees.
This creates a
high
pressure belt.
This causes
low
rainfall so
deserts
form here.
What are Trade Winds?
Surface winds
blowing towards the
equator
Function of polar cell
At the poles, air
sinks
due to
low
temperature.
This air will then move towards the
equator
at a low level.
Approx.
60
degrees, this air will meet
warmer
air, and move towards the poles.
The air will
rise upward
until it reaches the top of the atmosphere. The air moves in
two
directions.
Some air goes back to the poles as surface winds are forming the
polar
cell.
Function of ferrel cell
Some air from the
Polar
cell moves back to the equator meeting the
Hadley
cell
This forms the middle cell called the
Ferrel
cell.
Global Distribution of Tropical Storms : Typhoons
South
China
Sea and west Pacific Ocean
Global Distribution of Tropical Storms : Hurricanes
Gulf of Mexico,
Caribbean
Sea and west coast of Mexico
Global Distribution of Tropical Storms : Cyclones
Bay of Bengal,
Indian
Ocean and northern Australia
Where do Tropical Storms form?
They develop over the
warm
tropical oceans between
5°
and
30°
north and south of the
equator.