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global atmospheric circulation
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Global atmospheric circulation
Interconnected
circular
air
cells
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Global atmospheric circulation
Involves
high
pressure,
rising
warm
air,
surface
winds moving from
high
to
low
pressure, transferring
heat
and
moisture
Winds
curve
due to Earth's
rotation
and change
seasonally
due to
tilt
and
rotation
of Earth
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Global atmospheric circulation
1. Surface
winds
move from
high
to
low
pressure
2. Transferring
heat
and
moisture
from one area to another
3. Winds
curve
due to Earth's
rotation
4. Change
seasonally
due to
tilt
and
rotation
of Earth
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Atmosphere becomes
thin
at
higher
altitudes
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Jet
streams occur at
high altitudes
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Thunderstorms occur at
high altitudes
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Hadley
cells,
polar
cells, and
Ferrel
cells are part of global atmospheric circulation
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Tropical
storms called hurricanes and
typhoons
form south of the equator
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Global atmospheric circulation
Drives the world's
weather
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UK weather
Cloudy
and
wet
because
cold polar air
meets warm
subtropical
air. the surface winds bring
warm
and
wet
weather as rising air
cools
and
condenses
forming
clouds
and
rain
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Desert weather
Hot and dry because of
sinking
air and
high
pressure meaning little rain, hot day and very cold nights
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Equatorial weather
Hot and sweaty because of
low
pressure and
rising
air.
hot
and
humid
air rises,
cools
and
condenses,
causing
heavy
rain
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Tropical
rainforests are found where the sun is directly
overhead
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