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GEOGRAPHY
Extreme Weather
Global atmospheric circulation
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Created by
Charlotte hansmeyer
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Winds
are large scale movements of air caused by differences in
air pressure
winds are a part of
cells
, which are loops that have warm
rising
air and cool
falling
air
warm air —>
rises
—>
low
pressure (on earth)
cool air —>
falls
—>
high
pressure (on earth)
the sun heats the world
unevenly.
the equator and low
latitudes
get more heat, whereas the
poles
get less heat
this drives global
atmospheric
circulation
Hadley cells (around the
equator
)
the sun warms the earth and this is transferred to the air above
Warm air —>
rises
—> low pressure
Creates
clouds
which condense
Rain is associated with
low
pressure
Lots of
rain
along the equator (rainforests)
Ferrel cells (
30-60
degrees N/S)
at 30 degrees the air cools and sinks, creating
high
pressure. here there are clear skies and
desert
climates
the air sinks and either moves back to the
equator
or towards the
poles
at 60 degrees there is
low
pressure as warm air from the ferrel cell and cool air from polar cell
mixes
lots of
rain
here
polar cells (
60-90
N/S)
at the poles cold air sinks, creating
high pressure
(clear skies, cool air)
cold air sinks and moves
away
from poles
from the equator: pressure is
low (equator)
high (
30 degrees
= deserts)
low (
90 degrees
=
uk
)
high (
poles
)
Wind
Wind is air moving from areas of high to low
pressure,
which means that
atmospheric circulation
causes winds
this makes some parts of the world
windier
Winds are weak in low
pressure belts
Winds are strong
between
pressure belts
precipitation
Precipitation occurs when warm, wet air rises and
cools
, which causes the water vapour to condense
air rises in
low
pressure belts, so precipitation is often and
intense
in these areas
Rainforests are usually in
low
pressure belts
High
pressure belts is where air sinks and precipitation is
low,
like deserts
temperature
the
equator
receives the most energy from the
sun
, whereas the
poles
receive the least