Save
geography 🌍
weather hazards ⛈️
Save
Share
Learn
Content
Leaderboard
Learn
Created by
lily 😔
Visit profile
Cards (13)
global
atmospheric
circulation: transfer of
heat
from the
equator
to the
poles
by movement of
air
air moves due to difference in
air pressure
(air moves from
high
pressure areas to
low
pressure areas)
the
global atmospheric
circulation system is divided into
cells
each cell has:
warm
rising air that creates a
low
pressure belt
cool
sinking air that creates a
high
pressure belt
each
hemisphere
has
3
cells
the 3 cell types are
hadley
cell,
ferrel
cell and
polar
cell
hadley cells:
the
sun
warms the earth at the
equator
, causing the air to
rise
and creating a
low
pressure belt
as the air rises it
cools
and moves
away
from the equator
at 30° north or south of the equator, the cool air
sinks
and creates a
high
pressure belt
coriolis
effect: the
curving
of winds due to the earth‘s
rotation
ferrel
cells: at the ground surface, the
cool
air moves either…
back towards the
equator
as
trade winds
or towards the poles as
westerlies
polar cells:
at 60° north or south of the
equator
the
warmer
surface winds meet
colder
air from the
poles
the warmer air
rises
and creates
low
pressure
some of the
air
moves back towards the
equator
and the rest moves towards the
poles
at the poles the
cool
air
sinks
and creates
high
pressure
the
high
pressure air is drawn back towards the
equator
at the equator:
sun
is directly
overhead
, meaning the earth’s surface receives a lot of of
solar
radiation, so it’s
hot
warm
moist
air
rises
and forms
clouds
so it
rains
a lot
at 30°
north
and
south
of the equator:
the air has released most of its
moisture
as
rain
the
dry
air means there are few
clouds
and little
rainfall
deserts
are often found at this
latitude
uk climate:
the uk lies in the
low
pressure zone
60°
north of the
equator
warm
rising air brings lots of
cloud
cover and
rainfall
low
pressure systems are carried from the
atlantic
by
westerly
winds