The global atmospheric circulation system transports heat around the Earth's atmosphere and affects climate and weather patterns. It involves warm air rising at the equator and cold air sinking at the poles, creating circulation cells. Without this system, temperatures would become more extreme between the tropics and poles.
The global transportation
systemof heat in the
atmosphere is one of the
Earth’s most critical systems.
Without this system the
tropics would continue to get
hotter and the poles would
continue to get colder. It’s
also responsible for climate
and weather patterns.
LO: To understand how global atmospheric circulation
effects global weather and climate.
All key words
MUST be
highlighted or
underlined.
08 November 2018
2.
You canYou can describe how global atmospheric circulation effects
global weather and climate.
You use a limited range of specialist terms
You have a reasonable accuracy in the use of spelling, punctuation
and grammar.
You can outline how global atmospheric circulation effects global
weather and climate.
You use a good range of specialist terms
You have a considerable accuracy in spelling, punctuation and grammar.
You can explain how global atmospheric circulation effects global
weather and climate.
You use a wide range of specialist terms where appropriate.
Accurate use of spelling, punctuation and grammar.
L3 - Detailed
Answer
L2 - Clear
Answer
L1 - Basic
Answer
Learning Outcomes – Success Criteria
LO: To understand how global atmospheric circulation effects global weather and
climate.
3.
The sun heatsup air in the
earth’s atmosphere. The
temperature of the earth’s
atmosphere depends on latitude
(how far away you are from the
equator). As the suns energy is
more concentrated at the
equator, the air here is warm and
the air at the North & South
Pole is cold.
LO: To understand how global atmospheric circulation effects global weather and
climate.
4.
The most important
influenceon worldwide
variations in climate is
latitude. Because the
curved surface of the
Earth, the equator
receives much higher
insolation than the
polar latitudes.
LO: To understand how global atmospheric circulation effects global weather and
climate.
5.
In areas ofhigh insolation
the air is heated and it
becomes less dense and rises
to higher altitude. This
creates a global climate zone
of low pressure.
In areas with low insolation,
there is cold dense air that
sinks and creates an area of
high pressure.
LO: To understand how global atmospheric circulation effects global weather and
climate.
6.
LO: To understandhow global atmospheric circulation effects global weather and
climate.
7.
LO: To understandhow global atmospheric circulation effects global weather and
climate.
8.
The 3 Cell
Model
Showsthe
redistribution
of energy
from areas of
surplus to
areas of
deficit. This
helps keep
the global
energy
balance
LO: To understand how global atmospheric circulation effects global weather and
climate.
9.
Items you willneed:
• Scissors
• Red, light blue, dark blue
& green colouring pencils.
• Glue stick
• Highlighters
• Pen
Over the major parts of the Earth's
surface there are large-scale wind
circulations present. The global
circulation can be described as the
world-wide system of winds by which
the transport of heat from tropical to
polar latitudes is accomplished.
LO: To understand how global atmospheric circulation effects global weather and
climate.
10.
Step One
Carefully cutaround the
different model parts.
LO: To understand how global atmospheric circulation effects global weather and
climate.
11.
Step Two
Lightly foldthe model in
half to cut the semi-
circular dotted line.
LO: To understand how global atmospheric circulation effects global weather and
climate.
12.
Step Three
Fold thesemi-circular
arch up over the
‘Earth’ and glue the
model’s based into
your exercise book.
LO: To understand how global atmospheric circulation effects global weather and
climate.
13.
Step Three
Next, gluetogether
the ‘fingers’ of the
smaller section
onto the main
section of your GCS
model.
LO: To understand how global atmospheric circulation effects global weather and
climate.
14.
Step Four
Once youhave
glued the two
sections together,
trim the parts that
are sticking out
from the arch.
LO: To understand how global atmospheric circulation effects global weather and
climate.
15.
Step Five
Using agreen
(land) and blue
(ocean) crayon,
colour the Earth.
Be quick! Don’t take
too long!
LO: To understand how global atmospheric circulation effects global weather and
climate.
16.
You will nowneed to
include a key next to your
diagram!
Step Six
Now shade the arrows
shown red. These are
representing the
movement of warm
air (low pressure).
LO: To understand how global atmospheric circulation effects global weather and
climate.
17.
Step Seven
Next, shadedark
blue the arrows
shown that represent
the movement of
cold dry air (high
pressure) on your
model.
Don’t forget to add this
to your key!
LO: To understand how global atmospheric circulation effects global weather and
climate.
18.
Step Eight
Now labelthe following
lines of latitude.
Arctic Circle
Tropic of Cancer
Equator
Tropic of Capricorn
Antarctic Circle
LO: To understand how global atmospheric circulation effects global weather and
climate.
19.
Step Nine
Now youwill need
label the different
cells of your model.
You could use a
highlighter to make
these labels stand out.
Polar Cell
Ferrel Cell
Hadley Cell
Ferrel Cell
Polar Cell
LO: To understand how global atmospheric circulation effects global weather and
climate.
20.
Step Eleven
Draw aline with a Yellow
pen or highlighter to
represent the sun’s rays. As
shown, have one ray
leading to the Equator and
another to the Antarctic
Circle.
Once completed, label the
two rays.
Equatorial Insolation
Polar Insolation
LO: To understand how global atmospheric circulation effects global weather and
climate.
21.
1
2
3
4 5
6
Step Thirteen
Nowadd the following
numbers around the
outside of your model.
These will represent the
different parts of your
GCS model.
LO: To understand how global atmospheric circulation effects global weather and
climate.
22.
1. Air coolsand sinks, creating a belt of high pressure and a cold, dry climate.
2. At about 60°N and S, cold polar air mixes with warmer air and rises,
creating a belt of low pressure.
3. Cool air sinks, creating a belt of high pressure. As the sinks it becomes
warmer and drier.
4. Warm air rises, creating a belt of low pressure. As the air rises, it cools.
Clouds form and then release precipitation. Above, the air will eventually
separate and move to higher latitudes.
5. Sun’s heat is concentrated.
6. Sun’s heat is spread out.
Step Fourteen
Write the following information below your model to represent each stage of the GAC.
You could use a highlighter for
key points/terms.
LO: To understand how global atmospheric circulation effects global weather and
climate.