

Energy Transfer in the Atmosphere
Presentation
•
Science
•
9th - 12th Grade
•
Hard
Joseph Anderson
FREE Resource
17 Slides • 10 Questions
1
Energy in the
Atmosphere
Notes Part 2
2
Energy in the Atmosphere
*Remember*
● Conduction - energy transfer by contact
○ Ex: Burning your hand when you touch a
hot pan
● Convection - energy transfer by circulation
or movement of a liquid or gas by
convection currents
○ Ex: warm air rising, cooler air sinking
3
The Greenhouse Effect -
A good thing!
● Without the greenhouse
effect, the life would
probably not exist, because
it helps warm the Earth!
○
Average temperature
without greenhouse
effect = -18℃ or -0.4℉
○
Average temperature
WITH the greenhouse
effect = 15℃ or 59℉
4
Human Causes Global Warming
● The more greenhouse
gases in the atmosphere,
the more heat that is
trapped which makes the Earth warmer
○ Called global warming
● Scientists think that our
activities are increasing the
natural greenhouse effect
5
Fill in the Blanks
6
Global Warming
Effects
●
The effects of global warming
○
Warmer summers and
winters
○
Some places will be
wetter or drier, affecting
farming
○
Melting ice caps, which
raise sea levels
○
Life would have to adapt
to the changes
7
Long-term
fluctuations in
weather patterns
could have
extreme impacts
on farmers,
slashing crop
yields, forcing
farmers to adopt
new practices to
adapt to the new
conditions.
8
Multiple Choice
Which is NOT an effect of increased global warming?
changes in global food production
increase in extreme weather events
9
The Debate
●
Over the last 4 billion years,
climates on the Earth have
constantly changed
●
As we are coming out of an
ice age, is this warming trend
natural, or man-made?
●
Your job as citizens is to
research, learn, and find the
truth! Learn all you can so you
can make an informed
decision!
10
No Greenhouse Effect
11
Radiation Balance
● The Radiation
Balance: Energy in,
Energy Out
○ The amount of
energy Earth
receives and the
amount of energy
returned to space
must be
approximately
equal.
12
Fill in the Blanks
13
Why Air Moves
● Density Differences
○ Air Rises at the Equator and sinks at the Poles
○ As the cold, more dense air sinks, it creates
areas of high pressure around the poles. This
cold polar air then flows toward the equator,
where the warm air creates low pressure
● Pressure always goes from high to low. The high
pressure air wants to fill in the low-pressure area.
● Pressure Belts are found every 30°
○ Convection cells are separated by pressure
belts, band of high and low pressure
14
Dropdown
15
Fill in the Blanks
16
Fill in the Blanks
17
18
—Someone Famous
19
The Coriolis Effect
● The Coriolis
Effect - the
apparent
curving of
the path of
the currents
due to the
Earth’s
rotation
● Simulation
20
Multiple Choice
the apparent curving of the path of the currents due to the Earth’s rotation
Convection Current
21
22
Local Winds
● Move short distances
and can blow from
any direction
○ Ex. Mountain and
valley breezes are
due by geography
○ Sea and land
breezes are
affected by
temperature
23
Multiple Choice
Local winds are ______ distance.
24
Multiple Choice
Local winds blow
left to right
in any direction
right to left
north to south
25
Sea/Land Breezes
●
26
The Ozone Hole
● The Earth's protective ozone layer is thinning over the
Arctic regions.
○ This allows more UV radiation, which damages
genes and can cause skin cancer, to reach the surface
● In 1987, many nations agreed to reduce the use of
CFCs, the chemicals that cause ozone depletion
○ CFCs remain active for 60-120 years, but it takes
MUCH longer to repair the ozone layer
Simulation
27
Multiple Choice
One negative effect of the hole in the ozone layer is
Energy in the
Atmosphere
Notes Part 2
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