Chapter 3: The Earth`s Atmosphere and Climates
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Transcript Chapter 3: The Earth`s Atmosphere and Climates
Geography PowerPoint on
Earth’s Systems and Climates
Age Range: High School
Educational Goals:
• Basic understanding of Greenhouse Effects
• Understand the relationship between solar energy and air
pressure
• Understand the importance of satellites
• Understanding of different climate zones around the world
Abstract
The information for this PowerPoint was taken from an AGS
World Geography text book. The information provided in the
book was difficult to understand and was not visually
stimulating for students. I pulled important facts and details
then added visuals. The PowerPoint also includes a hyperlink
to help explain the Greenhouse Effect. This can be manipulated
together as a class or individually. Upon completion, students
can individually take a quiz provided on that link. The slides
can also be used to help prepare students for the test. The
information can be removed thus leaving only the visuals. This
is especially helpful when describing different climate zones.
By creating this PowerPoint, students are still able to use the
text to answer section questions and they feel less overwhelmed
by the information presented.
Chapter 3: The Earth’s
Atmosphere and Climates
Global Energy Systems
Temperature is the measurement of heat in the
atmosphere.
Everyday the sun’s rays reach the earth.
Some rays are reflected back to space.
Some are absorbed and changed into heat energy.
http://www.epa.gov/globalwarming/kids/global_
warming_version2.html
The Greenhouse Effect
A greenhouse is
a special house
built to grow
plants.
The earth traps
energy the same
way.
Who receives solar
energy?
All of the earth receives solar energy.
The equator receives more solar energy
than the North and South poles.
Heat energy is shared through:
winds
ocean currents
Air Pressure
Air pressure creates the winds and ocean
currents that allows energy to be shared.
Low pressure
air is warmed, expands, becomes lighter,
rises
brings unstable weather
Air Pressure
High pressurecold air
• dense (heavy)
• mostly clear, dry weather
Air pressure zones 1. Equator low pressure 2. Subpolar low pressure
3. Subtropical high pressure 4. Polar high pressure
Air Pressure Zones
1. Equator low
pressure
2. Subpolar low
pressure
3. Subtropical high
pressure
4. Polar high
pressure
Satellites
They collect and send back information
about the earth.
2 types of light
visible light
infrared light - detects heat in clouds,
water, and land
Satellite Images
Satellite Importance
Tracking weather
clouds, storms, oceans
Environment
changes in vegetation (plants)
moisture
visible and infrared light
land surface
air pollution
pests (bugs)
monitor human activity (growth of cities)
burning of rainforests
forest fires
crop (farm) damage
paths of oil spills
animal movement
ground movement of earthquakes
World Climate Zones
Classifying Regions
Low Latitudes
humid tropical
tropical savanna
Dry/Semiarid
desert
steppe
Middle Latitudes
Mediterranean
humid subtropical
Middle Latitude
marine west coast
humid continental
High Latitude
subarctic
tundra
ice cap
Highland
Low Latitudes
Humid Tropical
along equator
South America
Zaire Basin Africa
Southeast Asia
weather patterns
warm and rainy year
round
Vegetation
tropical rainforest
Low Latitudes
Tropical Savanna
between humid
tropics and deserts
Africa
South America
Central America
Southern and
Southeast Asia
Australia
Weather
warm all year
rainy and dry seasons
Vegetation
tropical grassland with
few trees
Dry / Semiarid
Desert
Saharan Africa
southwest Asia
central and western
Australia
southwestern North
America
Weather
Arid (low rainfall)
tropics
- sunny and hot
middle latitudes
huge temperature
range
Steppe -
Dry / Semiarid
bordering deserts
northern and south
Africa
interior western North
America
central and interior
Asia and Australia
southern South
America
Weather
semiarid - a little rain
hot summers
cool winters
similar to desert temp
Vegetation grassland, few trees
Middle Latitudes
Mediterranean
middle latitudes, west
coast
southern Europe
southwest Asia
California
southwestern Australia
central Chile
southwestern South Africa
Weather
dry, sunny warm summers
mild, humid winters
Vegetation
scrub, woodland,
grassland
Middle Latitudes
Humid Subtropical
east coasts in middle
latitudes
southeastern United States
eastern Asia
central southern Europe
southeastern parts of
South Africa and Australia
Weather
hot, humid summers
mild, humid winters
in path of hurricanes and
typhoons
Vegetation
mixed forest
Middle Latitudes
Marine West Coast
upper-middle latitudes,
west coast
Europe and North America
North America
southwestern South
America
Weather
cloudy, mild summers
cool, rainy winters
strong ocean influence
Vegetation
temperate, evergreen
forest
Middle Latitudes
Humid Continental
east coasts and upper
middle latitudes
northeastern North
America
northern and eastern
Europe
northeastern Asia
Weather
4 seasons
long, cold winters
short, warm summers
rain varies
Vegetation
mixed forest
High Latitudes
Subarctic
high latitude of
interior and east
coasts
northern North
America, Europe, and
Asia
Weather
extreme temperatures
• long cold winters
• short warm summers
• very little rain
Vegetation
northern evergreen
forest
High Latitude
Tundra
high latitude coasts
northern parts of North
America, Europe, Asia
Antarctica
subantarctica islands
Weather
cold all year
• long cold winters
• short cool summers
• little rain
Vegetation
moss, lichens, low
shrubs, permafrost bogs
in summer
High Latitude
Ice Cap
polar regions
Antarctica
Greenland
Arctic Basin Islands
Weather
freezing cold
• snow ice all year
• little rain
• temperature is not
higher than freezing
Highland
High mountain
regions
western North and
South America
eastern Asia and
Africa
southern and central
Europe and Asia
Weather
determined by
elevation
higher - cooler
lower - similar to
surroundings
Summary
What did we learn?
Global Energy
Greenhouse Effect
solar energy
air pressure
Satellites
World climate zones
Review
Which statements is true?
We learned there is not a real importance in
understanding climates.
We learned that many factors play a role in
influencing climates such as;
–
–
–
–
–
–
ocean currents
wind
elevation
people
Earth’s surface
sun
We learned global warming is not an important
issue.