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Changing AtmosphereChanging Atmosphere
created by TeachPower.net
Origin of the AtmosphereOrigin of the Atmosphere
• 4.6 billion years ago the earth’s
atmosphere was probably made of
hydrogen and helium.
• Earth’s surface was covered in
volcanoes and lakes of lava.
–Volcanoes release large amounts of CO2,
steam, and N2.
Origin of the Atmosphere CONT’DOrigin of the Atmosphere CONT’D
• CO2 absorbs heat
which warmed the
atmosphere.
• When the volcanic
activity subsided
steam condensed to
form
–Clouds
–Rivers and lakes
Today’s AtmosphereToday’s Atmosphere
• Today the atmosphere mostly consist
of nitrogen and oxygen not hydrogen
and CO2.
SmogSmog
• Because of the Industrial Age our
atmosphere is consistently being filled
with pollutants.
• When these pollutants accumulate in
the upper atmosphere it creates a
layer called smog.
Greenhouse EffectGreenhouse Effect
• CO2 and other gases absorb infrared
radiation that enters from space and
reflects from the ground.
• When this heat is trapped it warms
the atmosphere – Greenhouse Effect.
Ozone DepletionOzone Depletion
• Ozone is the layer of air in the
stratosphere that protects us from UV
radiation.
• This layer is thinning slowly due to
chemicals released into the air by
styrofoam, air conditioners, aerosol
cans called chlorofluorocarbons
(CFC’s).
Earth’s AtmosphereEarth’s Atmosphere
• Layer of air made up of a mixture of gases with some
suspended solids and liquids.
• Other Gases: Argon, CO2, H2O
• Trace Gases: Ne, He, Methane, Kr, Xe, H, O3
• Other types of gases are smog, O3
Atmosphere
Nitrogen
Oxygen
Other Gases
Types of Solids & LiquidsTypes of Solids & Liquids
• Dust, salt, & ice
– How do you think those 3 solids end up in the air?
• Water Vapor
– Water is the only substance that appears in the atmosphere in all
3 states (solid, liquid, and gas)
Structure of the AtmosphereStructure of the Atmosphere
• Troposphere – weather, clouds, and smog occur in this
layer. “Tropos” means “changing” in Greek/Latin. At the
top of the temp. is about –76 ºF.
• Stratosphere – O3 (Ozone) layer keeps harmful levels
of UV radiation from reaching earth’s surface. “Stratos”
means “layer” .
• Mesosphere – meteors burn up in this layer. “Mesos”
means “middle”. Temp. here is about –130 ºF.
• Thermosphere – extends out into space with no
definite outer limit.
Atmosphere (Cont.)Atmosphere (Cont.)
• Ionosphere – lower layer of the Thermosphere. The
sun’s energy tickles little ions and molecules in this layer
causing them to glow which creates the Aurora Borealis
or the “Northern Lights”.
• Exosphere – “Exos” means outer so this layer is the
outermost layer of our atmosphere. Satellites travel in
this region of space.
Air PressureAir Pressure
• Air pressure – is the result of the weight of a column of
air pushing down on an area. The column of air above
your desk to the top of the atmosphere weighs about as
much as a school bus.

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Atmosphere characteristics

  • 2. Origin of the AtmosphereOrigin of the Atmosphere • 4.6 billion years ago the earth’s atmosphere was probably made of hydrogen and helium. • Earth’s surface was covered in volcanoes and lakes of lava. –Volcanoes release large amounts of CO2, steam, and N2.
  • 3. Origin of the Atmosphere CONT’DOrigin of the Atmosphere CONT’D • CO2 absorbs heat which warmed the atmosphere. • When the volcanic activity subsided steam condensed to form –Clouds –Rivers and lakes
  • 4. Today’s AtmosphereToday’s Atmosphere • Today the atmosphere mostly consist of nitrogen and oxygen not hydrogen and CO2.
  • 5. SmogSmog • Because of the Industrial Age our atmosphere is consistently being filled with pollutants. • When these pollutants accumulate in the upper atmosphere it creates a layer called smog.
  • 6. Greenhouse EffectGreenhouse Effect • CO2 and other gases absorb infrared radiation that enters from space and reflects from the ground. • When this heat is trapped it warms the atmosphere – Greenhouse Effect.
  • 7. Ozone DepletionOzone Depletion • Ozone is the layer of air in the stratosphere that protects us from UV radiation. • This layer is thinning slowly due to chemicals released into the air by styrofoam, air conditioners, aerosol cans called chlorofluorocarbons (CFC’s).
  • 8. Earth’s AtmosphereEarth’s Atmosphere • Layer of air made up of a mixture of gases with some suspended solids and liquids. • Other Gases: Argon, CO2, H2O • Trace Gases: Ne, He, Methane, Kr, Xe, H, O3 • Other types of gases are smog, O3 Atmosphere Nitrogen Oxygen Other Gases
  • 9. Types of Solids & LiquidsTypes of Solids & Liquids • Dust, salt, & ice – How do you think those 3 solids end up in the air? • Water Vapor – Water is the only substance that appears in the atmosphere in all 3 states (solid, liquid, and gas)
  • 10. Structure of the AtmosphereStructure of the Atmosphere • Troposphere – weather, clouds, and smog occur in this layer. “Tropos” means “changing” in Greek/Latin. At the top of the temp. is about –76 ºF. • Stratosphere – O3 (Ozone) layer keeps harmful levels of UV radiation from reaching earth’s surface. “Stratos” means “layer” . • Mesosphere – meteors burn up in this layer. “Mesos” means “middle”. Temp. here is about –130 ºF. • Thermosphere – extends out into space with no definite outer limit.
  • 11. Atmosphere (Cont.)Atmosphere (Cont.) • Ionosphere – lower layer of the Thermosphere. The sun’s energy tickles little ions and molecules in this layer causing them to glow which creates the Aurora Borealis or the “Northern Lights”. • Exosphere – “Exos” means outer so this layer is the outermost layer of our atmosphere. Satellites travel in this region of space.
  • 12. Air PressureAir Pressure • Air pressure – is the result of the weight of a column of air pushing down on an area. The column of air above your desk to the top of the atmosphere weighs about as much as a school bus.

Notas do Editor

  1. This PowerPoint lesson and its content is copyright of Craig Warner [cwarner@teachpower.net] TeachPower.net - © TeachPower.net 2005 . All rights reserved. Any redistribution or reproduction of part or all of the contents in any form is prohibited other than the following: You may print or download to a local hard disk extracts for your personal and non-commercial use only. You may copy the content to individual third parties for their personal use, but only if you acknowledge the website (http://teachpower.net) and cwarner@teachpower.net as the source of the material. You may change, add, or delete content for your personal and non-commercial use to fit your school’s curriculum. You may not , except with my express written permission via email , distribute or commercially exploit the content. Nor may you transmit it or store it in any other website or other form of electronic retrieval system.