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The Atmosphere
• The sun’s energy interacts with
  Earth’s atmosphere and the oceans,
  providing Earth’s climate and
  weather and produce the clouds,
  winds, storms, rains, etc.
The Structure of the
• Troposphere Atmosphere
 –Temperatures
  decrease with
  altitude 16oC 
  -60oC
The Structure of the
• Troposphere Atmosphere
 –The air is warmed by heat
  radiating from Earth’s surface, the
  evaporation of water vapor, and
  water vapor condensing back to
  Earth.
 –Extends from Earth’s surface
  upward 12 km (7 miles) and
  contains 90% of the atmospheric
  gases.
The Structure of the
  Atmosphere (cont’d)
        • Stratosphere
            – The tropopause (the
              dividing line
              between the
              troposphere and
              the stratosphere)
              occurs where the
              temperature no
              longer decreases.
            – Temperatures
              increase with
              altitude -60oC  0oC
The Structure of the
  Atmosphere (cont’d)
         • Stratosphere
           – Contains the ozone
             layer (O3) that
             reduces the amount
             of harmful
             ultraviolet radiation.
           – Extends from 12 km
             to 50 km (7-30
             miles).
           – Contains 9% of the
             atmospheric gases.
The Structure of the
  Atmosphere (cont’d)
        • Mesosphere
          – The stratopause
            (between the
            stratosphere and
            mesosphere) occurs
            where the
            temperature stops
            increasing.
          – The temperature
            decreases with
            altitude 0oC  -90oC
The Structure of the
  Atmosphere (cont’d)
        • Mesosphere
          –There are very few
           gas molecules, so
           the pressure is
           1/1000th of that at
           Earth’s surface.
          –Extends from 50
           km to 90 km (30-
           54 miles).
The Structure of the
         Atmosphere (cont’d)
• Thermosphere
  –The mesopause
   (between the
   mesosphere and
   thermosphere)
   occurs where the
   temperature stops
   going down.
The Structure of the
         Atmosphere (cont’d)
• Thermosphere
  –The
   temperature
   increases with
   altitude -90oC
    unknown
  –This is the site
   of the Aurora
   Borealis
Composition of Air and Air
            Pressure
• Air contains nitrogen
  (78%); Oxygen (21%);
  Argon (1%); Carbon
  Dioxide (0.03%); and
  Neon, Helium, Krypton,
  Xenon, and Hydrogen
  (trace amounts)
• Water vapor and other
  contaminants are not
  included in the
  composition listed above.
Composition of Air and Air
            Pressure
• Air pressure is the force
  with which a column of air
  presses down on Earth’s
  surface.
• The average atmospheric
  pressure on Earth’s surface
  at sea level = 1 atm
  (atmosphere).

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Earth's Atmosphere Layers

  • 1. The Atmosphere • The sun’s energy interacts with Earth’s atmosphere and the oceans, providing Earth’s climate and weather and produce the clouds, winds, storms, rains, etc.
  • 2. The Structure of the • Troposphere Atmosphere –Temperatures decrease with altitude 16oC  -60oC
  • 3. The Structure of the • Troposphere Atmosphere –The air is warmed by heat radiating from Earth’s surface, the evaporation of water vapor, and water vapor condensing back to Earth. –Extends from Earth’s surface upward 12 km (7 miles) and contains 90% of the atmospheric gases.
  • 4. The Structure of the Atmosphere (cont’d) • Stratosphere – The tropopause (the dividing line between the troposphere and the stratosphere) occurs where the temperature no longer decreases. – Temperatures increase with altitude -60oC  0oC
  • 5. The Structure of the Atmosphere (cont’d) • Stratosphere – Contains the ozone layer (O3) that reduces the amount of harmful ultraviolet radiation. – Extends from 12 km to 50 km (7-30 miles). – Contains 9% of the atmospheric gases.
  • 6. The Structure of the Atmosphere (cont’d) • Mesosphere – The stratopause (between the stratosphere and mesosphere) occurs where the temperature stops increasing. – The temperature decreases with altitude 0oC  -90oC
  • 7. The Structure of the Atmosphere (cont’d) • Mesosphere –There are very few gas molecules, so the pressure is 1/1000th of that at Earth’s surface. –Extends from 50 km to 90 km (30- 54 miles).
  • 8. The Structure of the Atmosphere (cont’d) • Thermosphere –The mesopause (between the mesosphere and thermosphere) occurs where the temperature stops going down.
  • 9. The Structure of the Atmosphere (cont’d) • Thermosphere –The temperature increases with altitude -90oC  unknown –This is the site of the Aurora Borealis
  • 10. Composition of Air and Air Pressure • Air contains nitrogen (78%); Oxygen (21%); Argon (1%); Carbon Dioxide (0.03%); and Neon, Helium, Krypton, Xenon, and Hydrogen (trace amounts) • Water vapor and other contaminants are not included in the composition listed above.
  • 11. Composition of Air and Air Pressure • Air pressure is the force with which a column of air presses down on Earth’s surface. • The average atmospheric pressure on Earth’s surface at sea level = 1 atm (atmosphere).