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Ryan Beaudry Introduction to the Structure and Composition of Earths Atmosphere
Terms Atmosphere-The gases, droplets, and particles surrounding Earth’s surface. Weather-Day to Day conditions of the atmosphere. Climate-The statistical properties of the atmosphere, including measures of average conditions, variability, etc. Climatology-The study of long term atmospheric conditions.
CRAZY FACT -The total mass of the atmosphere is equivelant to 5.65 billion million tons.                            “Understanding Weather and Climate”, Fifth Edition, Aguado and Burt, page 5
Vertical Structure Troposphere-Lowest layer of the atmosphere.  Where almost all weather takes place. Decreasing temperatures. Depth= 8 to 16km(3.6 to 10 miles). Stratosphere-Second lowest layer of atmosphere. Very little weather occurs. Increasing temperatures. Depth=Approx. 20km(12 miles).
Vertical Structure CONT. Mesosphere- Third layer in the atmosphere.  Decreasing temperatures. Depth=Approx. 80km(50 miles). Thermosphere- Outermost layer of atmosphere. Increasing temperatures. Depth=Begins at 80km
ADDITIONS Tropopause-Transition zone where the temperature ceases to decrease. Stratopause-Top of stratosphere, temperatures continue to increase.
ADDITIONS CONT. Ozone Layer-Within the stratosphere where the gas, ozone, is abundant. Mesopause-Very top of the mesosphere, continuing into the thermosphere. Ionosphere-Extends from the upper mesopshere into the thermosphere.
http://burro.cwru.edu/Academics/Astr201/Atmosphere/structure.jpg
COMPOSITION OF ATMOSPHERE
Made up of:        -Mixture of invisible gases       -Large number of suspended microscopic        particles and water droplets.
Relevant Terms Homosphere-The lowest 80km of the atmosphere, which the relative abundance of the permanent gases is constant. Heterosphere-The high atmosphere where gases are not well mixed but rather are stratified according to weight.  Where lighter weighing gases are found.
Gases Making Up Atmosphere Permanent Gases-Those gases whose relative abundance is constant within the homosphere. Variable Gases-Gases present in amounts that vary greatly in abundance, either vertically, horizontal, or seasonal.  Water vapor is the most important variable gas.
http://geogrify.net/GEO1/Images/FOPG/03T2.jpg
RESOURCES    Information from the book: Aguado: Understanding Weather and Climate, Fifth Edition                    Copyright © 2010 Pearson Education, Inc. Pictures on Page 1- planetgreen.discovery.com(left), windows2universe.org(right) Atmosphere Structure picture- http://burro.cwru.edu/Academics/Astr201/Atmosphere/structure.jpg Composition chart- http://geogrify.net/GEO1/Images/FOPG/03T2.jpg Slide 10 Picture -http://www.examiner.com/images/blog/replicate/EXID47225/images/causes02.jpg
      The End

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Structure and Composition of the Atmosphere

  • 1. Ryan Beaudry Introduction to the Structure and Composition of Earths Atmosphere
  • 2. Terms Atmosphere-The gases, droplets, and particles surrounding Earth’s surface. Weather-Day to Day conditions of the atmosphere. Climate-The statistical properties of the atmosphere, including measures of average conditions, variability, etc. Climatology-The study of long term atmospheric conditions.
  • 3. CRAZY FACT -The total mass of the atmosphere is equivelant to 5.65 billion million tons. “Understanding Weather and Climate”, Fifth Edition, Aguado and Burt, page 5
  • 4. Vertical Structure Troposphere-Lowest layer of the atmosphere. Where almost all weather takes place. Decreasing temperatures. Depth= 8 to 16km(3.6 to 10 miles). Stratosphere-Second lowest layer of atmosphere. Very little weather occurs. Increasing temperatures. Depth=Approx. 20km(12 miles).
  • 5. Vertical Structure CONT. Mesosphere- Third layer in the atmosphere. Decreasing temperatures. Depth=Approx. 80km(50 miles). Thermosphere- Outermost layer of atmosphere. Increasing temperatures. Depth=Begins at 80km
  • 6. ADDITIONS Tropopause-Transition zone where the temperature ceases to decrease. Stratopause-Top of stratosphere, temperatures continue to increase.
  • 7. ADDITIONS CONT. Ozone Layer-Within the stratosphere where the gas, ozone, is abundant. Mesopause-Very top of the mesosphere, continuing into the thermosphere. Ionosphere-Extends from the upper mesopshere into the thermosphere.
  • 10. Made up of: -Mixture of invisible gases -Large number of suspended microscopic particles and water droplets.
  • 11. Relevant Terms Homosphere-The lowest 80km of the atmosphere, which the relative abundance of the permanent gases is constant. Heterosphere-The high atmosphere where gases are not well mixed but rather are stratified according to weight. Where lighter weighing gases are found.
  • 12. Gases Making Up Atmosphere Permanent Gases-Those gases whose relative abundance is constant within the homosphere. Variable Gases-Gases present in amounts that vary greatly in abundance, either vertically, horizontal, or seasonal. Water vapor is the most important variable gas.
  • 14. RESOURCES Information from the book: Aguado: Understanding Weather and Climate, Fifth Edition Copyright © 2010 Pearson Education, Inc. Pictures on Page 1- planetgreen.discovery.com(left), windows2universe.org(right) Atmosphere Structure picture- http://burro.cwru.edu/Academics/Astr201/Atmosphere/structure.jpg Composition chart- http://geogrify.net/GEO1/Images/FOPG/03T2.jpg Slide 10 Picture -http://www.examiner.com/images/blog/replicate/EXID47225/images/causes02.jpg
  • 15. The End