structure and composition of the atmosphere
TRANSCRIPT
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Ryan Beaudry
Introduction to the Structure and Composition of Earths
Atmosphere
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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.
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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
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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).
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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
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ADDITIONS
• Tropopause-Transition zone where the temperature ceases to decrease.
• Stratopause-Top of stratosphere, temperatures continue to increase.
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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.
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http://burro.cwru.edu/Academics/Astr201/Atmosphere/structure.jpg
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COMPOSITION OF ATMOSPHERE
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• Made up of:
-Mixture of invisible gases -Large number of suspended microscopic
particles and water droplets.
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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.
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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.
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http://geogrify.net/GEO1/Images/FOPG/03T2.jpg
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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
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The End