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Layers of the Atmosphere
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Atmosphere The atmosphere is the blanket of gases that surrounds the Earth Composition: 78% Nitrogen 21% Oxygen 1% other gases such as Argon, Carbon Dioxide, Water Vapor and Ozone
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Atmosphere The atmosphere is divided up into 4 different layers:
Troposphere Stratosphere Mesosphere Thermosphere
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Troposphere(approx. 0 – 10 km)
Contains most of the mass of the atmosphere Most weather takes place in the troposphere Temperature decreases (15 C (57F) -40 C/ (-40F)) Has the greatest air density The top of the troposphere is called the tropopause
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Stratosphere (approx. 10-50 km)
Air density decreases Airplanes fly in this layer (to avoid weather) Temperature increases with increasing altitude (-40 C (-40 F) -3 C (27F)) Contains the Ozone Layer Stratopause
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Ozone Ozone (O3) – A gas in the stratosphere that blocks UV radiation
CFC’s (a form of pollution) can deplete ozone
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Mesosphere (approx. 50 – 90 km)
Temperature decreases (-3 C (27 F) -90 C (-130 F)) Meteors from outer space burn up in this layer The Mesopause is the coldest part of the atmosphere
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Thermosphere (approx. 90 km – 500 km)
Has the greatest temperature range ( -90 C (-130 F) 2000 C (3632 F)) Because gases are spaced so far apart Has low air density Contains the Ionosphere – Region where gases are ionized by the suns energy
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The Exosphere ( approx. 500 km – Outer Space)
The upper portion of the Thermosphere where gases escape into outer space Has the lowest air density Contains lighter gases such as hydrogen and helium
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