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Published byTheodore Hunter Modified over 9 years ago
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Composition Nitrogen (N 2 ): 78% Oxygen (O 2 ): 21% Other Gases: 1% Argon (Ar): 0.934% Carbon Dioxide (CO 2 ): 0.037% Water Vapor (H 2 O): 0.01 to.04% Neon (Ne): 18.2 ppmv (parts per million by volume) Helium (He): 5.0 ppmv Methane (CH4): 1.8 ppmv Krypton (Kr): 1.1 ppmv Hydrogen (H2): 0.5 ppmv Nitrous Oxide (N 2 O): 0.5 ppmv Xenon (Xe): 0.09 ppmv Ozone (O 3 ): 0.0 to 0.07 ppmv Nitrogen Dioxide (NO 2 ): 0.02 ppmv
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Pressure Air Pressure The measure of the force with which the air molecules push on a surface ○ The lower the altitude, the higher the pressure ○ The higher the altitude, the lower the pressure
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The Atmosphere Layers
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Troposphere 0-16 km from earth’s surface Top is 10 to 16 km depending on latitude and season. Temp Range: Highest ever recorded 57.8º C in Libya Coldest ever recorded -89º C in Antartica Layer right next to the earth’s surface Most dense 90% of atmospheric mass Carbon dioxide, water vapor, clouds, air pollution, weather, and life forms are found here The top of the troposphere is called the tropopause.
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Stratosphere From between 10 and 16 to 50 km above Earth’s Surface Temp Range: -85º C to 0º C Air is very thin and contains little moisture Temperature rises with altitude because of ozone (O 3 ) Ozone Layer is found in stratosphere Ozone absorbs solar energy in the form of ultraviolet radiation (warms air, protects Earth’s surface)
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Mesosphere 50 to 85 km from Earth’s surface Temp Range: 0º C to -90º C Temperature gets colder as altitude increases Meteors are burned up in this layer
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Thermosphere 85 to 500-1000 km above the Earth’s surface Temperature can be up to 2000º C in sunlight! Space Shuttle and ISS (International Space Station) orbit in this layer What we would think of as “outer space” Temp increases as altitude increases Absorbs much of Sun’s UV (Ultraviolet) and X-ray energy Northern Lights (Aurora Borealis) and Southern Lights take place here
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Exosphere From between 500-1,000 to 10,000 km (half the distance to the moon) No clear boundary between exosphere and space Molecules stay due to the Earth’s gravitational pull Molecules so few and far between they hardly collide
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Troposphere Stratosphere Mesosphere Ionosphere Exosphere Thermosphere Write in the labels! Ozone layer
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