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Published byPierce Fleming Modified over 8 years ago
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Atmosphere
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What makes up our atmosphere? Nitrogen Oxygen Argon
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Nitrogen Cycle
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Atmospheric Pressure There is less air at higher altitudes. Force of 10 Newtons at Sea Level
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Atmospheric Pressure As altitude INCREASES Air Pressure DECREASES DECREASES
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Temperature Varies with increase in altitude Why? Solar energy absorption varies as it moves down through the atmosphere.
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Troposphere Layer closest to the Earth –Almost all water vapor and CO 2 Temperature DECREASES Tropopause is the upper boundary –It varies with latitude
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Stratosphere From tropopause to 50 km –Contains almost all ozone Temperature INCREASES Stratopause is the upper boundary
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Mesosphere From 50-80 km –Coldest layer Temperature DECREASES Mesopause is the upper boundary
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Thermosphere N and O absorb solar energy Temperature INCREASES 2 Layers –Ionosphere- lower region –Exosphere- upper region
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Tropopause Stratopause Mesopause Exosphere Troposphere Stratosphere Mesosphere Thermosphere Ionosphere
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