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Earth’s Changing Atmosphere
Chapter 15
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Earth’s atmosphere supports life
Atmosphere – a layer of air and gases that surrounds and protects the earth Keeps Earth warm Transports energy to different regions Although important, it is very thin comparatively
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Atmosphere characteristics
As you go up in the atmosphere (altitude), the air becomes less dense or thinner. Density is the amount of “stuff” in a certain amount of space ( volume) The higher you get the less air molecules are between you and the top of the atmosphere. That means there are less air molecules pushing on you ( less air pressure)
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A recipe for the atmosphere?
Mostly gases Some tiny solid or liquid particles 78% nitrogen 21 % oxygen 1% trace gases ( argon, carbon dioxide, etc)
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Sudden changes in our atmosphere
Volcanic eruptions -lots of gases and ash into the atmosphere in a short period of time. Forest fires - carbon dioxide, smoke and ash enter the atmosphere Dust storms - clouds of eroded soil particles enter the atmosphere by strong winds.
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Energy movement in the atmosphere
Radiation- energy transfer through waves Conduction - energy transfer by direct contact Convection –energy transfer by movement of liquid or gas (hot/less dense material rises as cooler/more dense material sinks)
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Layers of the atmosphere
Troposphere ( closest to the earth) Stratosphere ( contains the ozone layer) Mesosphere Thermosphere
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Gases in the atmosphere absorb radiation
Certain gases in the atmosphere help protect Earth from ultraviolet and infrared radiation The Ozone layer is a layer of ozone in the stratosphere that absorbs harmful ultraviolet radiation
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What keeps the Earth Warm?
A “blanket” of greenhouse gases allows the suns radiation to pass through but then traps some of the reflected heat in. This process is called the greenhouse effect.
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