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The Atmosphere and Climate
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Atmosphere
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Atmosphere The mixture of gases that surrounds Earth
Nitrogen, oxygen, carbon dioxide, and other gases are all parts of this mixture These gases are constantly added and removed
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Composition of the Atmosphere
78% Nitrogen 21% Oxygen
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Not just gases The atmosphere also contains atmospheric dust (many types of tiny, solid particles) in addition to gases. Atmospheric dust can include: Soil Salt Ash Pollen Bacteria and viruses Aerosols – tiny liquid droplets
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Layers of the Atmosphere
Four layers: Troposphere Stratosphere Mesosphere Thermosphere
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Troposphere The atmospheric layer nearest the surface of the Earth
It extends to 18 km above Earth’s surface
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Stratosphere The layer above the troposphere
Where the ozone layer is located
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Mesosphere The layer above the stratosphere
Extends to an altitude of about 80 km
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Thermosphere Layer of the atmosphere furthest from Earth’s surface
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Temperature in the Atmosphere
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Energy and Heating Three mechanisms transfer energy from the sun:
Radiation Convection Conduction Radiation - the transfer of energy across space and in the atmosphere Convection - the transfer of heat by air currents. Hot air rises and cold air sinks. Conduction - the flow of heat from a warmer object to a colder object when the objects are placed in direct physical contact
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Heating Earth Our planet only receives about two-billionths of the sun’s energy About half the energy that reaches the atmosphere will pass though to Earth’s surface
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Weather and Climate
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The Earth Has Many Different Climates (1)
Weather Climate Air circulation in lower atmosphere due to:
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The Earth Has Many Different Climates (2)
Currents Prevailing winds Earth’s rotation Redistribution of heat from the sun
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Natural Capital: Generalized Map of the Earth’s Current Climate Zones
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Global Air Circulation
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Coriolis Effect
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Energy Transfer by Convection in the Atmosphere
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Connected Deep and Shallow Ocean Currents
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Thermohaline Circulation
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Global Air Circulation, Ocean Currents, and Biomes
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Greenhouse Gases Warm the Lower Atmosphere
CO2 CH4 N2O Greenhouse effect Human-enhanced global warming
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Flow of Energy to and from the Earth
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The Earth’s Surface Features Affect Local Climates
Heat absorption by land and water Effect of Mountains Rain shadow effect Cities Microclimates
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Rain Shadow Effect
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