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Published byShawn Price Modified over 9 years ago
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CHARACTERISTICS OF THE ATMOSPHERE
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Composition of Atmosphere Made up mostly of Nitrogen (N) Oxygen makes up a little more than 20%
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Atmospheric Pressure Gravity pulls molecules towards Earth Creates air pressure Atmosphere is held by gravity As altitude increases, air pressure decreases
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Atmospheric Temperature As altitude increases, temperature decreases Lower part of atmosphere is warmer Contains high percentage of gases that absorb solar energy
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Layers of the Atmosphere Troposphere Stratosphere Mesosphere The layer in which we live Lies next to Earth’s surface Home of the Ozone layer Middle layer Coldest layer
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Layers of the Atmosphere cont’d Thermosphere Ionosphere Edge of the Atmosphere Uppermost layer Home of the Auroras Upper Mesosphere and Lower Thermosphere Nitrogen and Oxygen absorb harmful solar energy
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GLOBAL WINDS AND LOCAL WINDS
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Why Air Moves Equator and Poles Cold air sinks Creates a high pressure around the poles Cold air then flows toward the equator
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Pressure Belts Coriolis Effect Every 30° latitude Bands of high and low pressure Curving of path of currents due to Earth’s rotation
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Global Winds Polar Easterlies Westerlies Wind belts that extend from the poles to 60° latitude Wind belts found between 30° and 60° latitude
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Trade Winds Doldrums Winds that blow from 30° to almost the equator Where trade winds meet around the equator
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Horse Latitudes Jet Streams At about 30° North and 30° South Sinking air creates an area of high pressure Narrow belts of high- speed winds Blow in the upper Troposphere and lower Stratosphere
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Local Winds Mountain and Valley Breezes Sea and Land Breezes Generally move short distances Can blow from any direction Caused by an area’s geography Affected by temperature
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Sea Breeze Land Breeze wind that blows from an ocean or lake to land land warms faster than water happens during day winds that blow from land to a body of water land cools faster than water happens at night
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AIR POLLUTION
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Primary Pollutants Secondary Pollutants Pollutants put directly into the air by human or natural activity When primary pollutants react with other primary pollutants or natural substances (water vapor)
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Industrial Air Pollution Indoor Air Pollution Burning of fossil fuels Ex: Power plants Sometimes can be more polluted than outside air
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Ozone Ozone Hole Layer is thinning over the Arctic and Antarctic regions Allows more UV radiation to reach Earth’s surface CFCs cause Ozone depletion CFCs remain active for 60-120 years
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Human Effects from Air Pollution Short-term effects Long-term effects Coughing Sneezing Headaches Eye irritation Lung cancer
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Clean Air Act EPA Requires many industries to use pollution-control devices Sets air quality standards-
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