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Published byEvelyn Williamson Modified over 6 years ago
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The Atmosphere Atmosphere Composition - 76% Nitrogen - 23% Oxygen
Chapter 17 Atmosphere Composition - 76% Nitrogen - 23% Oxygen - Also contains: water vapor- source of clouds and precipitation ozone- blocks UV rays
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Atmosphere Structure * Air pressure decreases with height
* Temperature generally decreases with height Temperature Layers 1) Thermosphere- hottest layer (top) 2) Mesosphere- coldest layer 3) Stratosphere- contains ozone 4) Troposphere- weather occurs (bottom)
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Atmosphere Structure
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Earth’s Effects on the Atmosphere
- Rotation – Earth spins on its axis - Revolution – Earth orbits the sun * Earth is tilted 23.5 degrees - remember: Earth’s tilt causes seasons Example Summer – tilted toward the sun (more daylight) Winter – tilted away from sun (less daylight)
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Tilt of Earth’s Axis
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Earth’s Tilt and the Seasons
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Heat - energy moving from one area to another - Temperature- measure of moving energy Types of Heat 1) Conduction- energy through matter 2) Convection- energy moving inside matter 3) Radiation- energy given off an object * Heat moves from HIGH to LOW!!*
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Types of Energy Transfer (heat)
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Solar Radiation Effects
1) Absorbs into objects 2) Bounces off objects 3) Goes through objects Examples -Greenhouse Effect- gases in the air that trap radiation - Albedo- radiation reflected by a surface ex.- clouds block radiation during day (cooler) clouds trap radiation at night (hotter) - Land heats & cools faster than water
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Solar Radiation Effects
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Albedo
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Isotherms lines on weather maps that connect points where temperature is the same - generally run east - west & show a decrease in temperatures from tropics toward the poles
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