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Chapter 19: Earth’s Atmosphere
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3 methods of energy transfer
Radiation (EMR) Conduction (BY TOUCH) Convection (MOVEMENT OF GAS OR LIQUID) 3 methods of energy transfer
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Greenhouse effect – “good” & natural global warming “bad”
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Latitude vs solar energy
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Earth’s orbit affects angle of sun’s rays
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How does the atmosphere circulate?
Fluids move from high to low pressure Equator moves faster than poles Warm air rises, cold air sinks Earth rotates How does the atmosphere circulate?
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Coriolis Effect: curving of moving object’s path b/c of rotation
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Coriolis Effect in action
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Global winds: set up by Coriolis effect & convection
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Jet streams
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Local winds caused by uneven heating
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Valley breeze – warm air moves up mt. breeze – cold air moves down
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The End
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