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Unit 3 Notes Part 4: Greenhouse Effect
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What is the Greenhouse Effect?
The warming of the Earth due to an atmosphere. The greenhouse effect causes an increase in the temperature of a planet as heat energy from sunlight is trapped by the gaseous atmosphere.
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How does the Greenhouse Effect work?
Solar Energy (sunlight) is short-wavelength radiation which easily penetrates the Earth's atmosphere and warms the Earth Only about one quarter of incoming sunlight is reflected by the atmosphere.
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How does the Greenhouse Effect work?
The warmed Earth emits long-wavelength radiation (infrared waves or heat energy) back into space These longer waves are mostly absorbed by greenhouse gasses, trapping the energy. Some energy is reradiated back to Earth.
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What happens to the incoming solar radiation as it passes through Earth’s atmosphere?
Incoming solar radiation is made up of some UV and infrared, but is mostly visible light 70-75% makes it through the atmosphere UV is absorbed by ozone Infrared is absorbed by water vapor Water Vapor Carbon Dioxide Oxygen and Ozone Methane Nitrous Oxide Rayleigh Scattering
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What happens to the outgoing thermal radiation as it travels from Earth’s surface toward space?
The energy absorbed by the surface is radiated from the Earth as longwave radiation 15-30% makes it out to space Some of this is absorbed by water vapor, followed by CO2, methane, and nitrous oxide
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Describe the major “greenhouse gases?”
Water vapor, which causes about 36-70% of the greenhouse effect on Earth (not including clouds) Carbon Dioxide, which causes 9-26% Methane, which causes 4-9% Ozone, which causes 3-7% Nitrous Oxide This animation shows how a carbon dioxide molecule vibrates when it absorbs heat. Courtesy of UCAR (LEARN and COMET)
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