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The Greenhouse Effect
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Image from: www.anthonares.net/ ogle_planet.jpg
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Image from: http://www.astro.lsa.umich.edu/sas/scales_universe/solar_system.jpg Our Solar System
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Venus Thick Atmosphere: 96% CO 2, Sulfuric Acid Average Temperature: 850 o F Mars Thin Atmosphere: 95% CO 2, also Argon, etc. Average Temperature: -64 o F Greenhouse Effect on Other Planets Earth Atmosphere: 79% N 2, 20% O 2, 1% Other gases Average Temperature: 56 o F
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All weather takes place in the Troposphere Earth’s Atmosphere Image from: www.wyckoffschools.org/.../ images/atmosphere.gi UV Light
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Ozone hole over Antarctica, September 2006. The blue and purple colors are where there is the least ozone. Ozone depletion is human caused – due to the release of Chlorine and Bromine gases into the Stratosphere. Image from: http://www.nasa.gov/vision/earth/lookingatearth/ozone_record.html Depletion of the Ozone Layer
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Spectrum of the sun compared with that of the earth Slide from: Scott Denning, 2007 Atmospheric Science Class
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Image from: http://www.noirextreme.com
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All weather takes place in the Troposphere Shortwave radiation comes through the atmosphere Earth warms and radiates longwave radiation
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All weather takes place in the Troposphere Shortwave radiation comes through the atmosphere Earth warms and radiates longwave radiation
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The average atmospheric temperature varies year by year, but overall, there has been a noticeable increase since 1920. From book: Essentials of Geology, S. Marshak, p. 533
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Carbon is always on the move From book: Essentials of Geology, S. Marshak, p. 520
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Eruption of Mount Cleveland, Alaska adds Carbon Dioxide to the air. Image from: www.nasa.gov/.../ image_feature_756_prt.htm
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Plants use Carbon Dioxide and sunlight to grow. The byproduct of Photosynthesis is Oxygen and sugars that make the plant grow. Image from: grapevine.net.au/.../ science/photosynthesis.html
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When plant material burns, it releases Carbon Dioxide in the Atmosphere. Image from: www.wpclipart.com/weather/ scenes/forest_fire.png
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Image from Energy Information Administration
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There is 30 percent more Carbon today than there was 150 years ago
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Carbon in the atmosphere joins with Oxygen to form CO 2 Carbon atom Oxygen atoms
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Image from IPCC Present-day Greenhouse Gas Sources 56.6% Carbon Dioxide, fossil fuels (oil, coal) 7.9% Nitrous Oxide 17.3% Carbon Dioxide, decay of plant material 14.3% Methane, natural gas, agriculture, etc.
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Carbon is always on the move From book: Essentials of Geology, S. Marshak, p. 520
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All weather takes place in the Troposphere Shortwave radiation comes through the atmosphere Earth warms and radiates longwave radiation, heat is trapped
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The average atmospheric temperature varies year by year, but overall, there has been a noticeable increase since 1920. From book: Essentials of Geology, S. Marshak, p. 533
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