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Published byCori Sullivan Modified over 8 years ago
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The Atmosphere: One component of the climate system Composition / Structure Radiative transfer Vertical and latitudinal heat transport Atmospheric circulation Climate modeling Suggested further reading: Hartmann, Global Physical Climatology (Academic Press, 1994)
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Atmospheric layers
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Typical Vertical Profiles pressure temperature
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Solstice surface temperatures Annual range
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Sea surface temperature
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Atmospheric composition
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Atmospheric layers
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Evolution of halogenated gases
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Growth of CO 2 and CH 4
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Atmospheric mass
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Total mass ~ 5 x 10 18 kg = 5 x 10 15 t
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Atmospheric mass Total mass ~ 5 x 10 18 kg = 5 x 10 15 t ~ 7 x 10 5 t per capita
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Atmospheric mass Total mass ~ 5 x 10 18 kg = 5 x 10 15 t ~ 7 x 10 5 t per capita CO 2 (370 ppm) : ~ 200 t per capita
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Atmospheric mass Total mass ~ 5 x 10 18 kg = 5 x 10 15 t ~ 7 x 10 5 t per capita CO 2 (370 ppm) : ~ 200 t per capita O 3 (0.5 ppm) : ~ 300 kg per capita
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Atmospheric mass Total mass ~ 5 x 10 18 kg = 5 x 10 15 t ~ 7 x 10 5 t per capita CO 2 (370 ppm) : ~ 200 t per capita O 3 (0.5 ppm) : ~ 300 kg per capita [Cl] (2 ppb) : ~ 1.5 kg per capita
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Atmospheric absorption
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Planetary energy balance
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Total albedo (observed from space)
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Planetary energy balance
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Emission temperature Planetary energy balance
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Net outgoing longwave radiation (measured from space: Wm -2 ) Recall: absorbed solar rad per unit area
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