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Chapter 19: Earth’s Atmosphere.

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Presentation on theme: "Chapter 19: Earth’s Atmosphere."— Presentation transcript:

1 Chapter 19: Earth’s Atmosphere

2 What is in our atmosphere?
78% N2  Cycle, nitrogen-fixed by bacteria in soil to roots, returned via waste & decay 21% O2  Cycle, used by respiration, fires, weathering, returned by photosynthesis Ozone: O3, absorbs harmful UV radiation, damaged by CFCs & exhaust 1% Ar & other Particulates: tiny solid or liquid from volcanoes, sea spray, pollen What is in our atmosphere?

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4 Weight of atmosphere pressing down on Earth  air pressure
Pressure decreases w/ altitude Pressure increases as temperature increases Pressure decreases as humidity increases b/c water vapor is less dense than air Measured w / barometer (atm., mm, mb) Atmospheric Pressure

5 Measuring Air Pressure
Mercurial Aneroid Measuring Air Pressure

6 Layers of the Atmosphere
Temperature patterns mark layers As Altitudes increases, Pressure decreases Layers of the Atmosphere

7 Layers of the Atmosphere
Troposphere At surface, weather, almost ½ of all H2O & CO2 Altitude increases, Temperature decreases Ends in Tropopause (12 km) Stratosphere Contains OZONE LAYER As altitude increases, temperature increases b/c absorbing sun’s energy (UV) Ends in Stratopause Layers of the Atmosphere

8 Layers of the Atmosphere cont.
Mesosphere Temperature decreases as altitude increases Coldest temperature Ends with Mesopause Thermosphere Highest temperatures b/c of radiation, O2 & N2 absorbing sun’s energy Contains IONOSPHERE (Auroras) Exosphere: entrance into space Layers of the Atmosphere cont.

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10 How does the sun’s energy affect OUR atmosphere?
Electromagnetic Radiation Energy from sun, travels through space @ 3 x 10 m/s Earth heated by energy transfer 8 How does the sun’s energy affect OUR atmosphere?

11 Electromagnetic Radiation
LONGER WAVELENGTHS/LOWER ENERGY SHORTER WAVELENGTHS/HIGHER ENERGY Electromagnetic Radiation

12 Upper Atmosphere (U.A.) absorbs almost all radiation except some visible & infrared reach surface
SCATTERING: L.A. deflects radiation in all directions Absorbed radiation heats surface & emitted as infrared

13 What’s reflected is “ALBEDO”


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