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Earth's Atmosphere

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Most of our weather, however, occurs within the first 10 to 15 km. ... Sea salt. Pollution. Smoke. ash. Ozone Formation in the Stratosphere. O2 UV-C O O ... – PowerPoint PPT presentation

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Title: Earth's Atmosphere


1
Earth's Atmosphere (CH 1, pp.3-19)
99 of atmospheric gases, including water vapor,
extend only 30 kilometer (km) above earth's
surface. - Most of our weather, however,
occurs within the first 10 to 15 km.
2
Composition of the Atmosphere
  • A mixture of many gases
  • Composition is not constant

Fairly stable gases
Nitrogen Oxygen Argon
Variable Components
Water Vapor Aerosols Ozone Carbon Dioxide
3
Atmospheric Composition
Other Gasses 7
Other Gasses 1
Ar 93
Methane Ozone Nitrous Oxides Aerosols Water vapor

Nitrogen and Oxygen are the two most abundant
gasses in the atmosphere
4
Water Vapor
Clouds are made when water vapor in the air
turns into liquid This process releases Latent
Heat
5
Aerosols
Small solid particles and liquid droplets in the
air (excluding cloud Droplets and precipitation).
Ex. Haze over the Himalayas The Asian Brown
Cloud
6
Aerosols
Dust off the coast of Morocco
Other examples include Pollen Sea
salt Pollution Smoke ash
From MODIS
7
Ozone Formation in the Stratosphere
O2 UV-C ? O O O O2 M ? O3 M
Protects the Earth from Harmful Ultraviolet
rays From the sun.
8
Atmospheric Vertical Structure
Pressure Density
-The number of air Molecules decrease with
height, therefore Density (mass/volume) and
Pressure (force/area) decrease with height
-Standard Atmospheric Pressure 1013.25mb or
29.92 in Hg.
Figure 1.7
9
Atmospheric Layers
300 km
  • 4 layers are defined by trends in average air
    temperature
  • Molecules in the thermosphere have extremely high
    temperatures
  • Mesosphere cools with height
  • -Stratosphere warms due to ozone (O3) absorption
    of high energy solar radiation
  • - Troposphere cools with height because the
    Earth is warm from solar heating

Figure 1.9 p.16
Temperature Inversion where temperature
increases with height
10
Atmospheric Mixture and Charge
  • Additional layers include
  • Layers defined by mixing of gasses
  • The homosphere evenly mixed atmospheric gasses
  • b) The poorly-mixed
    heterosphere
  • AND
  • Electrically charged portion of the atmosphere
    called the ionosphere

Figure 1.10
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