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Composition and Layers of the Atmosphere
Mr. Silva
Ag Earth Science
Composition of the Atmosphere• Nitrogen 78.08%• Oxygen 20.95%• Argon 0.93% (9300 ppm)• Carbon Dioxide 0.035% (350 ppm)• Neon 18 ppm• Helium 5.2 ppm• Methane 1.4 ppm• Ozone 0.07 ppm
3. Composition of the Atmosphere
Other Components of the Atmosphere
• Water Droplets• Ice Crystals• Sulfuric Acid Aerosols• Volcanic Ash• Windblown Dust• Sea Salt• Human Pollutants
3. Composition of the Atmosphere
Aerosols
Aerosols Any solid or liquid particle in the
atmosphere.
• Natural (e.g. dust) and human (e.g. soot) sources.
• Can remain suspended for long periods of time (days to weeks).
• Contribute to cloud formation and precipitation by acting as condensation nuclei.
Aerosols: Saharan Dust Storm
Dust particles are about 10 micro-meters in size (0.00001 meters). Roughly 1/10 the
width of a human hair. Big ones settle out..
Aerosols: Pollution over Los Angeles
Ozone: O3
Partial PressureGas Molecular
WeightPartial
Pressure
Nitrogen 28 78%
Oxygen 32 21%
Argon 40 0.9%
Water Vapor 18 0-4%
Carbon Dioxide 44 350 ppm
2. Partial pressure, vapor pressure and humidity
Layers of the Atmosphere
Structure (Layers) of the Atmosphere
• Defined by Temperature Profiles• Troposphere
– Where Weather Happens
• Stratosphere– Ozone Layer
• Mesosphere• Thermosphere
– Ionosphere
4. Layers in the atmosphere are defined by temperature profiles
The Troposphere
• Most dense• All weather takes place here
Troposphere• Heating of the Surface creates warm air at
surface• Warm air rises, but air expands as it rises
and cools as it expands (Adiabatic cooling)
• Heating + Adiabatic Cooling = Warm air at surface, cooler air above
• Buoyancy = Cool air at surface, warmer air above
• Two opposing tendencies = constant turnover4. Layers in the atmosphere are defined by temperature profiles
The Stratosphere
• Dry• Absorbs ultraviolet
radiation (UV)• Ozone layer is here
• Ozone (O3) absorbs much UV C and UV B waves.
Stratosphere
• Altitude 11-50 km• Temperature increases with altitude• -60 C at base to 0 C at top• Reason: absorption of solar energy to
make ozone at upper levels (ozone layer)
• Ozone (O3) is effective at absorbing solar ultraviolet radiation
4. Layers in the atmosphere are defined by temperature profiles
The Mesosphere
• Coldest• Many meteors burn up here
Mesosphere
• 50 – 80 km altitude• Temperature decreases with altitude• 0 C at base, -95 C at top• Top is coldest region of atmosphere
4. Layers in the atmosphere are defined by temperature profiles
The Thermosphere (Ionosphere)
• Region of charged ions (positive) and electrons
• Electrons are torn off atoms by sunlight of short wavelengths
• Electrons don’t recombine easily because the distance between molecules is large at high altitudes and collisions are not frequent
Thermosphere
• 80 km and above• Temperature increases with altitude as
atoms accelerated by solar radiation• -95 C at base to 100 C at 120 km• Heat content negligible• Traces of atmosphere to 1000 km• Formerly called Ionosphere
4. Layers in the atmosphere are defined by temperature profiles