General Characteristics Of The Atmosphere Flashcards
Extent of the atmosphere and evidence?
Top of atmosphere does not have a clear definition
Evidence exists of atmosphere at high levels:
Satelite drag -1600km
Aurora Borealis - 1000km
Describe vertical distribution of air density;
1/2 of weight in the lower 18,000ft /5-6km
What are 3 atmospheric properties?
Mobility
Capacity for expansion
Capacity for compression
Define Mobility in regards to the atmosphere.
Air must be mobile to produce weather
Define capacity for Expansion.
Expansion causes temperature to cool and clouds to form
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Utmost importance to meteorology, without it there would be no weather
Define capacity for Compression;
Compression causes the temperature to warm, and any clouds to dissipate
List the 5 most abundant gases in the atmosphere and state the percentage of volume of the two most abundant;
Nitrogen 78%
Oxygen 21%
Water vapour <_3%
Argon 0.91%
Carbon Dioxide 0.03% (varies)
Which gas is most important to the weather and discuss why it is important.
Water vapour is the most important gas to weather
It can condense into liquid water (forming clouds and precipitation)
It can sublimate into solid water (Forming ice crystals, hail, snow, frost)
Define and state the importance of lithometeors;
Could could not form without these particles/ condensation nuclei
Define hyrdometeors;
All clouds and precipitation are composed of either liquid water droplets or ice crystals and therefore are composed of hydrometeors
Name 2 Basic forms of air pollution:
Solid particles (incomplete burning of fuel particles)(coal, fuel containing lead additives, etc)
- larger particles fall to ground
-smaller particles remain suspended in the air
How is the vertical classification of the atmosphere defined?
Divided into terms of temperature
Divisions are called spheres
Transition zone between two spheres is a “pause”
State the 3 lowest vertical divisions, and their pauses (and the fourth for a bonus point!)
From the surface upward:
- Troposphere
\ Tropopause
- Stratosphere
\ Stratopause
- Mesosphere
\ Mesopause
- Thermosphere
Describe the Troposphere;
Temperature decreases with height to its upper limit called the tropopause
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Almost all weather occurs in the troposphere, due to its precense of water vapour and vertical air currents
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Winds increase with height to reach a maximum just below the tropopause
Describe the tropopause;
Dividing line between the troposphere and the stratosphere
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Occurs when temperature stops decreasing and becomes constant with height (isothermal)
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Height lowest over cold air and highest over warm air
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Average height: 11km/36,000ft
|\ Poles: 7km /25,000 ft
\ Equator: 15km/ 56,000 ft
Higher tropopause = higher base of cirrus