The Atmosphere Flashcards
Define the term: Troposphere
- Lowest layer of the atmosphere
- Averages 36,090ft
- Temperature and pressure decrease with height
- Has almost all aerosols and water vapour
Define the term: Tropopause
- Boundary between the troposphere/stratosphere
- Higher over the equator, lower over the poles
- Higher in summer, lower in winter
- Higher during the day, lower at night
Define the term: Stratosphere
- Air is stable
- Usually devoid of cloud
- Is where the Ozone is
- Temperature slightly increases with height or is isothermal
Explain how surface pressure within the tropospheric column affects the height of the tropopause.
- Pressure increase = height of the tropopause increase
- Pressure decrease = height of the tropopause decrease
Explain how temperature within the tropospheric column affects the height of the tropopause.
Temperature increase = height of tropopause increase
Temperature decrease = height of tropopause decrease
State the average tropopause height and temperature at the equator.
- 56,000ft
- Minus 75 degrees Celsius
State the average tropopause height and temperature at the poles.
- 26,000ft
- Minus 45 degrees Celsius
State the average tropopause height and temperatures at the mid latitudes.
- 36,090ft
- Minus 56.5 degrees Celsius
Explain the sources of aerosols within the atmosphere.
- Tiny solid particles
- Salt from ocean spray (most common in NZ)
- Smoke and dust
- Volcanic ash
Explain the effects of aerosols within the atmosphere.
- Allow vapour to change to liquid or solid.
- Known as condensation nuclei or freezing nuclei
- Reduce visibility if too many
Explain the importance of aerosols within the atmosphere
- Cloud would not form without them
- Absence of them increases danger of aircraft icing (aircraft then becomes the condensation nuclei)
- Air becomes super saturated with no aerosols around
- Not many at the poles so air can reach 400% relative humidity
Describe the effect of increasing height and/or latitude on water vapour and aerosol content within the atmosphere.
- Source of water vapour and aerosols is the surface
- Both decrease in quantity with height
- Hardly any of both above the troposphere
Explain the effects on temperature within the atmosphere due to water vapour.
- Absorbs both solar and terrestrial radiation
- Warms the atmosphere
Explain the effects on temperature within the atmosphere due to carbon dioxide.
- Absorbs terrestrial radiation
- Warms the atmosphere
- Does not absorb solar radiation
Explains the effects on temperature within the atmosphere due to Ozone.
- Absorbs ultraviolet light
- Warms the area its located in, the stratosphere
- Creates an inversion acting as a weather lid on the troposphere.
With respect to the tropopause, describe the idealised global tropopause detailing approximate altitudes and the position of jet-streams.
- Sub tropical jet stream = 200hPa level 30degreesN/S
- 38,000 ft
- Polar Jet stream = 300-500hPa Level 60degreesN/S
- 30,000 - 18,000ft
With respect to the tropopause, explain why the height of the tropopause varies with latitude and season.
- Changes due to temperature of troposphere or stratosphere
- Warming the troposphere increases its height
- Cooling the stratosphere increases its height
Explain why the stratosphere is generally devoid of cloud and turbulence.
- Inversion/isothermal created due to the Ozone - this acts as a lid as the colder air below cannot rise any further.