Flash Cards Geography Climate
Structure of Atmosphere?
- Troposphere
- Stratosphere
- Mesosphere
- Thermosphere /Exosphere
Temperature Inversion?
Area where temperature changes in reverse direction
Inversion?
When temperature increases with altitude
Positive Lapse Rate?
When temperature decreases with height
Negative Lapse Rate?
When temperature increases with height.
Troposphere?
- Layer we live in
- Contains weather- water vapour/clouds
- 17km at equator and 8km at poles
- Temperature decreases with altitude
- Upper limit-Tropopause
Stratosphere?
- Characterised by steady increase in temperature, due to high concentration of ozone which absorbs Uv radiation
- Upper limit-Stratopause
- Protective shield against meteorites
Mesosphere?
- Temperature drops rapidly with height as there is nothing to absorb it. No ozone or water vapour
- Winds extreme
- Upper limit-Mesopause
- Least understood too high for aircraft and low for spacecraft
Thermosphere?
- Thickest layer with the lightest gases
- Scattered molecule absorb UV propelling them at high speed and temperature causing temperatures like 1500C
- ISS orbit
Exosphere?
- Explains a and contracts causing it too come into contact with solar storm, causing explosive events/ solar flares
- Weather satellites
Gases?
Permanent- Nitrogen, O2, Argon
Variable- Co2, Methane, Ozone
Solids?
Pollution particulate, dust, pollen, plastic, salt, silica
Mass and Weight?
Individual molecule have mass therefore weight due to gravity- exerts pressure on surface
Compressibility?
Lower layers more compressed. When air is heated it expands reducing compression. Air is cooled it contracts increasing compression
Mobility?
Attempts to equalise pressure causing wind. Horizontal-advecation, Vertical-convection
Insolation?
Incoming Solar Radiation. The energy the sun gives off as shortwave radiation.
Energy Transfer?
- Terrestrial or Longwave Radiation- warms atmosphere from below
- Conduction- heat is passed from one molecule to another or from surface to air by direct contact.
- Convection- heater air become less dense and rises and cool air sinks in to replace it.
- Latent Heat- energy is water vapour that is radiated when it condenses.
How is insolation lost?
- Absorption- upper layers absorb deadly radiation. Ozone, vapour, dust.
- Scattering- dust scatters radiation and cause sunsets by scattering visible light.
- Reflection or Surface Albedo- reflect sunlight back , lighter reflects better.
Greenhouse Effect?
Natural process made possible by gases in Earths atmosphere. They trap heat and reflect it back down to Earths surface. Prevents Earth from cooling too much.
Greenhouse?
Sunlight enters glass as shortwave radiation. Converted to longwave and traps heat.
What caused large amounts of greenhouse gases to be released?
Industrial Revolution in 1700s and 1800s
Uses for Greenhouse Gases?
Co2- fossil fuels burned
Methane-livestock farming
CFCs- Aerosols and Polystyrene
Ozone-Smog reacting with organic compounds
Nitrous Oxide-Agriculture
Global Warming?
The increase of the Earths surface temperature due to the emissions of greenhouse gases.
Carbon Cycle?
Carbon is essential for life. It is stored in oceans, plants, atmosphere and rocks. Carbon is recycled for photosynthesis and when ingested. When they die their remains deconpose and turn into rocks, minerals and fossil fuels. Released back into atmosphere when burnt.