6.1 Introduction to the Atmosphere Flashcards
Atmosphere definition
a dynamic system (with inputs, outputs, flows and storages) that has undergone changes throughout geological time.
Atmosphere Inputs
- Water (evaporation and transpiration)
- CO2, SO4 and NO2 from combustion
- Volcanic ash
- Solar radiation
- oxygen through photosynthesis
- aerosols
Atmosphere outputs
- precipitation
- solar radiation
- oxygen for respiration
- CO2 for photosynthesis
Amount nitrogen
78%
- dilutes oxygen
- prevents rapid burning at the earth’s surface
- living things need it to make proteins
Amount oxygen
21%
- passive importance to weather and climate
- produced by photosynthesis
- reduced by deforestation
- needed for animal life
Amount argon
0.9% - Used in light bulbs.
Amount carbon dioxide
0.04%
- absorbs long wave radiation from earth and therefore contributes to natural greenhouse effect
- increases due to human activity is a major cause of global warming
- used by plants for photosynthesis
- increased by burning fossil fuels and deforestation
Amount water vapour
0.2 - 4.0%
- source of cloud formation and percipitation
- reflects/absorbs incoming radiation
- keeps global temp. constant
- provides majority of natural greenhouse effect
- essential for life
Atmosphere levels
- troposphere
- stratosphere
- mesosphere
- thermosphere
Troposphere
- fall in temp with height as atmosphere thins
- Most of the atmospheric mass is found.
- Most of our weather occurs here.
- Humans and other organisms have most interaction e.g. through exchange of gases or through introduction of pollutants.
- Greenhouse gases (GHG) help to regulate the temperature of the earth.
Mesosphere
- Temperature declines with height
- Coldest part of the atmosphere.
- density prevents absorption of energy
Stratosphere
- Temperature is constant at about -60°C in the lower part of the stratosphere, which is shielded by the ozone layer but then increases with altitude.
- The air is dry.
- stable
- thin
- increase in temp with height is due to absorption of solar radiation
- Ozone layer at the top of the stratosphere. Stratospheric ozone absorbs ultra violet radiation from the sun
Thermosphere
- Temperatures climb sharply in the lower thermosphere (below 200 to 300 km altitude), then level off and hold fairly steady with increasing altitude above that height.
- virtual vacuum
- rise in absorbed energy due to energised short wave radiation
Albedo definition
a measure of the reflectivity of a surface.
Albedo effect
when applied to the Earth is a measure of how much of the Sun’s energy is reflected back into space