nitrogen
permanent gas, 78% of atmosphere
oxygen
permanent gas, 21% of atmosphere
variable gases
water vapor h20, carbon dioxide co2, methane ch4
current level of carbon dioxide in earth’s atmosphere
425 ppm
main elements of weather
air temperature, air pressure, humidity, clouds, precipitation, visibility, and wind
weather
the condition of atmosphere at any particular time and place (what we GET)
climate
average weather conditions over around 3+ decades (what we EXPECT)
hydrologic cycle
water cycle, continuous movement and exchange of water among the Earth’s surface, oceans and atmosphere, including phase changes (oceans as 70% of surface)
sun’s radiation
most important energy for the climate system of Earth, ultraviolet and visible radiation emitted
solar constant
1368 W/m^2 at the outer edge of earth’s atmosphere
visible light wavelengths
.4-.7 micrometers (red .7, purple/blue .4)
electromagnetic waves
can travel through a vacuum, move at the speed of light
shortwave radiation
the sun’s ultraviolet radiation
longwave radiation
the earth’s infrared, terrestrial radiation
stefan-boltzmann law
hotter objects emit more radiation than colder objects (sun more than earth)
wen’s displacement law
hotter objects emit radiation with shorter wavelengths (hot sun emits shortwave radiation, cool earth emits long wave radiation)
ozone shield
97% ozone is int he stratosphere and it protects humans from incoming ultraviolet radiation from the sun (cancerous)
montreal protocol
international agreement to reduce the use of ozone-depleting substances (like chlorofluorocarbons)
Dobson unit
amount of ozone o3 in air
photochemical smog
ozone near earth’s surface
specific hear
amount of heat required to raise temp of 1 gram of substance by 1C
substance’s specific heat
measured by that of liquid water
heat capacity
ability of a material to absorb heat (ocean greater than air because temp varies less)
temperature
measure of kinetic energy of atmospheric molecules