Atmosphere thin layer of gas that surrounds the earth
protects us from harmful radiation and contains oxygen
layers of atomosphere
troposphere
stratosphere
mesosphere
thermosphere
Troposphere 12 km
almost all weather and clouds appear here
air pressure drops as altitude increases
75% of the air is here
Stratosphere 12 km-50 km
ozone layer is here ( absorbs UV light )
warmer than troposphere because of UV energy
Mesosphere 50 km-85 km
meteors burn here
air pressure drops when altitude increases
Thermosphere 500 km-1000km
extremely thin air
Leo (low earth orbit) satellites orbit here
Exosphere
where atmosphere merges into space vaccum
Compositon of atomosphere
nitrogen 78%
oxygen 21%
variable gasses - water vapour
Greenhouse gasses
water vapour H2O
methane CH4
carbon dioxide CO2
Greenhouse effect the process that keeps the earths surface warm
energy from the sun comes down as visible light the earths atmosphere is largely transparent and the earths surface absorbs it then re-radiates back into space and infrared light
earths energy balance budget between the amount of energy coming from the sun to earth and energy outgoing from earth to space
solar energy is measured in w/m2
visible light is reflected by white surfaces like clouds and ice
visible light is absorbed by warm grounds and oceans
Processes that add carbon into atmosphere
cellular respiration (breathing)
Anaerobic decomposition (decaying)
Volcanic eruption (volcanoes)
Burning fossil fuels (factories)
Process that remove carbon
photosynthesis
ocean dissolving CO2
combustion reactions will always be fuel+oxygen=carbon dioxide+water