C13 The atmosphere Flashcards
how was the early atmosphere formed
volcanic eruptions released lots of CO2
gases in early atmosphere
mainly CO2
nitrogen and water vapour
traces of methane and ammonia
how did oxygen levels increase/ CO2 decrease
oceans formed- water vapour condensed
CO2 dissolved in seawater
removed in photosynthesis
‘locked in’ rocks and fossil fuels
algae photosynthesized- rise in O2
atmosphere % now
78% nitrogen
21% oxygen
small portions, CO2, water vapour
greenhouse effect
sun emits short electromagnetic wavelengths
surface absorbs wavelengths and cools by emitting longer wavelength infrared radiation
GGs absorb infrared
stimulates molecules, raising their temp
consequences of GGs
rising sea levels- melting ice caps
flooding of low lying land
increased coastal erosion
frequent extreme weather events
changes in temp
change in amount, timing and distribution of rainfall
change of distribution of wildlife
carbon footprint
total amount of CO2 and other greenhouse gases emitted over its full life cycle
hydrocarbon
only hydrogen and carbon atoms
produce carbon dioxide and water when fully oxidised
CO2 + H2O
sulfur impurities
burn to form sulfur dioxide
can cause acid rain
sulfur removed from fuels before burning
sulfur dioxide removed from flue gas
carbon monoxide
product of incomplete combustion
can cause global dimming