where R is the net radiation, S the insolation,
the planetary
albedo, F the outgoing longwave radiation, and Q the absorbed
solar radiation.
See Hartmann (1993).
The main anthropogenic sources of atmospheric nitrous oxide are combustion (of fossil fuels, wood, or other biomass) and the widespread use of fertilizers, although the estimates for the amount supplied by the latter are highly variable. Natural sources include gas release into the atmosphere by the oceans and tropical and temperate forest soils.