A global three-dimensional atmospheric tracer transport model is used
to study the sources End sinks of atmospheric carbon monoxide (GO). So
urce functions are included for the release of CO from the oxidation o
f methane, technological sources, biomass burning, the oxidation of hy
drocarbons and the oceans. The removal of CO from the atmosphere is as
sumed to be largely due to oxidation through reaction with hydroxyl ra
dicals (OH) and removal by soils. To compute CO destruction, a paramet
erised OH field, calibrated to reproduce the loss of methyl chloroform
, is employed. For the removal of CO by soils, a model is used which a
ssumes that the flux of CO into soils is dependent on net primary prod
uctivity. To constrain the magnitude of the CO sources and sinks, atmo
spheric observations of CO are used. The deduced total CO source is 18
55-2355 Tg. If present estimates of the release of CO from biomass bur
ning and oxidation of hydrocarbons are correct then removal by soils c
ould potentially be a substantial sink for CO.