INTERANNUAL EXTREMES IN THE RATE OF RISE OF ATMOSPHERIC CARBON-DIOXIDE SINCE 1980

OBSERVATIONS of atmospheric CO2 concentrations at Mauna Loa, Hawaii, a nd at the South Pole over the past four decades show an approximate pr oportionality between the rising atmospheric concentrations and indust rial CO2 emissions(1). This proportionality, which is most apparent du ring the first 20 years of the records, was disturbed in the 1980s by a disproportionately high rate of rise of atmospheric CO2, followed af ter 1988 by a pronounced slowing down of the growth rate. To probe the causes of these changes, we examine here the changes expected from th e variations in the rates of industrial CO2 emissions over this time(2 ), and also from influences of climate such as El Nino events. We use the C-13/C-12 ratio of atmospheric CO2 to distinguish the effects of i nterannual variations in biospheric and oceanic sources and sinks of c arbon. We propose that the recent disproportionate rise and fan in CO2 growth rate were caused mainly by interannual variations in global ai r temperature (which altered both the terrestrial biospheric and the o ceanic carbon sinks), and possibly also by precipitation. We suggest t hat the anomalous climate-induced rise in CO2 was partially masked by a slowing down in the growth rate of fossil-fuel combustion, and that the latter then exaggerated the subsequent climate-induced fall.