Nature 355, 339 - 342 (23 January 1992); doi:10.1038/355339a0

Indirect chemical effects of methane on climate warming

Jos Lelieveld & Paul J. Crutzen

Max-Planck-lnstitute for Chemistry, PO Box 3060, D-6500 Mainz, Germany

METHANE concentrations in the atmosphere have increased from about 0.75 to 1.7 p.p.m.v. since pre-industrial times^1,2. The current annual rate of increase of about 0.8% yr^-1 (ref. 2) is due to increases in industrial and agricultural emissions. This increase in atmospheric methane concentrations not only influences the climate directly, but also indirectly through chemical reactions. Here we show that the climate effects of methane's atmospheric chemistry have previously been overestimated, notably by the Inter-governmental Panel on Climate Change (IPCC)³, largely owing to neglect of the height dependence of certain atmospheric radiative processes. Using available estimates of fossil-fuel-related leaks of methane, our results show that switching from coal and oil to natural gas as an energy source would reduce climate warming. A significant fraction of methane emissions cannot, however, be accounted for by known sources; should leakages from gas production and distribution be underestimated for some countries, then it might be unwise to switch to using natural gas.

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