A simple methane model is presented in which lifetime changes are expr
essed as a function of CH4 concentration and emissions of NOx, CO and
NMHCs. The model parameters define the relative sensitivities of lifet
ime to these determining factors. The parameterized model is fitted to
results from five more complex atmospheric chemistry models and to 19
90 IPCC concentration projections. The IPCC data and four of the five
models are well fitted, implying that the models have similar relative
sensitivities. However, overall sensitivities of lifetime to changes
in atmospheric composition vary widely from model to model. The parame
terized model is used to estimate the history of past methane emission
s, lifetime changes and OH variations, with estimates of uncertainties
. The pre-industrial lifetime is estimated to be 15-34% lower than tod
ay. This implies that: 23-55% of past concentration changes are due to
lifetime changes. Pre-industrial emissions are found to be much highe
r (220-330 TgCH(4)/y) than the best estimate of present natural emissi
ons (155 TgCH(4)/y). The change in emissions since pre-industrial time
s is estimated to lie in the range 160-260 TgCH(4)/y, compared with th
e current best guess for anthropogenic emissions of 360 TgCH(4)/y. The
se results imply either that current estimates of anthropogenic emissi
ons are too high and/or that there have been large changes in natural
emissions. 1992 IPCC emissions scenarios are used to give projections
of future concentration and lifetime changes, together with their unce
rtainties. For any given emissions scenario, these uncertainties are l
arge. In terms of future radiative forcing and global-mean temperature
changes over 1990-2100 they correspond to uncertainties of at least /- 0.2 Wm(-2) and +/- 0.1 degrees C, respectively.