摘要:Methane is the second most important anthropogenic greenhouse gas in the atmosphere
next to carbon dioxide. Its global warming potential (GWP) for a time horizon of
100 years is 25, which makes it an attractive target for climate mitigation policies.
Although the methane GWP traditionally includes the methane indirect effects on the
concentrations of ozone and stratospheric water vapour, it does not take into account the
production of carbon dioxide from methane oxidation. We argue here that this
CO2-induced effect should be included for fossil sources of methane, which results
in slightly larger GWP values for all time horizons. If the global temperature
change potential is used as an alternative climate metric, then the impact of the
CO2-induced effect is proportionally much larger. We also discuss what the correction term
should be for methane from anthropogenic biogenic sources.