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We present a range of estimates for future radiative forcings due to changes in tropospheric ozone (O 3 T ). Ozone distributions were generated by the UKMO 3‐D chemistry‐transport model for 1990, 2030, 2060, and 2100, using four sets of boundary conditions. Anthropogenic emissions evolved following either the IPCC SRES “high” (A2) or “central” (B2) case. Each scenario was run with both a fixed (1990) climate, and with a changing climate, as generated by a coupled ocean‐atmosphere GCM, forced with IS92a emissions. Calculated global mean O 3 T radiative forcings for the A2 (B2) cases for 1990–2100 were +0.43 (+0.22) W m −2 when climate change was ignored; these fell to +0.27 (+0.09) W m −2 when climate change was included. Without climate change, CH 4 lifetimes (τ CH 4 ) lengthened by 7–12% between 1990 and 2100; however, when climate change was included, τ CH 4 fell by 0–5%. Hence climate warming exerts a negative feedback on itself by enhancing O 3 T and CH 4 destruction.
Stevenson et al. (Sat,) studied this question.