The potential of aircraft-induced ozone changes to force a substantial clim
ate impact is investigated by means of simulations with an atmospheric gene
ral circulation model, coupled to a mixed layer ocean model. We present res
ults from several numerical experiments that are based on ozone change patt
erns for 1992 aviation and on a future scenario for the year 2015. In both
cases, the climate signal is statistically significant. The strength of the
ozone impact is of comparable magnitude to that arising from aircraft CO2
emissions, thus meaning a non-negligible contribution to the total climate
effect of aviation emissions. There are indications of a characteristic sig
nature of the aircraft ozone related temperature response pattern, distinct
ly different from that associated with the increase of well-mixed greenhous
e gases. Likewise, the climate sensitivity to non-uniform ozone changes inc
luding a strong concentration perturbation at the tropopause may be higher
than the climate sensitivity to uniform changes of a greenhouse gas. In a h
ierarchy of experiments, for which the spatial structure of an aircraft-rel
ated ozone perturbation was left fixed, while the amplitude of the perturba
tion was artificially increased, the climate signal depends in a non-linear
way on the radiative forcing.