GREENHOUSE EFFECTS OF AIRCRAFT EMISSIONS AS CALCULATED BY A RADIATIVE-TRANSFER MODEL

With a radiative transfer model, assessments are made of the radiative forcing in northern midlatitudes due to aircraft emissions up to 1990 . Considered are the direct climate effects from the major combustion products carbon dioxide, nitrogen dioxide, water vapor and sulphur dio xide, as well as the indirect effect of ozone production from NOx emis sions. Our study indicates a local radiative forcing at the tropopause which should be negative in summer (-0.5 to 0.0 W/m(2)) and either ne gative or positive in winter (-0.3 tp 0.2 W/m(2)). To these values the indirect effect of contrails has to be added, which for the North Atl antic Flight Corridor covers the range -0.2 to 0.3 W/m(2) in summer an d 0.0 to 0.3 W/m(2) in winter. Apart from optically dense non-aged con trails during summer, negative forcings are due to solar screening by sulphate aerosols. The major positive contributions come from contrail s, stratospheric water vapor in winter and ozone in summer. The direct effect of NO2 is negligible and the contribution of CO2 is relatively small.