Tropospheric trends for CF4 and C2F6 since 1982 derived from SF6 dated stratospheric air

The stratosphere can be used as an archive of past tropospheric conditions. Measurements of the long‐lived trace gases CF 4 , C 2 F 6 , and SF 6 have been carried out on stratospheric air samples obtained by balloon borne cryosampling from altitudes of up to 34 km between 1987 and 1995. SF 6 observations were used to ‘date’ the air samples. Above 25 km height the SF 6 concentrations are lagging the tropospheric ones by several years: 4.5 years for the tropics, 6 years for mid‐latitudes and up to 10 years for the arctic winter vortex. The high ages of stratospheric air found inside the upper polar vortex may indicate that the lag of the peak halogen burden between the troposphere and the polar stratosphere is longer than previously assumed. The age information from SF 6 allows to reconstruct tropospheric trends for CF 4 and C 2 F 6 since 1982. Accordingly, for the period 1982 to 1995, concentrations increased from 62 to 75 ppt for CF 4 and from 1.5 to 2.6 ppt for C 2 F 6 . Mean increase rates of 1.00 ppt yr −1 for CF 4 and 0.084 ppt yr −1 for C 2 F 6 translate into annual injection rates of about 14,600 t yr −1 and 1,900 t yr −1 respectively. With aluminium production as the only major source, average emissions per ton of primary aluminium are thus calculated to be 0.77 kg for CF 4 and 0.10 kg of C 2 F 6 in 1994.