A chronology of tropospheric CF4 mixing ratios is reported for the northern
hemisphere, A decline of global emissions of CF4 from 16,000 to 11,000 met
ric tons yr(-1) is found for the periods 1978-1990 and 1992-1998, respectiv
ely. The atmospheric chronology of CF4 is applied to determine the age of a
ir of cryogenic air samples collected on rocket and balloon platforms. Age
values of 7 years are found inside the polar vortex between 25-44 km altitu
de and of 11 years between 56 and 61 km altitude, which is significantly hi
gher than predicted by most models currently used to assess the effects of
high-flying aircraft. The results suggest that the mesosphere is more isola
ted from below than previously believed. A comparison of age values derived
from CF4 and SF6 relative to predicted deviations constrains the atmospher
ic lifetime of SF6 to >5,000 years.