Eighteen years of NO2 measurements using zenith-scattered sunlight are anal
yzed for seasonal, cyclic, and episodic variability and secular trends. The
analysis shows a marked increase in stratospheric NO2 over the period, cor
responding to a trend of 5% per decade, and the influences of both the El C
hichon and Pinatubo eruptions are clearly evident. Smaller effects of the E
l Nino-Southern Oscillation and quasi-biennial oscillation are apparent, bu
t correlation with the solar cycle is poor after correction for autocorrela
tion. All of these effects are similar for sunrise and sunset NO2.