In situ measurements of NO, NO2, O-3, HO2, ClO, pressure, and temperature h
ave been made at high solar zenith angles (SZA, 70 degrees - 93 degrees) in
the lower stratosphere. These measurements are used to derive the photolys
is rate of NO2, J(NO2),, using a time-dependent method. The resultant J(NO2
) values and the results of a multiple-scattering actinic flux model show a
linear relationship throughout the SZA range. The difference of the two se
ts of J(NO2) values of about 11% suggests that the model scattering calcula
tion is very accurate at high SZA conditions near sunrise and sunset.