Aerosol optical depth in the visible range is affected by ozone absorp
tion (Chappuis band). In order to derive reliable information from ext
inction measurements of solar irradiance, a suitable correction has to
be considered. Ozone correction based on climatological data sets has
been proved ineffective. Better results are typically obtained on the
basis of indirect methods which, nevertheless, require some nd hoc as
sumptions such as the wavelength dependence on aerosol optical depth.
A validation of these indirect methods is provided in this paper. Dire
ct estimations of ozone profiles have been derived from ultra-violet a
nd visible spectral scattered solar radiation. The Umkehr method was r
esorted for implementing a suitable inversion scheme for the ozone pro
file. Our results show that indirect ozone correction procedures are r
eally capable of yielding absorption ozone-free aerosol optical depth.
(C) 1998 Elsevier Science Ltd. All rights reserved.