M. Huber et al., TOTAL ATMOSPHERIC OZONE DETERMINED FROM SPECTRAL MEASUREMENTS OF DIRECT SOLAR UV IRRADIANCE, Geophysical research letters, 22(1), 1995, pp. 53-56
With a double monochromator, high resolution spectral measurements of
direct solar UV-irradiance were performed in Arose during February and
March, 1993. Total atmospheric ozone amount is determined by fitting
model calculations to the measured spectra. The results are compared w
ith the operationally performed measurements of a Dobson and a Brewer
spectrometer. The total ozone amount determined from spectral measurem
ents differs from the results of the Dobson instrument by -1.1+/-0.9 %
and from those of the Brewer instrument by -0.4+/-0.7 %.