Analysis of Radiative Observations in Cloudy Atmosphere - Short-Wave Solar Radiation in the Earth's Atmosphere - page 242

λ = µ Fig. 7.5. Vertical profiles of the volume scattering coefficient for wavelength 0.55 m

retrieved from airborne radiative experiments 6 and 7

Fig. 7.6. Vertical profiles of the volume absorption coefficient retrieved from airborne ra-
diative experiments 6 and 7 for wavelengths

µ m indicated in figure

7.3.1
Data Processing of Ground Observations

Two experiments of the ground observations have been processed with (6.17).
The first experiment has been performed using spectrometer K-2 (see Sect. 3.2)
under overcast conditions at drifting Arctic station SP-22 on the 13th August
and 8th October 1979 with the error of the transmitted radiance measure-
ments within 3% (Radionov et al. 1981). There were extended, horizontally