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ω 0 retrievedfromthe
ground observation data: a inArctic, 1979 and b in St. Petersburg suburb (city Petrodvorets),
1996
Fig. 7.7a,b. Spectral dependence of single scattering co-albedo 1 -
τ 0 retrieved from the data of the ground
observations in Arctic: experiment 11 - 13 August 1979 and experiment 12 - 08 October
1979
Fig. 7.8. Spectral dependence of optical thickness
7.3.2
Data Processing of Satellite Observations
τ
ω
Optical thickness
0 for extended clouds
were obtained with inverse asymptotic formulas [(6.13), (6.28)]. The approx-
imate accounting of the horizontal inhomogeneity including the scattering of
radiation by the upper atmospheric layers was accomplished with (6.36) and
(6.39). Multidirectional reflected radiance measurements with the POLDER
0 and single scattering co-albedo 1−
 
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