| Abstract: | A statistical analysis of the variations of the brightness coefficient in the ocean-atmosphere system in the visible band was carried out using the results of remote measurements from the INTERKOSMOS-21 satellite. The variability of the seawater optical parameters and the Rayleigh component of light scattering were eliminated by computing the variations of the signals from the local average values along the route of measurements. The derived spectral dependence of the aerosol scattering component is characterized by a slight increase when the wavelength increases.Translated by Mikhail M. Trufanov. |
