Abstract
Abstract The model proposed provides for reconstruction of the aerosol scattering coefficient profile. In so doing, one needs as input data the scattering coefficient value of the dry aerosol substance at the near-ground level measured at the wavelength of 0.52 μm, relative air humidity, aerosol optical thickness, and mean temperature of air in the lower troposphere. The model allows for the correlation between the values of the scattering coefficient at different altitudes, as well as the dependence of the height of the mixing layer on the heating of the lower atmospheric layers. The errors in reconstructing the vertical profiles of the aerosol scattering coefficient are analyzed for different ways of taking into account the external factors and input parameters. It is shown that the use of such an approach provides a decrease in the rms error in reconstruction even at this stage by approximately 30% for winter and by 3 to 4 times for summer in comparison with the rms deviation of this parameter in the i...
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