Model Calculations of Ozone Content in the Atmosphere by Earth’s Outgoing Radiation

The model of the atmosphere in the form of a sequence of homogeneous layers 100 meters thick from the surface of the Earth to a height of 40 kilometers is considered. Layer parameters are defined for the standard atmosphere. Spectral sections 1002–1003 and 1020–1021 cm^–1 with opposite dependence of ozone absorption coefficient on its temperature change are selected. This model was transformed into one efficient homogeneous layer. The contribution to the outgoing radiation of the atmosphere in the selected spectral regions of the ozone absorption band (1002–1003 and 1020–1021 cm^–1) is equal to the contributions to the outgoing radiation of the Earth by all non-uniform layers constituting them. The possibility of adjusting the temperature of the Earth’s underlying surface is shown. The method of calculating the ozone content in the atmosphere by the outgoing radiation of the Earth is considered.