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

  • PHYSICAL BASES AND METHODS OF STUDYING THE EARTH FROM SPACE
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Abstract

The model of the atmosphere in the form of a sequence of homogeneous layers 100 m in thickness from the surface of the Earth to a height of 40 km is considered. Layer parameters are defined for the standard atmosphere. Spectral sections of 1002–1003 and 1020–1021 cm0–1 with an 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 nonuniform 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.

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Funding

The work was carried out as part of the State Task of the Zuev Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences.

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  1. V.E. Zuev Institute of Atmospheric Optics, Siberian Branch, Russian Academy of Sciences, Tomsk, Russia

    S. A. Shishigin

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  1. S. A. Shishigin
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Correspondence to S. A. Shishigin.

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Shishigin, S.A. Model Calculations of Ozone Content in the Atmosphere by Earth’s Outgoing Radiation. Izv. Atmos. Ocean. Phys. 59, 1180–1188 (2023). https://doi.org/10.1134/S0001433823090189

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