{"title":"Model Calculations of Ozone Content in the Atmosphere by Earth’s Outgoing Radiation","authors":"S. A. Shishigin","doi":"10.1134/s0001433823090189","DOIUrl":null,"url":null,"abstract":"<h3 data-test=\"abstract-sub-heading\">Abstract</h3><p>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<sup>–1</sup> 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<sup>–1</sup>) 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.</p>","PeriodicalId":54911,"journal":{"name":"Izvestiya Atmospheric and Oceanic Physics","volume":"14 1","pages":""},"PeriodicalIF":0.9000,"publicationDate":"2024-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Izvestiya Atmospheric and Oceanic Physics","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1134/s0001433823090189","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
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.
期刊介绍：
Izvestiya, Atmospheric and Oceanic Physics is a journal that publishes original scientific research and review articles on vital issues in the physics of the Earth’s atmosphere and hydrosphere and climate theory. The journal presents results of recent studies of physical processes in the atmosphere and ocean that control climate, weather, and their changes. These studies have possible practical applications. The journal also gives room to the discussion of results obtained in theoretical and experimental studies in various fields of oceanic and atmospheric physics, such as the dynamics of gas and water media, interaction of the atmosphere with the ocean and land surfaces, turbulence theory, heat balance and radiation processes, remote sensing and optics of both media, natural and man-induced climate changes, and the state of the atmosphere and ocean. The journal publishes papers on research techniques used in both media, current scientific information on domestic and foreign events in the physics of the atmosphere and ocean.
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