通过地球向外辐射计算大气中的臭氧含量模型

IF 0.9 4区地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES Izvestiya Atmospheric and Oceanic Physics Pub Date : 2024-01-31 DOI:10.1134/s0001433823090189

S. A. Shishigin

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引用次数: 0

摘要

摘要研究了从地球表面到 40 千米高处厚度为 100 米的一系列均质层形式的大气模型。层参数是为标准大气层定义的。选择了 1002-1003 和 1020-1021 cm0-1 光谱段，臭氧吸收系数与温度变化的关系相反。该模型被转化为一个有效的均质层。在选定的臭氧吸收带光谱区（1002-1003 和 1020-1021 厘米-1），大气层的外辐射量等于构成这些光谱区的所有非均匀层对地球外辐射量的贡献。显示了调整地球底层表面温度的可能性。考虑了通过地球外向辐射计算大气中臭氧含量的方法。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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

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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来源期刊

Izvestiya Atmospheric and Oceanic Physics 地学-海洋学

CiteScore

1.40

自引率

28.60%

发文量

审稿时长

6-12 weeks

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.