Titlebook: Global Energetics of the Atmosphere; Earth–Atmosphere Equ Boris M. Smirnov Book 2021 The Editor(s) (if applicable) and The Author(s), under

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Greenhouse Effect in Varying Atmosphere,framework of the above model for standard atmosphere which uses the line-by-line method and parameters for radiative transitions of atmospheric molecules from the HITRAN data bank. Interaction between optically active molecules of the atmosphere through the radiation field is governed by the Kirchho

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Emission of Atmospheric Particles, characterized by a sharp boundary. The mass of atmospheric condensed water in clouds in the form of water microdroplets follows from the analysis of passage of infrared radiation through the atmosphere, as well as from scattering of solar radiation by the atmosphere on the basis of the Fresnel theo

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Equilibrium Radiation of Earth and Venus,ationarity. In addition, in the first approximation, atmospheric regions which are responsible for atmospheric emission to the Earth’s surface and outside are separated. The power of solar radiation absorbed at each point of the globe is characterized by day and season oscillations. The equilibrium

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Physical Aspects of Climate Change, For simplicity, one parameter is used usually for this goal—the global temperature that is the temperature of the Earth’s surface averaged over the globe and time. An important factor of a change of the global temperature in time is the intensity of solar radiation that penetrates in the Earth’s at