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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Emission of Atmospheric Particles, smog and also they are responsible partially for absorption and reflection of solar radiation. Aerosols of the specific mass of the order of . are able to change remarkably the global temperature. If they are injected in the stratosphere as a result of volcano eruptions or nuclear explosions, they

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Physical Aspects of Climate Change,olution of the Earth’s temperature. In particular, the difference between the maximal and minimal temperatures in the course of Earth’s evolution is almost 20 .C that by one order of magnitude exceeds the corresponding value that is the basis of the Paris agreement 2015 on climate. The influence of

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Pierre-André Buigues,Khalid Sekkatinds. The first parcel of the mixture contains wet air from near-surface altitudes and the second one consists of cold air from high altitudes. The threshold of this process and optimal conditions are analyzed. Atmospheric winds are of importance both for formation of a supersaturated water vapor in

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Mario Baldassarri (Professor of Economics)he atmosphere and Earth’s surface, absorption and emission of infrared radiation by the Earth and atmosphere, and heat transport from the Earth to the atmosphere through air convection and due to water evaporation from the Earth’s surface and its condensation in the atmosphere. Global energetic flux

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Primal Representations of the Technology,as due to water microdroplets which constitute the clouds. Since the emission spectrum of the atmosphere consists mostly of individual broaden spectral lines due to vibration–rotation and rotation states of molecules, the infrared atmospheric spectrum consists of thousands broaden peaks. Therefore,