Self-similar regime in the formation of the atmospheric submicron aerosol

Physics

Scientific paper

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Aerosols, Air Pollution, Atmospheric Physics, Particle Size Distribution, Similarity Theorem, Asymptotic Properties, Coagulation, Condensing, Kinetic Equations, Particle Mass, Planetary Atmospheres, Stratosphere, Troposphere

Scientific paper

The possibility of using the self-similarity principle to analyze the kinetics of condensation-coagulation processes in submicron atmospheric aerosol is examined. The conditions associated with the evolution of the self-similar regime in the asymptotic stage of the aerosol mass spectrum evolution are defined; those include the power-law change of the mass of particles due to condensational growth and the homogeneity of the kernel of the kinetic coagulation equation. The spectrum of the self-similar regime is a wave moving with respect to time, with its left portion equal to zero. The results presented can be used directly to describe the submicron-component evolution for the tropospheric and stratospheric aerosols in the earth atmosphere and the aerosols in the clouds of Venus.

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