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Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals

This work is devoted to the construction of a locally one-dimensional difference scheme for calculating the first boundary value problem for a general parabolic equation for the mass distribution function of ice particles. The functions are introduced such that and give at each point at time the con...

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Главные авторы: Khibiev, A. H., Хибиев, А. Х.
Формат: Статья
Язык:English
Опубликовано: Pleiades Publishing 2025
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Online-ссылка:https://dspace.ncfu.ru/handle/123456789/30362
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spelling ir-123456789-303622025-04-02T11:51:54Z Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals Khibiev, A. H. Хибиев, А. Х. Approximation error Stability Difference scheme Convergence of the scheme Boundary value problem This work is devoted to the construction of a locally one-dimensional difference scheme for calculating the first boundary value problem for a general parabolic equation for the mass distribution function of ice particles. The functions are introduced such that and give at each point at time the concentration of cloud droplets and ice particles, respectively, whose mass is in the range from to The equation is written with respect to the function ; the function (the droplet mass distribution function) is given in the equation. The equation is part of a system of integro-differential equations for the mass distribution functions of droplets and ice particles describing microphysical processes in convective clouds against the background of a given thermohydrodynamics. A locally one-dimensional difference scheme for a general parabolic equation in a ‑dimensional parallelepiped is constructed by the method of total approximation. To describe the interaction of droplets and crystals, nonlocal (nonlinear) integral sources are included in the equation. Using energy inequalities, an a priori estimate is obtained, from which follows the stability and convergence of the difference scheme. The results of the work will be used to build a model of microphysical processes in mixed convective clouds, which will be used to conduct research in topical areas such as the study of the role of the system properties of clouds in the formation of their microstructural characteristics and the development of technology for managing precipitation processes in convective clouds by introducing particles of ice-forming reagents. 2025-04-02T11:50:20Z 2025-04-02T11:50:20Z 2024 Статья Ashabokov B.A., Khibiev A.K., Shkhanukov-Lafishev M.K. Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals // Theoretical Foundations of Chemical Engineering. - 2024. - 58 (5). - pp. 1745 - 1751. - DOI: 10.1134/S0040579525600457 https://dspace.ncfu.ru/handle/123456789/30362 en Theoretical Foundations of Chemical Engineering application/pdf application/pdf Pleiades Publishing
institution СКФУ
collection Репозиторий
language English
topic Approximation error
Stability
Difference scheme
Convergence of the scheme
Boundary value problem
spellingShingle Approximation error
Stability
Difference scheme
Convergence of the scheme
Boundary value problem
Khibiev, A. H.
Хибиев, А. Х.
Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals
description This work is devoted to the construction of a locally one-dimensional difference scheme for calculating the first boundary value problem for a general parabolic equation for the mass distribution function of ice particles. The functions are introduced such that and give at each point at time the concentration of cloud droplets and ice particles, respectively, whose mass is in the range from to The equation is written with respect to the function ; the function (the droplet mass distribution function) is given in the equation. The equation is part of a system of integro-differential equations for the mass distribution functions of droplets and ice particles describing microphysical processes in convective clouds against the background of a given thermohydrodynamics. A locally one-dimensional difference scheme for a general parabolic equation in a ‑dimensional parallelepiped is constructed by the method of total approximation. To describe the interaction of droplets and crystals, nonlocal (nonlinear) integral sources are included in the equation. Using energy inequalities, an a priori estimate is obtained, from which follows the stability and convergence of the difference scheme. The results of the work will be used to build a model of microphysical processes in mixed convective clouds, which will be used to conduct research in topical areas such as the study of the role of the system properties of clouds in the formation of their microstructural characteristics and the development of technology for managing precipitation processes in convective clouds by introducing particles of ice-forming reagents.
format Статья
author Khibiev, A. H.
Хибиев, А. Х.
author_facet Khibiev, A. H.
Хибиев, А. Х.
author_sort Khibiev, A. H.
title Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals
title_short Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals
title_full Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals
title_fullStr Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals
title_full_unstemmed Locally One-Dimensional Scheme for the Distribution Function Equation by Ice Particle Masses Considering the Interaction of Droplets and Crystals
title_sort locally one-dimensional scheme for the distribution function equation by ice particle masses considering the interaction of droplets and crystals
publisher Pleiades Publishing
publishDate 2025
url https://dspace.ncfu.ru/handle/123456789/30362
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