Calculation of diffusion coefficient for meteor trails and artificial luminous clouds

Statistics – Computation

Scientific paper

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Artificial Clouds, Diffusion Coefficient, Meteor Trails, Monte Carlo Method, Photons, Radiative Transfer, Mean Free Path, Optical Thickness, Particle Density (Concentration), Radiant Flux Density, Solar Radiation, Upper Atmosphere

Scientific paper

Radiative transfer processes in an artificial cloud are studied on the assumption that the contaminant distribution in the cloud is radially symmetric, and the transfer equation is solved by the Monte Carlo method. Simulation of the history of an individual photon in the cloud, which is divided into elementary random events, such as selection of interaction spot, selection of direction of motion following reemission, selection of mean free path to next collision, etc., is the basis of the computational algorithm using the Monte Carlo method. By summing the number of reemission events occurring in different sections of the artificial formation, it is possible to obtain isophots and emission intensity profiles of a given formation illuminated by the sun at a particular moment of time.

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