Study of the structure of a meteor complex near the earth's orbit. I - Description of the model

Astronomy and Astrophysics – Astronomy

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Earth Orbits, Meteoroid Concentration, Meteoroid Dust Clouds, Meteoroid Showers, Comets, Hyperbolic Functions

Scientific paper

A model is defined for the distribution of meteor material in space. Most meteors, having masses no more than one gram, are assumed to be cometary material, boiled from the surface by solar radiation. Planetary perturbations eventually disturb the shapes and paths of elliptical swarms which form around the cometary nuclei and are dragged backward and distorted in the tails. All meteor material is assumed to originate in the solar system. The distribution of the particles is shown to converge asymptotically to a Tsipfa-Patero distribution, i.e., a hyperbolic intensity distribution affected by concentration and dispersion factors. The distribution is non-gaussian, and is valid only for complex systems, and in the case of the meteor swarms, must be validated experimentally.

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