On non-isothermicity of meteoric trails

Details On non-isothermicity of meteoric trails On non-isothermicity of meteoric trails

Dec 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975avest...9..232d&link_type=abstract

Astronomicheskii Vestnik, vol. 9, Oct.-Dec. 1975, p. 232-236. In Russian.

Physics

1

Fresnel Region, Meteor Trails, Meteoroid Concentration, Radio Meteors, Atmospheric Physics, Diffusion Coefficient, Radio Echoes, Radio Probing, Time Dependence, Upper Atmosphere

Scientific paper

On the basis of experimental data it has been shown that the diffusion coefficient of meteoric trail D changes considerably during the existence of radio-echo recorded from an unsaturated meteoric trail. A law of the change of value D in time has been established. It has been shown that the decrease of D ceases approximately in 0.17 sec after the formation of the first Fresnel zone.

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