On apparent changes in the ambipolar diffusion coefficient determined from radio-meteor echoes

Details On apparent changes in the ambipolar diffusion coefficient determined from radio-meteor echoes On apparent changes in the ambipolar diffusion coefficient determined from radio-meteor echoes

Jan 1980

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980jatp...42...69p&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 42, Jan. 1980, p. 69-72.

Physics

Ambipolar Diffusion, Diffusion Coefficient, Radio Echoes, Radio Meteors, Decay Rates, Electron Energy, Meteor Trails, Wave Reflection

Scientific paper

The predicted cooling times for meteor train electrons in a recent calculation (Baggaley and Webb, 1977) are an order of magnitude smaller than the experimental values of Delov (1975). Delov's results are based on the apparent variation with time of the ambipolar diffusion coefficient deduced from the decay rate of radio-meteor echoes. An alternative explanation for this apparent variation is presented as being due to radio wave reflection processes. Additional experiments are suggested which may be used to determine the source of this effect.

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