The significance of meteoric ionisation for the propagation of lightning spherics in the atmosphere of Titan

Mathematics

Scientific paper

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Atmospheric Ionization, Lightning, Satellite Atmospheres, Titan, Wave Propagation, Mathematical Models, Meteor Trails

Scientific paper

The meteoric layer hypothesis which states that the precipitation of meteorites is the likely mechanics for the generation of an ionized layer at an altitude of 500 to 600 km above Titan is checked against constraints imposed by space observations. It was considered that the absence of electrophilic species in the atmosphere of Titan, an efficient charge exchange mechanism between ambient ions and metallic ions of meteoric origin and the low coefficient which characterizes the radiative recombination of atomic ions might be responsible for the existence of a dense plasma layer that would prevent the upward escape of electromagnetic waves with frequencies of up to several MHz. However, no ionization layers and no lightning spherics were detected when Voyager 1 approached Titan in Nov. 1980.

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