What can be deduced from sporadic-E data

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What can be deduced from sporadic-E data

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The results of fundamental work based on the large amount of vertical sounding data, suggest a regular behaviour for the sporadic-E (Es) layer. In order to check the regularity of the Es layer appearance, a statistical analysis of its parameters, recorded by hourly ionospheric sounding at Grocka (44.6°N, 20.8°E), from 1978-1982, was carried out. A method for the determination of the local neutral wind pattern from the diurnal distribution of Es layer heights, is proposed. (6 pages)

Inspec keywords: atmospheric techniques; remote sensing by radar; wind; atmospheric structure; sporadic-E layer; thermosphere

Subjects: Instrumentation and techniques for aeronomy, space physics, and cosmic rays; Ionospheric structure; Radar equipment, systems and applications; Tides, waves, winds, and circulation in the upper atmosphere; Atmospheric, ionospheric and magnetospheric techniques and equipment; Radiowave and rocket soundings of the ionosphere; E-region

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