The latitudinal variation of ionospheric absorption

Details The latitudinal variation of ionospheric absorption The latitudinal variation of ionospheric absorption

Jan 1981

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1981jatp...43...59c&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 43, Jan. 1981, p. 59-63. Research supported by the University Grants Commi

Physics

3

Electromagnetic Absorption, Geomagnetic Latitude, Ionospheric Propagation, Equatorial Atmosphere, Incidence, Radio Wave Refraction, Refractivity

Scientific paper

The observed latitudinal variation in vertical incidence ionospheric absorption is explained as a purely geomagnetic effect. The quasitransverse (QT) zone contribution to total absorption in the equatorial zone dominates, producing an increase in absorption with higher dip angle values; for angles larger than 20 deg, the quasilongitudinal zone contribution dominates over the QT zone input, decreasing absorption with increasing dip angles.

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