Abstract
The polar ionosphere is basically different from the mid-latitude ionosphere, because it is tied up with the magneto- sphere. Particle fluxes and electric fields originating in the magnetosphere penetrate into the ionosphere and affect production, loss and transport of ionization there. Some of the polar F-region phenomena, as troughs, polar cap ionization etc. are discussed in the light of these processes.
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© 1980 D. Reidel Publishing Company
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Kohl, H. (1980). The Polar F-Region — Theory. In: Deehr, C.S., Holtet, J.A. (eds) Exploration of the Polar Upper Atmosphere. NATO Advanced Study Institutes Series, vol 64. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-8417-2_4
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DOI: https://doi.org/10.1007/978-94-009-8417-2_4
Publisher Name: Springer, Dordrecht
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