Solar activity effects in the ionospheric D region

Variations in the D-region electron concentration within the solar activity cycle are considered. It is demonstrated that conclusions of various authors, who have analyzed various sets of experimental data on [e], differ significantly. The most reliable seem to be the conclusions based on analys...

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Main Author: A. D. Danilov
Format: Article
Language:English
Published: Copernicus Publications 1998-12-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/16/1527/1998/angeo-16-1527-1998.pdf
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author A. D. Danilov
author_facet A. D. Danilov
author_sort A. D. Danilov
collection DOAJ
description Variations in the D-region electron concentration within the solar activity cycle are considered. It is demonstrated that conclusions of various authors, who have analyzed various sets of experimental data on [e], differ significantly. The most reliable seem to be the conclusions based on analysis of the [e] measurements carried out by the Faraday rotation method and on the theoretical concepts on the D-region photochemistry. Possible QBO effects in the relation of [e] to solar activity are considered and an assumption is made that such effects may be the reason for the aforementioned disagreement in conclusions on the [e] relation to solar indices.<br><br><b>Key words.</b> Atmospheric composition and structure · Ion chemistry of the atmosphere · Middle atmosphere
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spelling doaj.art-046646209c404443bf177e84ccda39cb2022-12-21T23:03:04ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761998-12-01161527153310.1007/s00585-998-1527-2Solar activity effects in the ionospheric D regionA. D. Danilov0Institute of Applied Geophysics, Rostokinskaya 9, Moscow 128 129, Russia Fax: + 7 095 187 75 13; e-mail: geophys@sovam.comVariations in the D-region electron concentration within the solar activity cycle are considered. It is demonstrated that conclusions of various authors, who have analyzed various sets of experimental data on [e], differ significantly. The most reliable seem to be the conclusions based on analysis of the [e] measurements carried out by the Faraday rotation method and on the theoretical concepts on the D-region photochemistry. Possible QBO effects in the relation of [e] to solar activity are considered and an assumption is made that such effects may be the reason for the aforementioned disagreement in conclusions on the [e] relation to solar indices.<br><br><b>Key words.</b> Atmospheric composition and structure · Ion chemistry of the atmosphere · Middle atmospherehttps://www.ann-geophys.net/16/1527/1998/angeo-16-1527-1998.pdf
spellingShingle A. D. Danilov
Solar activity effects in the ionospheric D region
Annales Geophysicae
title Solar activity effects in the ionospheric D region
title_full Solar activity effects in the ionospheric D region
title_fullStr Solar activity effects in the ionospheric D region
title_full_unstemmed Solar activity effects in the ionospheric D region
title_short Solar activity effects in the ionospheric D region
title_sort solar activity effects in the ionospheric d region
url https://www.ann-geophys.net/16/1527/1998/angeo-16-1527-1998.pdf
work_keys_str_mv AT addanilov solaractivityeffectsintheionosphericdregion