Electron density in the F1 layer over Norilsk in 2007–2014

We report the results of the analysis of annual variations in daily electron density (N) for various solar activity conditions — minimum, rise, and maximum (2007–2014) — obtained from digisonde measurements at the ionospheric station Norilsk (69.4° N, 88.1° E). New coefficients of the known semi-emp...

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Published in:Solar-Terrestrial Physics
Main Authors: Kushnarenko G.P., Yakovleva O.E., Kuznetsova G.M.
Format: Article in Journal/Newspaper
Language:English
Published: INFRA-M 2019
Subjects:
Online Access:https://doi.org/10.12737/stp-52201915
https://doaj.org/article/a44df5201b784ed8bf7715863b689751
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spelling ftdoajarticles:oai:doaj.org/article:a44df5201b784ed8bf7715863b689751 2023-05-15T17:24:59+02:00 Electron density in the F1 layer over Norilsk in 2007–2014 Kushnarenko G.P. Yakovleva O.E. Kuznetsova G.M. 2019-06-01T00:00:00Z https://doi.org/10.12737/stp-52201915 https://doaj.org/article/a44df5201b784ed8bf7715863b689751 EN eng INFRA-M https://naukaru.ru/en/nauka/article/29514/view https://doaj.org/toc/2500-0535 doi:10.12737/stp-52201915 2500-0535 https://doaj.org/article/a44df5201b784ed8bf7715863b689751 Solar-Terrestrial Physics, Vol 5, Iss 2, Pp 109-112 (2019) annual variations electron density semi-empirical model Astrophysics QB460-466 article 2019 ftdoajarticles https://doi.org/10.12737/stp-52201915 2022-12-31T01:59:17Z We report the results of the analysis of annual variations in daily electron density (N) for various solar activity conditions — minimum, rise, and maximum (2007–2014) — obtained from digisonde measurements at the ionospheric station Norilsk (69.4° N, 88.1° E). New coefficients of the known semi-empirical model (SEM) describing the connection between N and thermosphere characteristics are calculated to identify regularities of these variations exactly at Norilsk station. The height changes of annual variations in the noon electron density N are obtained in the F1 region (120–200 km). The experimental data approximation describes N quite satisfactorily at these heights in the daytime of different seasons under different solar activity conditions. It is shown that in the years of solar minimum at all heights of the F1 layer the tendency remains for maximum N in summer and for minimum N in winter. In later years and in the year of maximum solar activity, a characteristic feature of the behavior of N is the change in the phase of the annual variation by 180° in the range of heights from 170 to180 km: maximum N is observed in winter; and minimum, in summer. Article in Journal/Newspaper norilsk Directory of Open Access Journals: DOAJ Articles Norilsk ENVELOPE(88.203,88.203,69.354,69.354) Solar-Terrestrial Physics 5 2 109 112
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic annual variations
electron density
semi-empirical model
Astrophysics
QB460-466
spellingShingle annual variations
electron density
semi-empirical model
Astrophysics
QB460-466
Kushnarenko G.P.
Yakovleva O.E.
Kuznetsova G.M.
Electron density in the F1 layer over Norilsk in 2007–2014
topic_facet annual variations
electron density
semi-empirical model
Astrophysics
QB460-466
description We report the results of the analysis of annual variations in daily electron density (N) for various solar activity conditions — minimum, rise, and maximum (2007–2014) — obtained from digisonde measurements at the ionospheric station Norilsk (69.4° N, 88.1° E). New coefficients of the known semi-empirical model (SEM) describing the connection between N and thermosphere characteristics are calculated to identify regularities of these variations exactly at Norilsk station. The height changes of annual variations in the noon electron density N are obtained in the F1 region (120–200 km). The experimental data approximation describes N quite satisfactorily at these heights in the daytime of different seasons under different solar activity conditions. It is shown that in the years of solar minimum at all heights of the F1 layer the tendency remains for maximum N in summer and for minimum N in winter. In later years and in the year of maximum solar activity, a characteristic feature of the behavior of N is the change in the phase of the annual variation by 180° in the range of heights from 170 to180 km: maximum N is observed in winter; and minimum, in summer.
format Article in Journal/Newspaper
author Kushnarenko G.P.
Yakovleva O.E.
Kuznetsova G.M.
author_facet Kushnarenko G.P.
Yakovleva O.E.
Kuznetsova G.M.
author_sort Kushnarenko G.P.
title Electron density in the F1 layer over Norilsk in 2007–2014
title_short Electron density in the F1 layer over Norilsk in 2007–2014
title_full Electron density in the F1 layer over Norilsk in 2007–2014
title_fullStr Electron density in the F1 layer over Norilsk in 2007–2014
title_full_unstemmed Electron density in the F1 layer over Norilsk in 2007–2014
title_sort electron density in the f1 layer over norilsk in 2007–2014
publisher INFRA-M
publishDate 2019
url https://doi.org/10.12737/stp-52201915
https://doaj.org/article/a44df5201b784ed8bf7715863b689751
long_lat ENVELOPE(88.203,88.203,69.354,69.354)
geographic Norilsk
geographic_facet Norilsk
genre norilsk
genre_facet norilsk
op_source Solar-Terrestrial Physics, Vol 5, Iss 2, Pp 109-112 (2019)
op_relation https://naukaru.ru/en/nauka/article/29514/view
https://doaj.org/toc/2500-0535
doi:10.12737/stp-52201915
2500-0535
https://doaj.org/article/a44df5201b784ed8bf7715863b689751
op_doi https://doi.org/10.12737/stp-52201915
container_title Solar-Terrestrial Physics
container_volume 5
container_issue 2
container_start_page 109
op_container_end_page 112
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