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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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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1766116280821088256 |