Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at Juliusruh

<p>Understanding ionospheric dependence on solar activity is crucial for comprehension of the upper atmosphere. The response of the ionosphere to solar extreme ultraviolet (EUV) flux has previously been considered stable. Subsequent studies have revealed long-term changes that are not yet full...

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Main Authors: M. G. Tan Jun Rios, C. Borries, H. Liu, J. Mielich
Format: Article
Language:English
Published: Copernicus Publications 2025-01-01
Series:Annales Geophysicae
Online Access:https://angeo.copernicus.org/articles/43/73/2025/angeo-43-73-2025.pdf
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author M. G. Tan Jun Rios
M. G. Tan Jun Rios
C. Borries
H. Liu
J. Mielich
author_facet M. G. Tan Jun Rios
M. G. Tan Jun Rios
C. Borries
H. Liu
J. Mielich
author_sort M. G. Tan Jun Rios
collection DOAJ
description <p>Understanding ionospheric dependence on solar activity is crucial for comprehension of the upper atmosphere. The response of the ionosphere to solar extreme ultraviolet (EUV) flux has previously been considered stable. Subsequent studies have revealed long-term changes that are not yet fully understood. This work evaluates the stability of the ionospheric F2 layer (<i>Nm</i>F2) dependence on solar EUV indices throughout different solar cycles (SCs).</p> <p>Hourly values of the peak electron density of <i>Nm</i>F2 from Juliusruh station (54.6° N, 13.4° E) are analyzed between 1957 and 2023. Geomagnetic perturbations are removed. Third-degree polynomial-fit models dependent on different solar EUV proxies (MgII, F30, and F10.7) are generated separately for each solar cycle, each season, and each local time (LT) hour.</p> <p>The saturation effect is visible in our data and starts at lower F30 values in the ascending phase than in the descending phase. A highly pronounced local time dependence in January with the <span class="inline-formula"><i>R</i><sup>2</sup></span> (goodness of the description for each fit) value being maximum around the noon hours has been observed. The correlation is highest for F30 and MgII, especially under winter noon conditions, supporting the findings of recent studies that they are the best solar flux proxies for describing the <i>Nm</i>F2 dependence at all LT hours. Most importantly, the response of <i>Nm</i>F2 to solar flux shows a clear long-term change as the slopes of the model curves decrease with time for each solar cycle. Between SC20 and SC24, the observed decrease is consistently higher than 2.9 % per decade, reaching 4.4 % per decade at 90 sfu between 1964 and 2019.</p>
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spelling doaj-art-80df6ccc2364437abdf4544c29a224662025-01-21T09:44:31ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762025-01-0143738910.5194/angeo-43-73-2025Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at JuliusruhM. G. Tan Jun Rios0M. G. Tan Jun Rios1C. Borries2H. Liu3J. Mielich4German Aerospace Center, Institute for Solar-Terrestrial Physics, Neustrelitz, GermanyDepartment of Earth and Planetary Science, Kyushu University, Fukuoka, JapanGerman Aerospace Center, Institute for Solar-Terrestrial Physics, Neustrelitz, GermanyDepartment of Earth and Planetary Science, Kyushu University, Fukuoka, JapanDepartment Radar Remote Sensing, Leibniz Institute of Atmospheric Physics, Kühlungsborn, Germany<p>Understanding ionospheric dependence on solar activity is crucial for comprehension of the upper atmosphere. The response of the ionosphere to solar extreme ultraviolet (EUV) flux has previously been considered stable. Subsequent studies have revealed long-term changes that are not yet fully understood. This work evaluates the stability of the ionospheric F2 layer (<i>Nm</i>F2) dependence on solar EUV indices throughout different solar cycles (SCs).</p> <p>Hourly values of the peak electron density of <i>Nm</i>F2 from Juliusruh station (54.6° N, 13.4° E) are analyzed between 1957 and 2023. Geomagnetic perturbations are removed. Third-degree polynomial-fit models dependent on different solar EUV proxies (MgII, F30, and F10.7) are generated separately for each solar cycle, each season, and each local time (LT) hour.</p> <p>The saturation effect is visible in our data and starts at lower F30 values in the ascending phase than in the descending phase. A highly pronounced local time dependence in January with the <span class="inline-formula"><i>R</i><sup>2</sup></span> (goodness of the description for each fit) value being maximum around the noon hours has been observed. The correlation is highest for F30 and MgII, especially under winter noon conditions, supporting the findings of recent studies that they are the best solar flux proxies for describing the <i>Nm</i>F2 dependence at all LT hours. Most importantly, the response of <i>Nm</i>F2 to solar flux shows a clear long-term change as the slopes of the model curves decrease with time for each solar cycle. Between SC20 and SC24, the observed decrease is consistently higher than 2.9 % per decade, reaching 4.4 % per decade at 90 sfu between 1964 and 2019.</p>https://angeo.copernicus.org/articles/43/73/2025/angeo-43-73-2025.pdf
spellingShingle M. G. Tan Jun Rios
M. G. Tan Jun Rios
C. Borries
H. Liu
J. Mielich
Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at Juliusruh
Annales Geophysicae
title Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at Juliusruh
title_full Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at Juliusruh
title_fullStr Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at Juliusruh
title_full_unstemmed Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at Juliusruh
title_short Long-term changes in the dependence of <i>Nm</i>F2 on solar flux at Juliusruh
title_sort long term changes in the dependence of i nm i f2 on solar flux at juliusruh
url https://angeo.copernicus.org/articles/43/73/2025/angeo-43-73-2025.pdf
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