Long-term trends in the ionospheric F2 region with different solar activity indices

A new comprehensive data collection by Damboldt and Suessmann (2012a) with monthly <I>fo</I>F2 and M(3000)F2 median values is an excellent basis for the derivation of long-term trends in the ionospheric F2 region. Ionospheric trends have been derived only for stations with data serie...

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Main Authors: J. Mielich, J. Bremer
Format: Article
Language:English
Published: Copernicus Publications 2013-02-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/31/291/2013/angeo-31-291-2013.pdf
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spelling doaj-ce1aee9924cc4a3ebb234804f65a50d32020-11-24T22:40:16ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762013-02-013129130310.5194/angeo-31-291-2013Long-term trends in the ionospheric F2 region with different solar activity indicesJ. Mielich0J. Bremer1Leibniz-Institute of Atmospheric Physics at the Rostock University, Schloss-Str. 6, 18225 Kühlungsborn, GermanyLeibniz-Institute of Atmospheric Physics at the Rostock University, Schloss-Str. 6, 18225 Kühlungsborn, GermanyA new comprehensive data collection by Damboldt and Suessmann (2012a) with monthly <I>fo</I>F2 and M(3000)F2 median values is an excellent basis for the derivation of long-term trends in the ionospheric F2 region. Ionospheric trends have been derived only for stations with data series of at least 22 years (124 stations with <I>fo</I>F2 data and 113 stations with M(3000)F2 data) using a twofold regression analysis depending on solar and geomagnetic activity. <br><br> Three main results have been derived: <br><br> Firstly, it could be shown that the solar 10.7 cm radio flux F10.7 is a better index for the description of the solar activity than the relative solar sunspot number <I>R</I> as well as the solar EUV proxy E10.7. <br><br> Secondly, the global mean <I>fo</I>F2 and <I>hm</I>F2 trends derived for the interval between 1948 and 2006 are in surprisingly good agreement with model calculations of an increasing atmospheric greenhouse effect (Rishbeth and Roble, 1992). <br><br> Thirdly, during the years 2007 until 2009, the <I>hm</I>F2 values and to a smaller amount the <I>fo</I>F2 values strongly decrease. The reason for this effect is a reduction of the thermospheric density and ionization due to a markedly reduced solar EUV irradiation and extremely small geomagnetic activity during the solar cycle 23/24 minimum.https://www.ann-geophys.net/31/291/2013/angeo-31-291-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Mielich
J. Bremer
spellingShingle J. Mielich
J. Bremer
Long-term trends in the ionospheric F2 region with different solar activity indices
Annales Geophysicae
author_facet J. Mielich
J. Bremer
author_sort J. Mielich
title Long-term trends in the ionospheric F2 region with different solar activity indices
title_short Long-term trends in the ionospheric F2 region with different solar activity indices
title_full Long-term trends in the ionospheric F2 region with different solar activity indices
title_fullStr Long-term trends in the ionospheric F2 region with different solar activity indices
title_full_unstemmed Long-term trends in the ionospheric F2 region with different solar activity indices
title_sort long-term trends in the ionospheric f2 region with different solar activity indices
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2013-02-01
description A new comprehensive data collection by Damboldt and Suessmann (2012a) with monthly <I>fo</I>F2 and M(3000)F2 median values is an excellent basis for the derivation of long-term trends in the ionospheric F2 region. Ionospheric trends have been derived only for stations with data series of at least 22 years (124 stations with <I>fo</I>F2 data and 113 stations with M(3000)F2 data) using a twofold regression analysis depending on solar and geomagnetic activity. <br><br> Three main results have been derived: <br><br> Firstly, it could be shown that the solar 10.7 cm radio flux F10.7 is a better index for the description of the solar activity than the relative solar sunspot number <I>R</I> as well as the solar EUV proxy E10.7. <br><br> Secondly, the global mean <I>fo</I>F2 and <I>hm</I>F2 trends derived for the interval between 1948 and 2006 are in surprisingly good agreement with model calculations of an increasing atmospheric greenhouse effect (Rishbeth and Roble, 1992). <br><br> Thirdly, during the years 2007 until 2009, the <I>hm</I>F2 values and to a smaller amount the <I>fo</I>F2 values strongly decrease. The reason for this effect is a reduction of the thermospheric density and ionization due to a markedly reduced solar EUV irradiation and extremely small geomagnetic activity during the solar cycle 23/24 minimum.
url https://www.ann-geophys.net/31/291/2013/angeo-31-291-2013.pdf
work_keys_str_mv AT jmielich longtermtrendsintheionosphericf2regionwithdifferentsolaractivityindices
AT jbremer longtermtrendsintheionosphericf2regionwithdifferentsolaractivityindices
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