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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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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