A revised approach to the ƒ<i>o</i>F2 long-term trends analysis
A new approach to extract <i>fo</i>F2 long-term trends, which are free to a great extent from solar and geomagnetic activity effects, has been proposed. These trends are insensitive to the phase (increasing/decreasing) of geomagnetic activity, with long-term variations being smal...
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doaj-b7360a53daac4fb99b4c0a7744f0322a2020-11-24T22:57:12ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762002-10-01201663167510.5194/angeo-20-1663-2002A revised approach to the ƒ<i>o</i>F2 long-term trends analysisA. V. Mikhailov0A. V. Mikhailov1D. Marin2T. Yu. Leschinskaya3M. Herraiz4Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, Troitsk, Moscow Region 142190, RussiaCorrespondence to: A. V. Mikhailov (avm71@orc.ru)Atmospheric Sounding Station “El Arenosillo", INTA, SpainInstitute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation, Troitsk, Moscow Region 142190, RussiaFaculty of Physics, Complutense University, SpainA new approach to extract <i>fo</i>F2 long-term trends, which are free to a great extent from solar and geomagnetic activity effects, has been proposed. These trends are insensitive to the phase (increasing/decreasing) of geomagnetic activity, with long-term variations being small and insignificant for such relatively short time periods. A small but significant residual <i>fo</i>F2 trend, with the slope <i>K<sub>r</sub></i> = - 2.2 × 10<sup>-4</sup> per year, was obtained over a 55-year period (the longest avail-able) of observations at Slough. Such small trends have no practical importance. On the other hand, negative (although insignificant) residual trends obtained at 10 ionosonde stations for shorter periods (31 years) may be considered as a manifestation of a very long-term geomagnetic activity increase which did take place during the 20th century. All of the revealed <i>fo</i>F2 long-term variations (trends) are shown to have a natural origin related to long-term variations in solar and geomagnetic activity. There is no indication of any manmade <i>fo</i>F2 trends. </p> <p style="line-height: 20px;"><b>Key words.</b> Ionosphere (ionosphere-atmosphere interactions, ionospheric disturbances)https://www.ann-geophys.net/20/1663/2002/angeo-20-1663-2002.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
A. V. Mikhailov A. V. Mikhailov D. Marin T. Yu. Leschinskaya M. Herraiz |
spellingShingle |
A. V. Mikhailov A. V. Mikhailov D. Marin T. Yu. Leschinskaya M. Herraiz A revised approach to the ƒ<i>o</i>F2 long-term trends analysis Annales Geophysicae |
author_facet |
A. V. Mikhailov A. V. Mikhailov D. Marin T. Yu. Leschinskaya M. Herraiz |
author_sort |
A. V. Mikhailov |
title |
A revised approach to the ƒ<i>o</i>F2 long-term trends analysis |
title_short |
A revised approach to the ƒ<i>o</i>F2 long-term trends analysis |
title_full |
A revised approach to the ƒ<i>o</i>F2 long-term trends analysis |
title_fullStr |
A revised approach to the ƒ<i>o</i>F2 long-term trends analysis |
title_full_unstemmed |
A revised approach to the ƒ<i>o</i>F2 long-term trends analysis |
title_sort |
revised approach to the ƒ<i>o</i>f2 long-term trends analysis |
publisher |
Copernicus Publications |
series |
Annales Geophysicae |
issn |
0992-7689 1432-0576 |
publishDate |
2002-10-01 |
description |
A new approach to extract <i>fo</i>F2
long-term trends, which are free to a great extent from solar and geomagnetic
activity effects, has been proposed. These trends are insensitive to the phase
(increasing/decreasing) of geomagnetic activity, with long-term variations
being small and insignificant for such relatively short time periods. A small
but significant residual <i>fo</i>F2 trend, with the slope <i>K<sub>r</sub></i>
= - 2.2 × 10<sup>-4</sup> per year, was obtained over a 55-year period (the
longest avail-able) of observations at Slough. Such small trends have no
practical importance. On the other hand, negative (although insignificant)
residual trends obtained at 10 ionosonde stations for shorter periods (31
years) may be considered as a manifestation of a very long-term geomagnetic
activity increase which did take place during the 20th century. All of the
revealed <i>fo</i>F2 long-term variations (trends) are shown to have a natural
origin related to long-term variations in solar and geomagnetic activity. There
is no indication of any manmade <i>fo</i>F2 trends. </p>
<p style="line-height: 20px;"><b>Key words.</b> Ionosphere (ionosphere-atmosphere
interactions, ionospheric disturbances) |
url |
https://www.ann-geophys.net/20/1663/2002/angeo-20-1663-2002.pdf |
work_keys_str_mv |
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