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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Main Authors: A. V. Mikhailov, D. Marin, T. Yu. Leschinskaya, M. Herraiz
Format: Article
Language:English
Published: Copernicus Publications 2002-10-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/20/1663/2002/angeo-20-1663-2002.pdf
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spelling 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.&nbsp;</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
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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.&nbsp;</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
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