Solar cycle evolution of ULF wave power in solar wind and on ground

The solar cycle evolution of the ultra-low frequency (ULF) power was studied in solar wind and on ground. We aim finding out how the ULF power in interplanetary and on ground magnetic field evolves over the solar cycle 23 (SC23) and how well do they follow each other in monthly time scales. The hour...

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Main Authors: Hynönen Reko, Tanskanen Eija I., Francia Patrizia
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:Journal of Space Weather and Space Climate
Subjects:
Online Access:https://www.swsc-journal.org/articles/swsc/full_html/2020/01/swsc190018/swsc190018.html
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spelling doaj-4c7f3bb135a548628af893a0127b022a2021-04-02T13:33:44ZengEDP SciencesJournal of Space Weather and Space Climate2115-72512020-01-01104310.1051/swsc/2020046swsc190018Solar cycle evolution of ULF wave power in solar wind and on groundHynönen Reko0https://orcid.org/0000-0002-5959-9332Tanskanen Eija I.Francia Patrizia1Department of Electronics and Nanoengineering, Aalto University of TechnologyDipartimento di Scienze Fisiche e Chimiche, Università dell’Aquila, Via Vetoio, CoppitoThe solar cycle evolution of the ultra-low frequency (ULF) power was studied in solar wind and on ground. We aim finding out how the ULF power in interplanetary and on ground magnetic field evolves over the solar cycle 23 (SC23) and how well do they follow each other in monthly time scales. The hourly power of the ULF waves was computed in the Pc5 frequency range 2–7 mHz for years 1998–2008. The highest wave power in SC23 is found to occur in late 2003 and the lowest at the solar minimum. Ground ULF power follows the IMF power and solar wind speed, particularly well during declining phase. The ULF power in winter exceeds the ULF power in other seasons during the declining phase of SC23, while equinoxes dominate in the ascending phase and the solar maximum. The ground ULF power was found to rise with magnetic latitude from 54° to 73°, after which Pc5 power decreases towards the polar cap. The Pc5 power in the auroral zone is larger in the nightside than the dayside due to substorm activity implying that magnetotail processes are an important contributor to the nightside ULF power.https://www.swsc-journal.org/articles/swsc/full_html/2020/01/swsc190018/swsc190018.htmlulf wavessolar cyclespace climategeomagnetic pulsationspc5 waves
collection DOAJ
language English
format Article
sources DOAJ
author Hynönen Reko
Tanskanen Eija I.
Francia Patrizia
spellingShingle Hynönen Reko
Tanskanen Eija I.
Francia Patrizia
Solar cycle evolution of ULF wave power in solar wind and on ground
Journal of Space Weather and Space Climate
ulf waves
solar cycle
space climate
geomagnetic pulsations
pc5 waves
author_facet Hynönen Reko
Tanskanen Eija I.
Francia Patrizia
author_sort Hynönen Reko
title Solar cycle evolution of ULF wave power in solar wind and on ground
title_short Solar cycle evolution of ULF wave power in solar wind and on ground
title_full Solar cycle evolution of ULF wave power in solar wind and on ground
title_fullStr Solar cycle evolution of ULF wave power in solar wind and on ground
title_full_unstemmed Solar cycle evolution of ULF wave power in solar wind and on ground
title_sort solar cycle evolution of ulf wave power in solar wind and on ground
publisher EDP Sciences
series Journal of Space Weather and Space Climate
issn 2115-7251
publishDate 2020-01-01
description The solar cycle evolution of the ultra-low frequency (ULF) power was studied in solar wind and on ground. We aim finding out how the ULF power in interplanetary and on ground magnetic field evolves over the solar cycle 23 (SC23) and how well do they follow each other in monthly time scales. The hourly power of the ULF waves was computed in the Pc5 frequency range 2–7 mHz for years 1998–2008. The highest wave power in SC23 is found to occur in late 2003 and the lowest at the solar minimum. Ground ULF power follows the IMF power and solar wind speed, particularly well during declining phase. The ULF power in winter exceeds the ULF power in other seasons during the declining phase of SC23, while equinoxes dominate in the ascending phase and the solar maximum. The ground ULF power was found to rise with magnetic latitude from 54° to 73°, after which Pc5 power decreases towards the polar cap. The Pc5 power in the auroral zone is larger in the nightside than the dayside due to substorm activity implying that magnetotail processes are an important contributor to the nightside ULF power.
topic ulf waves
solar cycle
space climate
geomagnetic pulsations
pc5 waves
url https://www.swsc-journal.org/articles/swsc/full_html/2020/01/swsc190018/swsc190018.html
work_keys_str_mv AT hynonenreko solarcycleevolutionofulfwavepowerinsolarwindandonground
AT tanskaneneijai solarcycleevolutionofulfwavepowerinsolarwindandonground
AT franciapatrizia solarcycleevolutionofulfwavepowerinsolarwindandonground
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