Universal and local time components in Schumann resonance intensity

We extend the technique suggested by Sentman and Fraser (1991) and discussed by Pechony and Price (2006), the technique for separating the local and universal time variations in the Schumann resonance intensity. Initially, we simulate the resonance oscillations in a uniform Earth-ionosphere cavity w...

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Published in:Annales Geophysicae
Main Authors: A. P. Nickolaenko, M. Hayakawa
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2008
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-26-813-2008
https://doaj.org/article/2716ffef8e394c0ca5c8755d025432ca
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spelling ftdoajarticles:oai:doaj.org/article:2716ffef8e394c0ca5c8755d025432ca 2023-05-15T17:01:08+02:00 Universal and local time components in Schumann resonance intensity A. P. Nickolaenko M. Hayakawa 2008-05-01T00:00:00Z https://doi.org/10.5194/angeo-26-813-2008 https://doaj.org/article/2716ffef8e394c0ca5c8755d025432ca EN eng Copernicus Publications https://www.ann-geophys.net/26/813/2008/angeo-26-813-2008.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-26-813-2008 0992-7689 1432-0576 https://doaj.org/article/2716ffef8e394c0ca5c8755d025432ca Annales Geophysicae, Vol 26, Pp 813-822 (2008) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2008 ftdoajarticles https://doi.org/10.5194/angeo-26-813-2008 2022-12-31T13:14:50Z We extend the technique suggested by Sentman and Fraser (1991) and discussed by Pechony and Price (2006), the technique for separating the local and universal time variations in the Schumann resonance intensity. Initially, we simulate the resonance oscillations in a uniform Earth-ionosphere cavity with the distribution of lightning strokes based on the OTD satellite data. Different field components were used in the Dayside source model for the Moshiri (Japan, geographic coordinates: 44.365° N, 142.24° E) and Lehta (Karelia, Russia, 64.427° N, 33.974° E) observatories. We use the extended Fourier series for obtaining the modulating functions. Simulations show that the algorithm evaluates the impact of the source proximity in the resonance intensity. Our major goal was in estimating the universal alteration factors, which reflect changes in the global thunderstorm activity. It was achieved by compensating the local factors present in the initial data. The technique is introduced with the model Schumann resonance data and afterwards we use the long-term experimental records at the above sites for obtaining the diurnal/monthly variations of the global thunderstorms. Article in Journal/Newspaper karelia* Directory of Open Access Journals: DOAJ Articles Schumann ENVELOPE(-73.691,-73.691,-71.641,-71.641) Annales Geophysicae 26 4 813 822
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
A. P. Nickolaenko
M. Hayakawa
Universal and local time components in Schumann resonance intensity
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description We extend the technique suggested by Sentman and Fraser (1991) and discussed by Pechony and Price (2006), the technique for separating the local and universal time variations in the Schumann resonance intensity. Initially, we simulate the resonance oscillations in a uniform Earth-ionosphere cavity with the distribution of lightning strokes based on the OTD satellite data. Different field components were used in the Dayside source model for the Moshiri (Japan, geographic coordinates: 44.365° N, 142.24° E) and Lehta (Karelia, Russia, 64.427° N, 33.974° E) observatories. We use the extended Fourier series for obtaining the modulating functions. Simulations show that the algorithm evaluates the impact of the source proximity in the resonance intensity. Our major goal was in estimating the universal alteration factors, which reflect changes in the global thunderstorm activity. It was achieved by compensating the local factors present in the initial data. The technique is introduced with the model Schumann resonance data and afterwards we use the long-term experimental records at the above sites for obtaining the diurnal/monthly variations of the global thunderstorms.
format Article in Journal/Newspaper
author A. P. Nickolaenko
M. Hayakawa
author_facet A. P. Nickolaenko
M. Hayakawa
author_sort A. P. Nickolaenko
title Universal and local time components in Schumann resonance intensity
title_short Universal and local time components in Schumann resonance intensity
title_full Universal and local time components in Schumann resonance intensity
title_fullStr Universal and local time components in Schumann resonance intensity
title_full_unstemmed Universal and local time components in Schumann resonance intensity
title_sort universal and local time components in schumann resonance intensity
publisher Copernicus Publications
publishDate 2008
url https://doi.org/10.5194/angeo-26-813-2008
https://doaj.org/article/2716ffef8e394c0ca5c8755d025432ca
long_lat ENVELOPE(-73.691,-73.691,-71.641,-71.641)
geographic Schumann
geographic_facet Schumann
genre karelia*
genre_facet karelia*
op_source Annales Geophysicae, Vol 26, Pp 813-822 (2008)
op_relation https://www.ann-geophys.net/26/813/2008/angeo-26-813-2008.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-26-813-2008
0992-7689
1432-0576
https://doaj.org/article/2716ffef8e394c0ca5c8755d025432ca
op_doi https://doi.org/10.5194/angeo-26-813-2008
container_title Annales Geophysicae
container_volume 26
container_issue 4
container_start_page 813
op_container_end_page 822
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