Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016

Dynamics of seasonal variations of the amplitude of the VLF radio signal received in Yakutsk from the navigation station near Novosibirsk and the P-branches of the OH band (6-2) radiation intensity in the wavelength range 835 - 853 nm are considered. The radiation variations give information about m...

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Published in:E3S Web of Conferences
Main Authors: Korsakov Alexey, Kozlov Vladimir, Ammosova Anastasia, Ammosov Petr, Gavrilyeva Galina, Koltovskoi Igor, Pavlov Yegor
Format: Article in Journal/Newspaper
Language:English
French
Published: EDP Sciences 2017
Subjects:
geo
Online Access:https://doi.org/10.1051/e3sconf/20172001005
https://doaj.org/article/eb547004d39f4f8781ada2d503f807bd
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:eb547004d39f4f8781ada2d503f807bd 2023-05-15T18:45:22+02:00 Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016 Korsakov Alexey Kozlov Vladimir Ammosova Anastasia Ammosov Petr Gavrilyeva Galina Koltovskoi Igor Pavlov Yegor 2017-01-01 https://doi.org/10.1051/e3sconf/20172001005 https://doaj.org/article/eb547004d39f4f8781ada2d503f807bd en fr eng fre EDP Sciences 2267-1242 doi:10.1051/e3sconf/20172001005 https://doaj.org/article/eb547004d39f4f8781ada2d503f807bd undefined E3S Web of Conferences, Vol 20, p 01005 (2017) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2017 fttriple https://doi.org/10.1051/e3sconf/20172001005 2023-01-22T19:15:51Z Dynamics of seasonal variations of the amplitude of the VLF radio signal received in Yakutsk from the navigation station near Novosibirsk and the P-branches of the OH band (6-2) radiation intensity in the wavelength range 835 - 853 nm are considered. The radiation variations give information about mesopause region measured at the Maimaga station (130 km from Yakutsk). The observation from 2009 to 2016 covers period with minimum and maximum solar activity. The mesopause temperature and the VLF signal increase with increasing solar flux F10.7 in winter. The mesopause temperature seasonal variations and the VLF signal strength for the Novosibirsk-Yakutsk path are regularly inverted from year to year. By decade data averaging the VLF radio signal strength dependence on the temperature of the atmosphere at the OH excitation height can be expressed by a linear function. The coefficient of determination: R2 = 0.59, the anticorrelation coefficient: r10 = - 0.77. The variations of the VLF radio noise and the radio station signal for the eight-year interval are similar to solar activity (F10.7 index). The signal level of the radio station and radio noise registered in the winter is more sensitive to variations of F10.7 index in 24th solar cycle activity. Article in Journal/Newspaper Yakutsk Unknown Yakutsk E3S Web of Conferences 20 01005
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
French
topic geo
envir
spellingShingle geo
envir
Korsakov Alexey
Kozlov Vladimir
Ammosova Anastasia
Ammosov Petr
Gavrilyeva Galina
Koltovskoi Igor
Pavlov Yegor
Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016
topic_facet geo
envir
description Dynamics of seasonal variations of the amplitude of the VLF radio signal received in Yakutsk from the navigation station near Novosibirsk and the P-branches of the OH band (6-2) radiation intensity in the wavelength range 835 - 853 nm are considered. The radiation variations give information about mesopause region measured at the Maimaga station (130 km from Yakutsk). The observation from 2009 to 2016 covers period with minimum and maximum solar activity. The mesopause temperature and the VLF signal increase with increasing solar flux F10.7 in winter. The mesopause temperature seasonal variations and the VLF signal strength for the Novosibirsk-Yakutsk path are regularly inverted from year to year. By decade data averaging the VLF radio signal strength dependence on the temperature of the atmosphere at the OH excitation height can be expressed by a linear function. The coefficient of determination: R2 = 0.59, the anticorrelation coefficient: r10 = - 0.77. The variations of the VLF radio noise and the radio station signal for the eight-year interval are similar to solar activity (F10.7 index). The signal level of the radio station and radio noise registered in the winter is more sensitive to variations of F10.7 index in 24th solar cycle activity.
format Article in Journal/Newspaper
author Korsakov Alexey
Kozlov Vladimir
Ammosova Anastasia
Ammosov Petr
Gavrilyeva Galina
Koltovskoi Igor
Pavlov Yegor
author_facet Korsakov Alexey
Kozlov Vladimir
Ammosova Anastasia
Ammosov Petr
Gavrilyeva Galina
Koltovskoi Igor
Pavlov Yegor
author_sort Korsakov Alexey
title Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016
title_short Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016
title_full Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016
title_fullStr Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016
title_full_unstemmed Seasonal variations of mesopause temperature and the amplitude of the VLF signals of the Novosibirsk radio station during 2009-2016
title_sort seasonal variations of mesopause temperature and the amplitude of the vlf signals of the novosibirsk radio station during 2009-2016
publisher EDP Sciences
publishDate 2017
url https://doi.org/10.1051/e3sconf/20172001005
https://doaj.org/article/eb547004d39f4f8781ada2d503f807bd
geographic Yakutsk
geographic_facet Yakutsk
genre Yakutsk
genre_facet Yakutsk
op_source E3S Web of Conferences, Vol 20, p 01005 (2017)
op_relation 2267-1242
doi:10.1051/e3sconf/20172001005
https://doaj.org/article/eb547004d39f4f8781ada2d503f807bd
op_rights undefined
op_doi https://doi.org/10.1051/e3sconf/20172001005
container_title E3S Web of Conferences
container_volume 20
container_start_page 01005
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