Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997

The ionospheric Alfvén resonator (IAR) control mechanism over the EMIC wave transmission to the ground is demonstrated on a selected long-term frequency-variable subauroral Pcl event. The proper ionospheric plasma data obtained from EISCAT were accessible in a wide altitude range. Applying the numer...

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Bibliographic Details
Main Authors: Prikner, K, Mursula, K, Kangas, J, Feygin, F. Z
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:https://kramerius.lib.cas.cz/view/uuid:39e2fb2d-b00f-402b-9ddc-4f7e4ebec506
https://doi.org/10.1023/A:1022025619872
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author Prikner, K
Mursula, K
Kangas, J
Feygin, F. Z
author_facet Prikner, K
Mursula, K
Kangas, J
Feygin, F. Z
author_sort Prikner, K
collection Czech Academy of Sciences: dKNAV
description The ionospheric Alfvén resonator (IAR) control mechanism over the EMIC wave transmission to the ground is demonstrated on a selected long-term frequency-variable subauroral Pcl event. The proper ionospheric plasma data obtained from EISCAT were accessible in a wide altitude range. Applying the numerical method of simulation of a realistic inhomogeneous IAR, the problem of appearance and disappearance of the ground Pc1 signal record was clarified on the basis of coincidence between the EMIC wave frequency spectrum and the IAR fundamental frequency peak (the frequency window). A shift of the signal source field line to lower latitudes during the development of the disturbance was noticed, and the signal frequency variation on the ground was modelled in the nonstationary IAR. Variation of the IAR altitude structure in the fundamental frequency was illustrated on altitude profiles of the normalized wave magnetic field amplitude in the horizontal and vertical components. Particular conditions of L‖- and R‖-wave mode incidence were assumed. The electron density vertical profile of IAR determines the effective resonator dimensions. In this way the IAR fundamental frequency window controls the signal within the ionosphere and on the ground. K. Prikner, K. Mursula, J. Kangas, F. Z. Feygin. Obsahuje bibliografii
format Article in Journal/Newspaper
genre EISCAT
genre_facet EISCAT
geographic Kangas
geographic_facet Kangas
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institution Open Polar
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long_lat ENVELOPE(25.367,25.367,66.250,66.250)
op_collection_id ftczechacademysc
op_doi https://doi.org/10.1023/A:1022025619872
op_relation doi:https://doi.org/10.1023/A:1022025619872
op_rights policy:private
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spelling ftczechacademysc:oai:kramerius.lib.cas.cz:uuid:39e2fb2d-b00f-402b-9ddc-4f7e4ebec506 2025-03-16T15:26:23+00:00 Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997 Prikner, K Mursula, K Kangas, J Feygin, F. Z print média svazek https://kramerius.lib.cas.cz/view/uuid:39e2fb2d-b00f-402b-9ddc-4f7e4ebec506 https://doi.org/10.1023/A:1022025619872 unknown doi:https://doi.org/10.1023/A:1022025619872 policy:private 1997 Finsko Finland Pc1 pulsace měření EISCAT Pc1 pulsations Pc1 pearls ionospheric Alfvén resonator resonator response fundamental frequency window EISCAT measurements 7 550 model:article ftczechacademysc https://doi.org/10.1023/A:1022025619872 2025-02-18T02:25:01Z The ionospheric Alfvén resonator (IAR) control mechanism over the EMIC wave transmission to the ground is demonstrated on a selected long-term frequency-variable subauroral Pcl event. The proper ionospheric plasma data obtained from EISCAT were accessible in a wide altitude range. Applying the numerical method of simulation of a realistic inhomogeneous IAR, the problem of appearance and disappearance of the ground Pc1 signal record was clarified on the basis of coincidence between the EMIC wave frequency spectrum and the IAR fundamental frequency peak (the frequency window). A shift of the signal source field line to lower latitudes during the development of the disturbance was noticed, and the signal frequency variation on the ground was modelled in the nonstationary IAR. Variation of the IAR altitude structure in the fundamental frequency was illustrated on altitude profiles of the normalized wave magnetic field amplitude in the horizontal and vertical components. Particular conditions of L‖- and R‖-wave mode incidence were assumed. The electron density vertical profile of IAR determines the effective resonator dimensions. In this way the IAR fundamental frequency window controls the signal within the ionosphere and on the ground. K. Prikner, K. Mursula, J. Kangas, F. Z. Feygin. Obsahuje bibliografii Article in Journal/Newspaper EISCAT Czech Academy of Sciences: dKNAV Kangas ENVELOPE(25.367,25.367,66.250,66.250)
spellingShingle 1997
Finsko
Finland
Pc1 pulsace
měření EISCAT
Pc1 pulsations
Pc1 pearls
ionospheric Alfvén resonator
resonator response
fundamental frequency window
EISCAT measurements
7
550
Prikner, K
Mursula, K
Kangas, J
Feygin, F. Z
Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997
title Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997
title_full Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997
title_fullStr Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997
title_full_unstemmed Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997
title_short Ionospheric Alfvén resonator control over the frequency-variable Pc1 event in Finland on May 14, 1997
title_sort ionospheric alfvén resonator control over the frequency-variable pc1 event in finland on may 14, 1997
topic 1997
Finsko
Finland
Pc1 pulsace
měření EISCAT
Pc1 pulsations
Pc1 pearls
ionospheric Alfvén resonator
resonator response
fundamental frequency window
EISCAT measurements
7
550
topic_facet 1997
Finsko
Finland
Pc1 pulsace
měření EISCAT
Pc1 pulsations
Pc1 pearls
ionospheric Alfvén resonator
resonator response
fundamental frequency window
EISCAT measurements
7
550
url https://kramerius.lib.cas.cz/view/uuid:39e2fb2d-b00f-402b-9ddc-4f7e4ebec506
https://doi.org/10.1023/A:1022025619872