The response of the azimuthal component of the ionospheric electric field to auroral arc brightening

We have analyzed the response of azimuthal component of the ionospheric electric field to auroral arc activity. We have chosen for analysis three intervals of coordinated EISCAT and TV observations on 18 February, 1993. These intervals include three kinds of arc activity: the appearance of a new aur...

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Published in:Annales Geophysicae
Main Authors: Safargaleev, V., Lyatsky, W., Gazey, N. G., Smith, P. N., Kriviliov, V.
Format: Article in Journal/Newspaper
Language:English
Published: Springer Verlag 2000
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Online Access:https://doi.org/10.1007/s00585-000-0065-3
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author Safargaleev, V.
Lyatsky, W.
Gazey, N. G.
Smith, P. N.
Kriviliov, V.
author_facet Safargaleev, V.
Lyatsky, W.
Gazey, N. G.
Smith, P. N.
Kriviliov, V.
author_sort Safargaleev, V.
collection Niedersächsisches Online-Archiv NOA
container_issue 1
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container_title Annales Geophysicae
container_volume 18
description We have analyzed the response of azimuthal component of the ionospheric electric field to auroral arc activity. We have chosen for analysis three intervals of coordinated EISCAT and TV observations on 18 February, 1993. These intervals include three kinds of arc activity: the appearance of a new auroral arc, the gradual brightening of the existing arc and variations of the arc luminosity. The arcs were mostly east-west aligned. In all cases, the enhancement of arc luminosity is accompanied by a decrease in the westward component of the ionospheric electric field. In contrast, an increase of that component seems to be connected with arc fading. The observed response is assumed to have the same nature as the "short circuit" of an external electric field by the conductor. The possible consequence of this phenomenon is discussed. Keywords. Ionosphere (electric fields and currents; ionospheric irregularities) · Magnetospheric physics (auroral phenomena)
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https://doi.org/10.1007/s00585-000-0065-3
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spelling ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00036842 2025-01-16T21:42:11+00:00 The response of the azimuthal component of the ionospheric electric field to auroral arc brightening Safargaleev, V. Lyatsky, W. Gazey, N. G. Smith, P. N. Kriviliov, V. 2000-01 electronic https://doi.org/10.1007/s00585-000-0065-3 https://noa.gwlb.de/receive/cop_mods_00036842 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00036796/angeo-18-65-2000.pdf https://angeo.copernicus.org/articles/18/65/2000/angeo-18-65-2000.pdf eng eng Springer Verlag Annales Geophysicae -- http://www.bibliothek.uni-regensburg.de/ezeit/?1458425 -- https://www.ann-geophys.net/ -- https://www.ann-geophys.net/volumes.html -- http://link.springer.com/journal/585 -- 1432-0576 https://doi.org/10.1007/s00585-000-0065-3 https://noa.gwlb.de/receive/cop_mods_00036842 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00036796/angeo-18-65-2000.pdf https://angeo.copernicus.org/articles/18/65/2000/angeo-18-65-2000.pdf https://open-access.net/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2000 ftnonlinearchiv https://doi.org/10.1007/s00585-000-0065-3 2022-02-08T22:43:48Z We have analyzed the response of azimuthal component of the ionospheric electric field to auroral arc activity. We have chosen for analysis three intervals of coordinated EISCAT and TV observations on 18 February, 1993. These intervals include three kinds of arc activity: the appearance of a new auroral arc, the gradual brightening of the existing arc and variations of the arc luminosity. The arcs were mostly east-west aligned. In all cases, the enhancement of arc luminosity is accompanied by a decrease in the westward component of the ionospheric electric field. In contrast, an increase of that component seems to be connected with arc fading. The observed response is assumed to have the same nature as the "short circuit" of an external electric field by the conductor. The possible consequence of this phenomenon is discussed. Keywords. Ionosphere (electric fields and currents; ionospheric irregularities) · Magnetospheric physics (auroral phenomena) Article in Journal/Newspaper EISCAT Niedersächsisches Online-Archiv NOA Annales Geophysicae 18 1 65 73
spellingShingle article
Verlagsveröffentlichung
Safargaleev, V.
Lyatsky, W.
Gazey, N. G.
Smith, P. N.
Kriviliov, V.
The response of the azimuthal component of the ionospheric electric field to auroral arc brightening
title The response of the azimuthal component of the ionospheric electric field to auroral arc brightening
title_full The response of the azimuthal component of the ionospheric electric field to auroral arc brightening
title_fullStr The response of the azimuthal component of the ionospheric electric field to auroral arc brightening
title_full_unstemmed The response of the azimuthal component of the ionospheric electric field to auroral arc brightening
title_short The response of the azimuthal component of the ionospheric electric field to auroral arc brightening
title_sort response of the azimuthal component of the ionospheric electric field to auroral arc brightening
topic article
Verlagsveröffentlichung
topic_facet article
Verlagsveröffentlichung
url https://doi.org/10.1007/s00585-000-0065-3
https://noa.gwlb.de/receive/cop_mods_00036842
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00036796/angeo-18-65-2000.pdf
https://angeo.copernicus.org/articles/18/65/2000/angeo-18-65-2000.pdf