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...
Published in: | Annales Geophysicae |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2000
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Subjects: | |
Online Access: | https://doi.org/10.1007/s00585-000-0065-3 https://doaj.org/article/2a06c02f28494e9aaeca79fbfa2d6976 |
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author | V. Safargaleev W. Lyatsky N. G. Gazey P. N. Smith V. Kriviliov |
author_facet | V. Safargaleev W. Lyatsky N. G. Gazey P. N. Smith V. Kriviliov |
author_sort | V. Safargaleev |
collection | Directory of Open Access Journals: DOAJ Articles |
container_issue | 1 |
container_start_page | 65 |
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) |
format | Article in Journal/Newspaper |
genre | EISCAT |
genre_facet | EISCAT |
id | ftdoajarticles:oai:doaj.org/article:2a06c02f28494e9aaeca79fbfa2d6976 |
institution | Open Polar |
language | English |
op_collection_id | ftdoajarticles |
op_container_end_page | 73 |
op_doi | https://doi.org/10.1007/s00585-000-0065-3 |
op_relation | https://www.ann-geophys.net/18/65/2000/angeo-18-65-2000.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.1007/s00585-000-0065-3 0992-7689 1432-0576 https://doaj.org/article/2a06c02f28494e9aaeca79fbfa2d6976 |
op_source | Annales Geophysicae, Vol 18, Pp 65-73 (2000) |
publishDate | 2000 |
publisher | Copernicus Publications |
record_format | openpolar |
spelling | ftdoajarticles:oai:doaj.org/article:2a06c02f28494e9aaeca79fbfa2d6976 2025-01-16T21:42:13+00:00 The response of the azimuthal component of the ionospheric electric field to auroral arc brightening V. Safargaleev W. Lyatsky N. G. Gazey P. N. Smith V. Kriviliov 2000-01-01T00:00:00Z https://doi.org/10.1007/s00585-000-0065-3 https://doaj.org/article/2a06c02f28494e9aaeca79fbfa2d6976 EN eng Copernicus Publications https://www.ann-geophys.net/18/65/2000/angeo-18-65-2000.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.1007/s00585-000-0065-3 0992-7689 1432-0576 https://doaj.org/article/2a06c02f28494e9aaeca79fbfa2d6976 Annales Geophysicae, Vol 18, Pp 65-73 (2000) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2000 ftdoajarticles https://doi.org/10.1007/s00585-000-0065-3 2022-12-31T04:44:11Z 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 Directory of Open Access Journals: DOAJ Articles Annales Geophysicae 18 1 65 73 |
spellingShingle | Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 V. Safargaleev W. Lyatsky N. G. Gazey P. N. Smith V. Kriviliov 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 | Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 |
topic_facet | Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 |
url | https://doi.org/10.1007/s00585-000-0065-3 https://doaj.org/article/2a06c02f28494e9aaeca79fbfa2d6976 |