Response of the convecting high-latitude F layer to a powerful HF wave
A numerical model of the high-latitude ionosphere, which takes into account the convection of the ionospheric plasma, has been developed and utilized to simulate the F-layer response at auroral latitudes to high-power radio waves. The model produces the time variations of the electron density, posit...
Published in: | Annales Geophysicae |
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Springer Verlag
1997
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Online Access: | https://doi.org/10.1007/s00585-997-1291-8 https://noa.gwlb.de/receive/cop_mods_00037446 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037400/angeo-15-1291-1997.pdf https://angeo.copernicus.org/articles/15/1291/1997/angeo-15-1291-1997.pdf |
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00037446 2023-05-15T18:33:50+02:00 Response of the convecting high-latitude F layer to a powerful HF wave Mingaleva, G. I. Mingalev, V. S. 1997-10 electronic https://doi.org/10.1007/s00585-997-1291-8 https://noa.gwlb.de/receive/cop_mods_00037446 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037400/angeo-15-1291-1997.pdf https://angeo.copernicus.org/articles/15/1291/1997/angeo-15-1291-1997.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/s00585-997-1291-8 https://noa.gwlb.de/receive/cop_mods_00037446 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037400/angeo-15-1291-1997.pdf https://angeo.copernicus.org/articles/15/1291/1997/angeo-15-1291-1997.pdf https://open-access.net/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 1997 ftnonlinearchiv https://doi.org/10.1007/s00585-997-1291-8 2022-02-08T22:43:31Z A numerical model of the high-latitude ionosphere, which takes into account the convection of the ionospheric plasma, has been developed and utilized to simulate the F-layer response at auroral latitudes to high-power radio waves. The model produces the time variations of the electron density, positive ion velocity, and ion and electron temperature profiles within a magnetic field tube carried over an ionospheric heater by the convection electric field. The simulations have been performed for the point with the geographic coordinates of the ionospheric HF heating facility near Tromso, Norway, when it is located near the midnight magnetic meridian. The calculations have been made for equinox, at high-solar-activity, and low-geomagnetic-activity conditions. The results indicate that significant variations of the electron temperature, positive ion velocity, and electron density profiles can be produced by HF heating in the convecting high-latitude F layer. Article in Journal/Newspaper Tromso Tromso Niedersächsisches Online-Archiv NOA Norway Tromso ENVELOPE(16.546,16.546,68.801,68.801) Annales Geophysicae 15 10 1291 1300 |
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Open Polar |
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Niedersächsisches Online-Archiv NOA |
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ftnonlinearchiv |
language |
English |
topic |
article Verlagsveröffentlichung |
spellingShingle |
article Verlagsveröffentlichung Mingaleva, G. I. Mingalev, V. S. Response of the convecting high-latitude F layer to a powerful HF wave |
topic_facet |
article Verlagsveröffentlichung |
description |
A numerical model of the high-latitude ionosphere, which takes into account the convection of the ionospheric plasma, has been developed and utilized to simulate the F-layer response at auroral latitudes to high-power radio waves. The model produces the time variations of the electron density, positive ion velocity, and ion and electron temperature profiles within a magnetic field tube carried over an ionospheric heater by the convection electric field. The simulations have been performed for the point with the geographic coordinates of the ionospheric HF heating facility near Tromso, Norway, when it is located near the midnight magnetic meridian. The calculations have been made for equinox, at high-solar-activity, and low-geomagnetic-activity conditions. The results indicate that significant variations of the electron temperature, positive ion velocity, and electron density profiles can be produced by HF heating in the convecting high-latitude F layer. |
format |
Article in Journal/Newspaper |
author |
Mingaleva, G. I. Mingalev, V. S. |
author_facet |
Mingaleva, G. I. Mingalev, V. S. |
author_sort |
Mingaleva, G. I. |
title |
Response of the convecting high-latitude F layer to a powerful HF wave |
title_short |
Response of the convecting high-latitude F layer to a powerful HF wave |
title_full |
Response of the convecting high-latitude F layer to a powerful HF wave |
title_fullStr |
Response of the convecting high-latitude F layer to a powerful HF wave |
title_full_unstemmed |
Response of the convecting high-latitude F layer to a powerful HF wave |
title_sort |
response of the convecting high-latitude f layer to a powerful hf wave |
publisher |
Springer Verlag |
publishDate |
1997 |
url |
https://doi.org/10.1007/s00585-997-1291-8 https://noa.gwlb.de/receive/cop_mods_00037446 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037400/angeo-15-1291-1997.pdf https://angeo.copernicus.org/articles/15/1291/1997/angeo-15-1291-1997.pdf |
long_lat |
ENVELOPE(16.546,16.546,68.801,68.801) |
geographic |
Norway Tromso |
geographic_facet |
Norway Tromso |
genre |
Tromso Tromso |
genre_facet |
Tromso Tromso |
op_relation |
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/s00585-997-1291-8 https://noa.gwlb.de/receive/cop_mods_00037446 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00037400/angeo-15-1291-1997.pdf https://angeo.copernicus.org/articles/15/1291/1997/angeo-15-1291-1997.pdf |
op_rights |
https://open-access.net/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1007/s00585-997-1291-8 |
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Annales Geophysicae |
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10 |
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