Observations of HF-induced instability in the auroral E region

Enhancements were observed in backscattered radar power during an ionospheric heating experiment from two distinct altitude regions in the auroral E region above Tromsø. For the experiment the EISCAT Tromsø heater was operated with O mode and X mode alternated at 4.04 MHz, close to the 3rd electron...

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Published in:Annales Geophysicae
Main Authors: Schlatter, N. M., Ivchenko, N., Gustavsson, B., Leyser, T., Rietveld, M.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-31-1103-2013
https://angeo.copernicus.org/articles/31/1103/2013/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo15239 2023-05-15T16:04:28+02:00 Observations of HF-induced instability in the auroral E region Schlatter, N. M. Ivchenko, N. Gustavsson, B. Leyser, T. Rietveld, M. 2018-10-21 application/pdf https://doi.org/10.5194/angeo-31-1103-2013 https://angeo.copernicus.org/articles/31/1103/2013/ eng eng doi:10.5194/angeo-31-1103-2013 https://angeo.copernicus.org/articles/31/1103/2013/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-31-1103-2013 2020-07-20T16:25:27Z Enhancements were observed in backscattered radar power during an ionospheric heating experiment from two distinct altitude regions in the auroral E region above Tromsø. For the experiment the EISCAT Tromsø heater was operated with O mode and X mode alternated at 4.04 MHz, close to the 3rd electron gyroharmonic. Ion-line data recorded with the EISCAT UHF radar reveal different temporal evolutions as well as different ion-line characteristics for the enhancements from the two altitude regions. The upper layer is dominated by a strong central feature, whereas the lower layer has three peaks corresponding to the central feature and the two ion lines. The altitude region of the two closely spaced (altitude separation ~ 5 km) but distinct enhancements is close to the critical altitude for the heater wave. Text EISCAT Tromsø Copernicus Publications: E-Journals Tromsø Annales Geophysicae 31 6 1103 1108
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Enhancements were observed in backscattered radar power during an ionospheric heating experiment from two distinct altitude regions in the auroral E region above Tromsø. For the experiment the EISCAT Tromsø heater was operated with O mode and X mode alternated at 4.04 MHz, close to the 3rd electron gyroharmonic. Ion-line data recorded with the EISCAT UHF radar reveal different temporal evolutions as well as different ion-line characteristics for the enhancements from the two altitude regions. The upper layer is dominated by a strong central feature, whereas the lower layer has three peaks corresponding to the central feature and the two ion lines. The altitude region of the two closely spaced (altitude separation ~ 5 km) but distinct enhancements is close to the critical altitude for the heater wave.
format Text
author Schlatter, N. M.
Ivchenko, N.
Gustavsson, B.
Leyser, T.
Rietveld, M.
spellingShingle Schlatter, N. M.
Ivchenko, N.
Gustavsson, B.
Leyser, T.
Rietveld, M.
Observations of HF-induced instability in the auroral E region
author_facet Schlatter, N. M.
Ivchenko, N.
Gustavsson, B.
Leyser, T.
Rietveld, M.
author_sort Schlatter, N. M.
title Observations of HF-induced instability in the auroral E region
title_short Observations of HF-induced instability in the auroral E region
title_full Observations of HF-induced instability in the auroral E region
title_fullStr Observations of HF-induced instability in the auroral E region
title_full_unstemmed Observations of HF-induced instability in the auroral E region
title_sort observations of hf-induced instability in the auroral e region
publishDate 2018
url https://doi.org/10.5194/angeo-31-1103-2013
https://angeo.copernicus.org/articles/31/1103/2013/
geographic Tromsø
geographic_facet Tromsø
genre EISCAT
Tromsø
genre_facet EISCAT
Tromsø
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-31-1103-2013
https://angeo.copernicus.org/articles/31/1103/2013/
op_doi https://doi.org/10.5194/angeo-31-1103-2013
container_title Annales Geophysicae
container_volume 31
container_issue 6
container_start_page 1103
op_container_end_page 1108
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