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, Nicola M., Ivchenko, Nickolay, Gustavsson, Björn Johan, Leyser, Thomas, Rietveld, Michael T
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2013
Subjects:
Online Access:https://hdl.handle.net/10037/6044
https://doi.org/10.5194/angeo-31-1103-2013
id ftunivtroemsoe:oai:munin.uit.no:10037/6044
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/6044 2023-05-15T16:04:30+02:00 Observations of HF-induced instability in the auroral E region Schlatter, Nicola M. Ivchenko, Nickolay Gustavsson, Björn Johan Leyser, Thomas Rietveld, Michael T 2013 https://hdl.handle.net/10037/6044 https://doi.org/10.5194/angeo-31-1103-2013 eng eng Copernicus Annales Geophysicae 31(2013) nr. 6 s. 1103-1108 FRIDAID 1105279 http://dx.doi.org/10.5194/angeo-31-1103-2013 0992-7689 https://hdl.handle.net/10037/6044 URN:NBN:no-uit_munin_5726 openAccess VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437 VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437 Journal article Tidsskriftartikkel Peer reviewed 2013 ftunivtroemsoe https://doi.org/10.5194/angeo-31-1103-2013 2021-06-25T17:53:49Z 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. Article in Journal/Newspaper EISCAT Tromsø University of Tromsø: Munin Open Research Archive Tromsø Annales Geophysicae 31 6 1103 1108
institution Open Polar
collection University of Tromsø: Munin Open Research Archive
op_collection_id ftunivtroemsoe
language English
topic VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437
VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
spellingShingle VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437
VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
Schlatter, Nicola M.
Ivchenko, Nickolay
Gustavsson, Björn Johan
Leyser, Thomas
Rietveld, Michael T
Observations of HF-induced instability in the auroral E region
topic_facet VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437
VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
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 Article in Journal/Newspaper
author Schlatter, Nicola M.
Ivchenko, Nickolay
Gustavsson, Björn Johan
Leyser, Thomas
Rietveld, Michael T
author_facet Schlatter, Nicola M.
Ivchenko, Nickolay
Gustavsson, Björn Johan
Leyser, Thomas
Rietveld, Michael T
author_sort Schlatter, Nicola 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
publisher Copernicus
publishDate 2013
url https://hdl.handle.net/10037/6044
https://doi.org/10.5194/angeo-31-1103-2013
geographic Tromsø
geographic_facet Tromsø
genre EISCAT
Tromsø
genre_facet EISCAT
Tromsø
op_relation Annales Geophysicae 31(2013) nr. 6 s. 1103-1108
FRIDAID 1105279
http://dx.doi.org/10.5194/angeo-31-1103-2013
0992-7689
https://hdl.handle.net/10037/6044
URN:NBN:no-uit_munin_5726
op_rights openAccess
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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