Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation

Natural enhancements in the backscattered power of incoherent scatter radars up to 5 orders of magnitudes above the thermal backscatter are sometimes observed at high latitudes. Recently observations of enhancements in the backscattered power including a feature at zero Doppler shift have been repor...

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Published in:Annales Geophysicae
Main Authors: Schlatter, Nicola M., Ivchenko, Nickolay, Sergienko, T, Gustavsson, Björn Johan, Brändström, B. U. E.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2013
Subjects:
Online Access:https://hdl.handle.net/10037/6045
https://doi.org/10.5194/angeo-31-1681-2013
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/6045 2023-05-15T16:04:30+02:00 Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation Schlatter, Nicola M. Ivchenko, Nickolay Sergienko, T Gustavsson, Björn Johan Brändström, B. U. E. 2013 https://hdl.handle.net/10037/6045 https://doi.org/10.5194/angeo-31-1681-2013 eng eng Copernicus Annales Geophysicae 31(2013) nr. 10 s. 1681-1687 FRIDAID 1105268 http://dx.doi.org/10.5194/angeo-31-1681-2013 0992-7689 https://hdl.handle.net/10037/6045 URN:NBN:no-uit_munin_5738 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-31-1681-2013 2021-06-25T17:53:49Z Natural enhancements in the backscattered power of incoherent scatter radars up to 5 orders of magnitudes above the thermal backscatter are sometimes observed at high latitudes. Recently observations of enhancements in the backscattered power including a feature at zero Doppler shift have been reported. These enhancements are limited in altitude to tens of kilometers. The zero Doppler shift feature has been interpreted as a signature of electron density cavitation. Enhanced plasma lines during these observations have also been reported. We report on the first EISCAT UHF observations of enhanced backscattered radar power including a zero Doppler shift feature. The enhancements originated from two distinct and intermittent layers at about 200 km altitude. The altitude extent of the enhancements, observed during auroral high-energy electron precipitation, was < 2 km. Article in Journal/Newspaper EISCAT University of Tromsø: Munin Open Research Archive Annales Geophysicae 31 10 1681 1687
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
Sergienko, T
Gustavsson, Björn Johan
Brändström, B. U. E.
Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation
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 Natural enhancements in the backscattered power of incoherent scatter radars up to 5 orders of magnitudes above the thermal backscatter are sometimes observed at high latitudes. Recently observations of enhancements in the backscattered power including a feature at zero Doppler shift have been reported. These enhancements are limited in altitude to tens of kilometers. The zero Doppler shift feature has been interpreted as a signature of electron density cavitation. Enhanced plasma lines during these observations have also been reported. We report on the first EISCAT UHF observations of enhanced backscattered radar power including a zero Doppler shift feature. The enhancements originated from two distinct and intermittent layers at about 200 km altitude. The altitude extent of the enhancements, observed during auroral high-energy electron precipitation, was < 2 km.
format Article in Journal/Newspaper
author Schlatter, Nicola M.
Ivchenko, Nickolay
Sergienko, T
Gustavsson, Björn Johan
Brändström, B. U. E.
author_facet Schlatter, Nicola M.
Ivchenko, Nickolay
Sergienko, T
Gustavsson, Björn Johan
Brändström, B. U. E.
author_sort Schlatter, Nicola M.
title Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation
title_short Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation
title_full Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation
title_fullStr Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation
title_full_unstemmed Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation
title_sort enhanced eiscat uhf backscatter during high-energy auroral electron precipitation
publisher Copernicus
publishDate 2013
url https://hdl.handle.net/10037/6045
https://doi.org/10.5194/angeo-31-1681-2013
genre EISCAT
genre_facet EISCAT
op_relation Annales Geophysicae 31(2013) nr. 10 s. 1681-1687
FRIDAID 1105268
http://dx.doi.org/10.5194/angeo-31-1681-2013
0992-7689
https://hdl.handle.net/10037/6045
URN:NBN:no-uit_munin_5738
op_rights openAccess
op_doi https://doi.org/10.5194/angeo-31-1681-2013
container_title Annales Geophysicae
container_volume 31
container_issue 10
container_start_page 1681
op_container_end_page 1687
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