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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Online Access: | https://hdl.handle.net/10037/6045 https://doi.org/10.5194/angeo-31-1681-2013 |
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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 |
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Open Polar |
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University of Tromsø: Munin Open Research Archive |
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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 |
_version_ |
1766400081599135744 |