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...
Published in: | Annales Geophysicae |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus
2013
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Subjects: | |
Online Access: | https://hdl.handle.net/10037/6045 https://doi.org/10.5194/angeo-31-1681-2013 |
_version_ | 1829307746022850560 |
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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. |
collection | University of Tromsø: Munin Open Research Archive |
container_issue | 10 |
container_start_page | 1681 |
container_title | Annales Geophysicae |
container_volume | 31 |
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 |
genre | EISCAT |
genre_facet | EISCAT |
id | ftunivtroemsoe:oai:munin.uit.no:10037/6045 |
institution | Open Polar |
language | English |
op_collection_id | ftunivtroemsoe |
op_container_end_page | 1687 |
op_doi | https://doi.org/10.5194/angeo-31-1681-2013 |
op_relation | FRIDAID 1105268 https://hdl.handle.net/10037/6045 |
op_rights | openAccess |
publishDate | 2013 |
publisher | Copernicus |
record_format | openpolar |
spelling | ftunivtroemsoe:oai:munin.uit.no:10037/6045 2025-04-13T14:18:05+00:00 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 FRIDAID 1105268 https://hdl.handle.net/10037/6045 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 2025-03-14T05:17:55Z 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 |
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 |
title | 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_short | Enhanced EISCAT UHF backscatter during high-energy auroral electron precipitation |
title_sort | enhanced eiscat uhf backscatter during high-energy auroral electron precipitation |
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 |
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 |
url | https://hdl.handle.net/10037/6045 https://doi.org/10.5194/angeo-31-1681-2013 |