Auroral ion acoustic wave enhancement observed with a radar interferometer system

Published version. Source at http://doi.org/10.5194/angeo-33-837-2015 . Measurements of naturally enhanced ion acoustic line (NEIAL) echoes obtained with a five-antenna interferometric imaging radar system are presented. The observations were conducted with the European Incoherent SCATter (EISCAT) r...

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Published in:Annales Geophysicae
Main Authors: Schlatter, Nicola M., Belyey, Vasyl, Gustavsson, Björn Johan, Ivchenko, Nickolay, Whiter, Daniel, Dahlgren, Hanna, Tuttle, Sam, Grydeland, Tom
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
Online Access:https://hdl.handle.net/10037/8719
https://doi.org/10.5194/angeo-33-837-2015
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author Schlatter, Nicola M.
Belyey, Vasyl
Gustavsson, Björn Johan
Ivchenko, Nickolay
Whiter, Daniel
Dahlgren, Hanna
Tuttle, Sam
Grydeland, Tom
author_facet Schlatter, Nicola M.
Belyey, Vasyl
Gustavsson, Björn Johan
Ivchenko, Nickolay
Whiter, Daniel
Dahlgren, Hanna
Tuttle, Sam
Grydeland, Tom
author_sort Schlatter, Nicola M.
collection University of Tromsø: Munin Open Research Archive
container_issue 7
container_start_page 837
container_title Annales Geophysicae
container_volume 33
description Published version. Source at http://doi.org/10.5194/angeo-33-837-2015 . Measurements of naturally enhanced ion acoustic line (NEIAL) echoes obtained with a five-antenna interferometric imaging radar system are presented. The observations were conducted with the European Incoherent SCATter (EISCAT) radar on Svalbard and the EISCAT Aperture Synthesis Imaging receivers (EASI) installed at the radar site. Four baselines of the interferometer are used in the analysis. Based on the coherence estimates derived from the measurements, we show that the enhanced backscattering region is of limited extent in the plane perpendicular to the geomagnetic field. Previously it has been argued that the enhanced backscatter region is limited in size; however, here the first unambiguous observations are presented. The size of the enhanced backscatter region is determined to be less than 900 × 500 m, and at times less than 160 m in the direction of the longest antenna separation, assuming the scattering region to have a Gaussian scattering cross section in the plane perpendicular to the geomagnetic field. Using aperture synthesis imaging methods volumetric images of the NEIAL echo are obtained showing the enhanced backscattering region to be aligned with the geomagnetic field. Although optical auroral emissions are observed outside the radar look direction, our observations are consistent with the NEIAL echo occurring on field lines with particle precipitation.
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spelling ftunivtroemsoe:oai:munin.uit.no:10037/8719 2025-04-13T14:18:06+00:00 Auroral ion acoustic wave enhancement observed with a radar interferometer system Schlatter, Nicola M. Belyey, Vasyl Gustavsson, Björn Johan Ivchenko, Nickolay Whiter, Daniel Dahlgren, Hanna Tuttle, Sam Grydeland, Tom 2015-07-20 https://hdl.handle.net/10037/8719 https://doi.org/10.5194/angeo-33-837-2015 eng eng Copernicus Publications FRIDAID 1277850 https://hdl.handle.net/10037/8719 openAccess Ionosphere (Auroral ionosphere) VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437 VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437 Journal article Tidsskriftartikkel Peer reviewed 2015 ftunivtroemsoe https://doi.org/10.5194/angeo-33-837-2015 2025-03-14T05:17:56Z Published version. Source at http://doi.org/10.5194/angeo-33-837-2015 . Measurements of naturally enhanced ion acoustic line (NEIAL) echoes obtained with a five-antenna interferometric imaging radar system are presented. The observations were conducted with the European Incoherent SCATter (EISCAT) radar on Svalbard and the EISCAT Aperture Synthesis Imaging receivers (EASI) installed at the radar site. Four baselines of the interferometer are used in the analysis. Based on the coherence estimates derived from the measurements, we show that the enhanced backscattering region is of limited extent in the plane perpendicular to the geomagnetic field. Previously it has been argued that the enhanced backscatter region is limited in size; however, here the first unambiguous observations are presented. The size of the enhanced backscatter region is determined to be less than 900 × 500 m, and at times less than 160 m in the direction of the longest antenna separation, assuming the scattering region to have a Gaussian scattering cross section in the plane perpendicular to the geomagnetic field. Using aperture synthesis imaging methods volumetric images of the NEIAL echo are obtained showing the enhanced backscattering region to be aligned with the geomagnetic field. Although optical auroral emissions are observed outside the radar look direction, our observations are consistent with the NEIAL echo occurring on field lines with particle precipitation. Article in Journal/Newspaper EISCAT Svalbard University of Tromsø: Munin Open Research Archive Svalbard Annales Geophysicae 33 7 837 844
spellingShingle Ionosphere (Auroral ionosphere)
VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437
Schlatter, Nicola M.
Belyey, Vasyl
Gustavsson, Björn Johan
Ivchenko, Nickolay
Whiter, Daniel
Dahlgren, Hanna
Tuttle, Sam
Grydeland, Tom
Auroral ion acoustic wave enhancement observed with a radar interferometer system
title Auroral ion acoustic wave enhancement observed with a radar interferometer system
title_full Auroral ion acoustic wave enhancement observed with a radar interferometer system
title_fullStr Auroral ion acoustic wave enhancement observed with a radar interferometer system
title_full_unstemmed Auroral ion acoustic wave enhancement observed with a radar interferometer system
title_short Auroral ion acoustic wave enhancement observed with a radar interferometer system
title_sort auroral ion acoustic wave enhancement observed with a radar interferometer system
topic Ionosphere (Auroral ionosphere)
VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437
topic_facet Ionosphere (Auroral ionosphere)
VDP::Matematikk og Naturvitenskap: 400::Fysikk: 430::Rom- og plasmafysikk: 437
VDP::Mathematics and natural science: 400::Physics: 430::Space and plasma physics: 437
url https://hdl.handle.net/10037/8719
https://doi.org/10.5194/angeo-33-837-2015