Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statistics

A model developed several years ago by Huuskonen et al. (1984) predicted that vertical transport of ions in the nocturnal auroral E-region ionosphere can shift the electron density profiles in altitude during times of sufficiently large electric fields. If the vertical plasma transport...

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Main Authors: T. Bösinger, G. C. Hussey, C. Haldoupis, K. Schlegel
Format: Article
Language:English
Published: Copernicus Publications 2004-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/901/2004/angeo-22-901-2004.pdf
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author T. Bösinger
G. C. Hussey
C. Haldoupis
K. Schlegel
author_facet T. Bösinger
G. C. Hussey
C. Haldoupis
K. Schlegel
author_sort T. Bösinger
collection DOAJ
description A model developed several years ago by Huuskonen et al.&nbsp;(1984) predicted that vertical transport of ions in the nocturnal auroral E-region ionosphere can shift the electron density profiles in altitude during times of sufficiently large electric fields. If the vertical plasma transport effect was to operate over a sufficiently long enough time, then the real height of the E-region electron maximum should be shifted some km upwards (downwards) in the eastward (westward) auroral electrojet, respectively, when the electric field is strong, exceeding, say, 50&nbsp;mV/m. Motivated by these predictions and the lack of any experimental verification so far, we made use of the large database of the European Incoherent Scatter (EISCAT) radar to investigate if the anticipated vertical plasma transport is at work in the auroral E-region ionosphere and thus to test the Huuskonen et al.&nbsp;(1984) model. For this purpose a new type of EISCAT data display was developed which enabled us to order a large number of electron density height profiles, collected over 16 years of EISCAT operation, according to the electric field magnitude and direction as measured at the same time at the radar's magnetic field line in the F-region. Our analysis shows some signatures in tune with a vertical plasma transport in the auroral E-region of the type predicted by the Huuskonen et al.&nbsp;model. The evidence brought forward is, however, not unambiguous and requires more rigorous analysis.<br><br> <b>Key words.</b> Ionosphere (auroral ionosphere; plasma convection; electric fields and currents)
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spelling doaj.art-9151c7a68b5a41e0afa9a9c0cd4eff0a2022-12-22T03:35:42ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-03-012290191010.5194/angeo-22-901-2004Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statisticsT. Bösinger0G. C. Hussey1C. Haldoupis2K. Schlegel3Department of Physical Sciences, University of Oulu, Oulu, FinlandInstitute of Space and Atmospheric Studies, University of Saskatchewan, Saskatoon, CanadaPhysics Department, University of Crete, Iraklion, Crete, GreeceMax-Planck-Institut für Aeronomie, Katlenburg-Lindau, GermanyA model developed several years ago by Huuskonen et al.&nbsp;(1984) predicted that vertical transport of ions in the nocturnal auroral E-region ionosphere can shift the electron density profiles in altitude during times of sufficiently large electric fields. If the vertical plasma transport effect was to operate over a sufficiently long enough time, then the real height of the E-region electron maximum should be shifted some km upwards (downwards) in the eastward (westward) auroral electrojet, respectively, when the electric field is strong, exceeding, say, 50&nbsp;mV/m. Motivated by these predictions and the lack of any experimental verification so far, we made use of the large database of the European Incoherent Scatter (EISCAT) radar to investigate if the anticipated vertical plasma transport is at work in the auroral E-region ionosphere and thus to test the Huuskonen et al.&nbsp;(1984) model. For this purpose a new type of EISCAT data display was developed which enabled us to order a large number of electron density height profiles, collected over 16 years of EISCAT operation, according to the electric field magnitude and direction as measured at the same time at the radar's magnetic field line in the F-region. Our analysis shows some signatures in tune with a vertical plasma transport in the auroral E-region of the type predicted by the Huuskonen et al.&nbsp;model. The evidence brought forward is, however, not unambiguous and requires more rigorous analysis.<br><br> <b>Key words.</b> Ionosphere (auroral ionosphere; plasma convection; electric fields and currents)https://www.ann-geophys.net/22/901/2004/angeo-22-901-2004.pdf
spellingShingle T. Bösinger
G. C. Hussey
C. Haldoupis
K. Schlegel
Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statistics
Annales Geophysicae
title Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statistics
title_full Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statistics
title_fullStr Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statistics
title_full_unstemmed Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statistics
title_short Auroral E-region electron density height profile modificationby electric field driven vertical plasma transport:some evidence in EISCAT CP-1 data statistics
title_sort auroral e region electron density height profile modificationby electric field driven vertical plasma transport some evidence in eiscat cp 1 data statistics
url https://www.ann-geophys.net/22/901/2004/angeo-22-901-2004.pdf
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AT chaldoupis auroraleregionelectrondensityheightprofilemodificationbyelectricfielddrivenverticalplasmatransportsomeevidenceineiscatcp1datastatistics
AT kschlegel auroraleregionelectrondensityheightprofilemodificationbyelectricfielddrivenverticalplasmatransportsomeevidenceineiscatcp1datastatistics