Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems

Simultaneous observations with the IRIS, DASI and EISCAT systems are employed in the study of the spatial distribution and temporal evolution of auroral forms and precipitation regions during substorm activity. The evolution of the spectrum of precipitating electrons above Tromsø during the various...

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Published in:Annales Geophysicae
Main Authors: C. F. del Pozo, F. Honary, N. Stamatiou, M. J. Kosch
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2002
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-20-1361-2002
https://doaj.org/article/341f5f9786e74d7c9dbd46a4bd8428c0
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spelling ftdoajarticles:oai:doaj.org/article:341f5f9786e74d7c9dbd46a4bd8428c0 2023-05-15T16:04:33+02:00 Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems C. F. del Pozo F. Honary N. Stamatiou M. J. Kosch 2002-09-01T00:00:00Z https://doi.org/10.5194/angeo-20-1361-2002 https://doaj.org/article/341f5f9786e74d7c9dbd46a4bd8428c0 EN eng Copernicus Publications https://www.ann-geophys.net/20/1361/2002/angeo-20-1361-2002.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-20-1361-2002 0992-7689 1432-0576 https://doaj.org/article/341f5f9786e74d7c9dbd46a4bd8428c0 Annales Geophysicae, Vol 20, Pp 1361-1375 (2002) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2002 ftdoajarticles https://doi.org/10.5194/angeo-20-1361-2002 2022-12-31T03:13:22Z Simultaneous observations with the IRIS, DASI and EISCAT systems are employed in the study of the spatial distribution and temporal evolution of auroral forms and precipitation regions during substorm activity. The evolution of the spectrum of precipitating electrons above Tromsø during the various phases of substorms is discussed. The flux-energy spectrum in the 1–320 keV range is derived from EISCAT electron density profiles in the 70–140 km altitude range. At the late growth phase the precipitation flux at the higher energies increases faster than at the lower energies. The flux is always greater in the lower energy side of the spectrum and reaches a maximum a few minutes after substorm onset, then it decays while the spectrum narrows. The systematic analysis of 2-D structures corresponding with well-defined optical and absorption features is also discussed. The orientation, characteristic lengths (elongation and width) and the gravity centre of these spatial features are determined. The statistical analysis of centre position and the sizes of the corresponding signatures is presented. When substorm onset falls within the common field of view, there is a close correspondence between the optical and the absorption signatures of the auroral forms, as well as in their over-all north-south motion characteristic of the various phases of the substorm. Optical signatures of arcs are more evenly distributed in space, being narrower and elongated along the L-shells, while the absorption regions appear more structured and patchy, although generally following the arcs’ shape and alignment. Cross-correlation of the time series of maximum absorption and maximum green-line emission is very high and seems to show a systematic delay of absorption relative to optical emission. Time delays are generally larger for disturbed conditions (40 to 60 s) than for moderately active conditions (10 to 20 s). Key words. Interplanetary physics (energetic particles) – Ionosphere (auroral ionosphere; ionosphere–magnetosphere interactions) Article in Journal/Newspaper EISCAT Tromsø Directory of Open Access Journals: DOAJ Articles Tromsø Narrows The ENVELOPE(-67.167,-67.167,-67.617,-67.617) Annales Geophysicae 20 9 1361 1375
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
spellingShingle Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
C. F. del Pozo
F. Honary
N. Stamatiou
M. J. Kosch
Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description Simultaneous observations with the IRIS, DASI and EISCAT systems are employed in the study of the spatial distribution and temporal evolution of auroral forms and precipitation regions during substorm activity. The evolution of the spectrum of precipitating electrons above Tromsø during the various phases of substorms is discussed. The flux-energy spectrum in the 1–320 keV range is derived from EISCAT electron density profiles in the 70–140 km altitude range. At the late growth phase the precipitation flux at the higher energies increases faster than at the lower energies. The flux is always greater in the lower energy side of the spectrum and reaches a maximum a few minutes after substorm onset, then it decays while the spectrum narrows. The systematic analysis of 2-D structures corresponding with well-defined optical and absorption features is also discussed. The orientation, characteristic lengths (elongation and width) and the gravity centre of these spatial features are determined. The statistical analysis of centre position and the sizes of the corresponding signatures is presented. When substorm onset falls within the common field of view, there is a close correspondence between the optical and the absorption signatures of the auroral forms, as well as in their over-all north-south motion characteristic of the various phases of the substorm. Optical signatures of arcs are more evenly distributed in space, being narrower and elongated along the L-shells, while the absorption regions appear more structured and patchy, although generally following the arcs’ shape and alignment. Cross-correlation of the time series of maximum absorption and maximum green-line emission is very high and seems to show a systematic delay of absorption relative to optical emission. Time delays are generally larger for disturbed conditions (40 to 60 s) than for moderately active conditions (10 to 20 s). Key words. Interplanetary physics (energetic particles) – Ionosphere (auroral ionosphere; ionosphere–magnetosphere interactions)
format Article in Journal/Newspaper
author C. F. del Pozo
F. Honary
N. Stamatiou
M. J. Kosch
author_facet C. F. del Pozo
F. Honary
N. Stamatiou
M. J. Kosch
author_sort C. F. del Pozo
title Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems
title_short Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems
title_full Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems
title_fullStr Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems
title_full_unstemmed Study of auroral forms and electron precipitation with the IRIS, DASI and EISCAT systems
title_sort study of auroral forms and electron precipitation with the iris, dasi and eiscat systems
publisher Copernicus Publications
publishDate 2002
url https://doi.org/10.5194/angeo-20-1361-2002
https://doaj.org/article/341f5f9786e74d7c9dbd46a4bd8428c0
long_lat ENVELOPE(-67.167,-67.167,-67.617,-67.617)
geographic Tromsø
Narrows The
geographic_facet Tromsø
Narrows The
genre EISCAT
Tromsø
genre_facet EISCAT
Tromsø
op_source Annales Geophysicae, Vol 20, Pp 1361-1375 (2002)
op_relation https://www.ann-geophys.net/20/1361/2002/angeo-20-1361-2002.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-20-1361-2002
0992-7689
1432-0576
https://doaj.org/article/341f5f9786e74d7c9dbd46a4bd8428c0
op_doi https://doi.org/10.5194/angeo-20-1361-2002
container_title Annales Geophysicae
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container_issue 9
container_start_page 1361
op_container_end_page 1375
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