The importance of solar illumination for discrete and diffuse aurora

We present a comprehensive overview of the occurrence of discrete and diffuse aurora in the nightside Northern Hemisphere at invariant latitudes 55°-75°. Twenty-one months of Freja observations (1 January 1993 to 30 September 1994) from the Northern Hemi...

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Main Authors: M. Hamrin, P. Norqvist, K. Rönnmark, D. Fellgård
Format: Article
Language:English
Published: Copernicus Publications 2005-12-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/23/3481/2005/angeo-23-3481-2005.pdf
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spelling doaj-4c493f29abf047cbb7c24bd745cb11e92020-11-24T23:43:23ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762005-12-01233481348610.5194/angeo-23-3481-2005The importance of solar illumination for discrete and diffuse auroraM. Hamrin0P. Norqvist1K. Rönnmark2D. Fellgård3Department of Physics, Umeå university, Umeå, SwedenDepartment of Physics, Umeå university, Umeå, SwedenDepartment of Physics, Umeå university, Umeå, SwedenDepartment of Physics, Umeå university, Umeå, SwedenWe present a comprehensive overview of the occurrence of discrete and diffuse aurora in the nightside Northern Hemisphere at invariant latitudes 55°-75°. Twenty-one months of Freja observations (1 January 1993 to 30 September 1994) from the Northern Hemisphere, obtained at altitude, are included in this investigation. We investigate the importance of seasonal effects, solar illumination and geomagnetic activity for the auroral precipitation. The seasonal variations in the occurrence of discrete aurora are separated from the dependence on solar illumination of the ionosphere. When the effects of sunlight are eliminated, aurora is found to be more common during the summer. The occurrence of diffuse, as well as discrete aurora, is suppressed by solar illumination of the ionosphere. This dependence of diffuse auroral precipitation on ionospheric conditions is not predicted by theories that attribute diffuse aurora to equatorial pitch-angle diffusion of hot magnetospheric electrons.https://www.ann-geophys.net/23/3481/2005/angeo-23-3481-2005.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Hamrin
P. Norqvist
K. Rönnmark
D. Fellgård
spellingShingle M. Hamrin
P. Norqvist
K. Rönnmark
D. Fellgård
The importance of solar illumination for discrete and diffuse aurora
Annales Geophysicae
author_facet M. Hamrin
P. Norqvist
K. Rönnmark
D. Fellgård
author_sort M. Hamrin
title The importance of solar illumination for discrete and diffuse aurora
title_short The importance of solar illumination for discrete and diffuse aurora
title_full The importance of solar illumination for discrete and diffuse aurora
title_fullStr The importance of solar illumination for discrete and diffuse aurora
title_full_unstemmed The importance of solar illumination for discrete and diffuse aurora
title_sort importance of solar illumination for discrete and diffuse aurora
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2005-12-01
description We present a comprehensive overview of the occurrence of discrete and diffuse aurora in the nightside Northern Hemisphere at invariant latitudes 55°-75°. Twenty-one months of Freja observations (1 January 1993 to 30 September 1994) from the Northern Hemisphere, obtained at altitude, are included in this investigation. We investigate the importance of seasonal effects, solar illumination and geomagnetic activity for the auroral precipitation. The seasonal variations in the occurrence of discrete aurora are separated from the dependence on solar illumination of the ionosphere. When the effects of sunlight are eliminated, aurora is found to be more common during the summer. The occurrence of diffuse, as well as discrete aurora, is suppressed by solar illumination of the ionosphere. This dependence of diffuse auroral precipitation on ionospheric conditions is not predicted by theories that attribute diffuse aurora to equatorial pitch-angle diffusion of hot magnetospheric electrons.
url https://www.ann-geophys.net/23/3481/2005/angeo-23-3481-2005.pdf
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