Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles

According to observations, the discrete auroral arcs can sometimes be found, either deep inside the auroral oval or at the poleward border of the wide (so-called double) auroral oval, which map to very different regions of the magnetotail. To find common physical conditions for the auroral-arc g...

Full description

Bibliographic Details
Main Authors: A. G. Yahnin, V. A. Sergeev, B. B. Gvozdevsky, S. Vennerstrøm
Format: Article
Language:English
Published: Copernicus Publications 1997-08-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/15/943/1997/angeo-15-943-1997.pdf
_version_ 1828157046234546176
author A. G. Yahnin
V. A. Sergeev
B. B. Gvozdevsky
S. Vennerstrøm
author_facet A. G. Yahnin
V. A. Sergeev
B. B. Gvozdevsky
S. Vennerstrøm
author_sort A. G. Yahnin
collection DOAJ
description According to observations, the discrete auroral arcs can sometimes be found, either deep inside the auroral oval or at the poleward border of the wide (so-called double) auroral oval, which map to very different regions of the magnetotail. To find common physical conditions for the auroral-arc generation in these magnetotail regions, we study the spatial relationship between the diffuse and discrete auroras and the isotropic boundaries (IBs) of the precipitating energetic particles which can be used to characterise locally the equatorial magnetic field in the tail. From comparison of ground observation of auroral forms with meridional profiles of particle flux measured simultaneously by the low-altitude NOAA satellites above the ground observation region, we found that (1) discrete auroral arcs are always situated polewards from (or very close to) the IB of >30-keV electrons, whereas (2) the IB of the >30-keV protons is often seen inside the diffuse aurora. These relationships hold true for both quiet and active (substorm) conditions in the premidnight-nightside (18-01-h) MLT sector considered. In some events the auroral arcs occupy a wide latitudinal range. The most equatorial of these arcs was found at the poleward edge of the diffuse auroras (but anyway in the vicinity of the electron IB), the most poleward arcs were simultaneously observed on the closed field lines near the polar-cap boundary. These observations disagree with the notion that the discrete aurora originate exclusively in the near-Earth portion of plasma sheet or exclusively on the PSBL field lines. Result (1) may imply a fundamental feature of auroral-arc formation: they originate in the current-sheet regions having very curved and tailward-stretched magnetic field lines.
first_indexed 2024-04-11T23:22:52Z
format Article
id doaj.art-12ab7feb17e846778fdc1124ed17bd11
institution Directory Open Access Journal
issn 0992-7689
1432-0576
language English
last_indexed 2024-04-11T23:22:52Z
publishDate 1997-08-01
publisher Copernicus Publications
record_format Article
series Annales Geophysicae
spelling doaj.art-12ab7feb17e846778fdc1124ed17bd112022-12-22T03:57:25ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05761997-08-011594395810.1007/s00585-997-0943-zMagnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particlesA. G. Yahnin0V. A. Sergeev1B. B. Gvozdevsky2S. Vennerstrøm3Polar Geophysical Institute, Apatity, Murmansk region, 184200, Russia<br>Tel: +7 815 55 37 475; Fax: +7 815 55 30925; e-mail: yahnin@pgi-ksc.murmansk.suInstitute of Physics, University of St. Petersburg, St. Petersburg, RussiaPolar Geophysical Institute, Apatity, Murmansk region, 184200, Russia<br>Tel: +7 815 55 37 475; Fax: +7 815 55 30925; e-mail: yahnin@pgi-ksc.murmansk.suDanish Meteorological Institute, Solar-Terrestrial Physics Division, Copenhagen, DenmarkAccording to observations, the discrete auroral arcs can sometimes be found, either deep inside the auroral oval or at the poleward border of the wide (so-called double) auroral oval, which map to very different regions of the magnetotail. To find common physical conditions for the auroral-arc generation in these magnetotail regions, we study the spatial relationship between the diffuse and discrete auroras and the isotropic boundaries (IBs) of the precipitating energetic particles which can be used to characterise locally the equatorial magnetic field in the tail. From comparison of ground observation of auroral forms with meridional profiles of particle flux measured simultaneously by the low-altitude NOAA satellites above the ground observation region, we found that (1) discrete auroral arcs are always situated polewards from (or very close to) the IB of &gt;30-keV electrons, whereas (2) the IB of the &gt;30-keV protons is often seen inside the diffuse aurora. These relationships hold true for both quiet and active (substorm) conditions in the premidnight-nightside (18-01-h) MLT sector considered. In some events the auroral arcs occupy a wide latitudinal range. The most equatorial of these arcs was found at the poleward edge of the diffuse auroras (but anyway in the vicinity of the electron IB), the most poleward arcs were simultaneously observed on the closed field lines near the polar-cap boundary. These observations disagree with the notion that the discrete aurora originate exclusively in the near-Earth portion of plasma sheet or exclusively on the PSBL field lines. Result (1) may imply a fundamental feature of auroral-arc formation: they originate in the current-sheet regions having very curved and tailward-stretched magnetic field lines.https://www.ann-geophys.net/15/943/1997/angeo-15-943-1997.pdf
spellingShingle A. G. Yahnin
V. A. Sergeev
B. B. Gvozdevsky
S. Vennerstrøm
Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles
Annales Geophysicae
title Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles
title_full Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles
title_fullStr Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles
title_full_unstemmed Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles
title_short Magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles
title_sort magnetospheric source region of discrete auroras inferred from their relationship with isotropy boundaries of energetic particles
url https://www.ann-geophys.net/15/943/1997/angeo-15-943-1997.pdf
work_keys_str_mv AT agyahnin magnetosphericsourceregionofdiscreteaurorasinferredfromtheirrelationshipwithisotropyboundariesofenergeticparticles
AT vasergeev magnetosphericsourceregionofdiscreteaurorasinferredfromtheirrelationshipwithisotropyboundariesofenergeticparticles
AT bbgvozdevsky magnetosphericsourceregionofdiscreteaurorasinferredfromtheirrelationshipwithisotropyboundariesofenergeticparticles
AT svennerstrøm magnetosphericsourceregionofdiscreteaurorasinferredfromtheirrelationshipwithisotropyboundariesofenergeticparticles