Comparison of simulated and observed large-scale, field-aligned current structures

Recently, a model of large-scale, field-aligned current (FAC) structures, based on zero-frequency MHD surface wave (SW) modes that can emerge from the solar wind-Earth's magnetosphere interaction, has been proposed. The FAC polarity and intensity distribution are quantified as a function of...

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Main Author: P. Nenovski
Format: Article
Language:English
Published: Copernicus Publications 2008-02-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/281/2008/angeo-26-281-2008.pdf
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spelling doaj-a7739f014e684969b5e5c79d6c0eee942020-11-25T00:20:20ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-02-012628129310.5194/angeo-26-281-2008Comparison of simulated and observed large-scale, field-aligned current structuresP. Nenovski0Geophysical Institute, Bulgarian Academy of Sciences, 1113 Sofia, BulgariaRecently, a model of large-scale, field-aligned current (FAC) structures, based on zero-frequency MHD surface wave (SW) modes that can emerge from the solar wind-Earth's magnetosphere interaction, has been proposed. The FAC polarity and intensity distribution are quantified as a function of the solar wind parameters and the interplanetary magnetic field (IMF) magnitude that enter as input parameters. Besides, there are input parameters intrinsic to the Earth's magnetosphere &ndash; the size of the polar cap and the boundary regions and their plasma density variations. Influence of the IMF <I>B<sub>y</sub></I> component on the FAC structure is examined here. Depending on the IMF <I>B<sub>y</sub></I> magnitude, the predicted six-cell FAC structure tends to evolve in a spiral-like fashion. This large-scale FAC model is compared with experimental evidences and empirical FAC models based on DE-2 satellite data and high-precision Oersted and Magsat satellite magnetometer data. Among the various achievements of these long-term satellite measurements, an observation/discovery of a ground-based state of FACs which includes a pair of large-scale FACs in the polar cap under both positive and negative IMF <I>B<sub>z</sub></I> has been pointed out. The FAC pattern is qualitatively and quantitatively consistent with experimental data for both polar cap FAC and Region 1 and Region 2 FAC systems.https://www.ann-geophys.net/26/281/2008/angeo-26-281-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author P. Nenovski
spellingShingle P. Nenovski
Comparison of simulated and observed large-scale, field-aligned current structures
Annales Geophysicae
author_facet P. Nenovski
author_sort P. Nenovski
title Comparison of simulated and observed large-scale, field-aligned current structures
title_short Comparison of simulated and observed large-scale, field-aligned current structures
title_full Comparison of simulated and observed large-scale, field-aligned current structures
title_fullStr Comparison of simulated and observed large-scale, field-aligned current structures
title_full_unstemmed Comparison of simulated and observed large-scale, field-aligned current structures
title_sort comparison of simulated and observed large-scale, field-aligned current structures
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-02-01
description Recently, a model of large-scale, field-aligned current (FAC) structures, based on zero-frequency MHD surface wave (SW) modes that can emerge from the solar wind-Earth's magnetosphere interaction, has been proposed. The FAC polarity and intensity distribution are quantified as a function of the solar wind parameters and the interplanetary magnetic field (IMF) magnitude that enter as input parameters. Besides, there are input parameters intrinsic to the Earth's magnetosphere &ndash; the size of the polar cap and the boundary regions and their plasma density variations. Influence of the IMF <I>B<sub>y</sub></I> component on the FAC structure is examined here. Depending on the IMF <I>B<sub>y</sub></I> magnitude, the predicted six-cell FAC structure tends to evolve in a spiral-like fashion. This large-scale FAC model is compared with experimental evidences and empirical FAC models based on DE-2 satellite data and high-precision Oersted and Magsat satellite magnetometer data. Among the various achievements of these long-term satellite measurements, an observation/discovery of a ground-based state of FACs which includes a pair of large-scale FACs in the polar cap under both positive and negative IMF <I>B<sub>z</sub></I> has been pointed out. The FAC pattern is qualitatively and quantitatively consistent with experimental data for both polar cap FAC and Region 1 and Region 2 FAC systems.
url https://www.ann-geophys.net/26/281/2008/angeo-26-281-2008.pdf
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