Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere

During substorms the magnetic field configuration changes in time; stretching of the magnetosphere during growth phase is followed by its collapse after the onset of the expansion phase. In this study the ionospheric origin oxygen ion dynamics in a time-dependent magnetosphere is analyzed. An induct...

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Main Author: E. B. Wodnicka
Format: Article
Language:English
Published: Copernicus Publications 1996-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/3/221/1996/npg-3-221-1996.pdf
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spelling doaj-31ed3b04196a40748db7d7e739b4340a2020-11-24T22:42:42ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79461996-01-0133221227Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphereE. B. WodnickaDuring substorms the magnetic field configuration changes in time; stretching of the magnetosphere during growth phase is followed by its collapse after the onset of the expansion phase. In this study the ionospheric origin oxygen ion dynamics in a time-dependent magnetosphere is analyzed. An induction electric field of several mV/m due to the reconfigurating magnetic field determines the details of the ion extraction from the auroral topside ionosphere. Two regimes of motion are discernible; a regime in regions far from the equatorial plane where the magnetic moment is conserved and a regime near the equatorial plane, in which the motion produces magnetic moment jumps and oscillations. The time spent by the ion in the regions is determined by the initial characteristics of the ion and by the field transition features. Lyapunov characteristic exponents are calculated to estimate the sensitivity of the system to initial conditions. Their values are higher for orbits with chaotic segments compared with the orbits in the static magnetic field and depend on the amplitude of the induced electric field. It follows from the study that the region of chaos usually localized far beyond 10 R<sub>E </sub>in the plasma sheet is expected to approach closer to the Earth ( r = 6 - 7 R<sub>E</sub>) during substorm associated reconfigurations of the magnetosphere, due to the auroral ionospheric ions.http://www.nonlin-processes-geophys.net/3/221/1996/npg-3-221-1996.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. B. Wodnicka
spellingShingle E. B. Wodnicka
Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere
Nonlinear Processes in Geophysics
author_facet E. B. Wodnicka
author_sort E. B. Wodnicka
title Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere
title_short Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere
title_full Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere
title_fullStr Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere
title_full_unstemmed Conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere
title_sort conjectured chaotic nature of the ionosphere-magnetosphere coupling in a reconfigurating magnetosphere
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 1996-01-01
description During substorms the magnetic field configuration changes in time; stretching of the magnetosphere during growth phase is followed by its collapse after the onset of the expansion phase. In this study the ionospheric origin oxygen ion dynamics in a time-dependent magnetosphere is analyzed. An induction electric field of several mV/m due to the reconfigurating magnetic field determines the details of the ion extraction from the auroral topside ionosphere. Two regimes of motion are discernible; a regime in regions far from the equatorial plane where the magnetic moment is conserved and a regime near the equatorial plane, in which the motion produces magnetic moment jumps and oscillations. The time spent by the ion in the regions is determined by the initial characteristics of the ion and by the field transition features. Lyapunov characteristic exponents are calculated to estimate the sensitivity of the system to initial conditions. Their values are higher for orbits with chaotic segments compared with the orbits in the static magnetic field and depend on the amplitude of the induced electric field. It follows from the study that the region of chaos usually localized far beyond 10 R<sub>E </sub>in the plasma sheet is expected to approach closer to the Earth ( r = 6 - 7 R<sub>E</sub>) during substorm associated reconfigurations of the magnetosphere, due to the auroral ionospheric ions.
url http://www.nonlin-processes-geophys.net/3/221/1996/npg-3-221-1996.pdf
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