Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation study

We investigate with the help of a magnetohydrodynamic (MHD) model how the large-scale topology of the magnetosphere develops for a constant interplanetary magnetic field (IMF) with different IMF clock angles and for an IMF <i>B<sub>y</sub></i> sign change during northward...

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Main Authors: A. Kullen, P. Janhunen
Format: Article
Language:English
Published: Copernicus Publications 2004-03-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/951/2004/angeo-22-951-2004.pdf
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author A. Kullen
P. Janhunen
author_facet A. Kullen
P. Janhunen
author_sort A. Kullen
collection DOAJ
description We investigate with the help of a magnetohydrodynamic (MHD) model how the large-scale topology of the magnetosphere develops for a constant interplanetary magnetic field (IMF) with different IMF clock angles and for an IMF <i>B<sub>y</sub></i> sign change during northward IMF. A detailed examination of the topological changes in the tail and the ionosphere for different IMF conditions shows a good agreement with observational results. </p><p style="line-height: 20px;"> The MHD simulations for different constant IMF clock angle cases show the expected field-line bending and tail twisting for nonzero IMF <i>B<sub>y</sub></i>. The tail becomes longer and at its tailward end stronger twisted for IMF <i>B<sub>z</sub></i>>&#x2223;<i>B<sub>y</sub></i>&#x2223; than for IMF <i>B<sub>z</sub></i><&#x2223;<i>B<sub>y</sub></i>&#x2223;. The field lines originating in the high-latitude flank of the far-tail plasma sheet map into the near-Earth tail lobes and to a strongly poleward displaced polar cap boundary. A comparison with observations suggests that an oval-aligned arc may occur on the high-latitude part of the polar cap boundary. </p><p style="line-height: 20px;"> An IMF <i>B<sub>y</sub></i> sign change causes large deformations of the tail. After the IMF <i>B<sub>y</sub></i> flip the near-Earth and far-tail plasma sheet regions are oppositely twisted which causes in the near-Earth tail a bifurcation of the closed field line region that moves from one flank to the other. The bifurcated part of the closed field line region maps to a bridge of closed field lines moving over the entire polar cap. This moving bridge may be interpreted as the mapped region of a moving transpolar arc. Based on earlier observations, such a type of polar arcs is expected to occur after an IMF <i>B<sub>y</sub></i> sign change.<br><br> <b>Key words. </b>Ionosphere (auroral ionosphere; ionospheremagnetosphere interactions). Space plasma physics (numerical simulation studies)
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spelling doaj.art-9156f4c89b1147d2aa5fb972dfb744ba2022-12-22T01:15:37ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-03-012295197010.5194/angeo-22-951-2004Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation studyA. Kullen0P. Janhunen1Alfvén Laboratory, Royal Institute of Technology, Stockholm, SwedenGeophysical Research, Finnish Meteorological Institute, Helsinki, FinlandWe investigate with the help of a magnetohydrodynamic (MHD) model how the large-scale topology of the magnetosphere develops for a constant interplanetary magnetic field (IMF) with different IMF clock angles and for an IMF <i>B<sub>y</sub></i> sign change during northward IMF. A detailed examination of the topological changes in the tail and the ionosphere for different IMF conditions shows a good agreement with observational results. </p><p style="line-height: 20px;"> The MHD simulations for different constant IMF clock angle cases show the expected field-line bending and tail twisting for nonzero IMF <i>B<sub>y</sub></i>. The tail becomes longer and at its tailward end stronger twisted for IMF <i>B<sub>z</sub></i>>&#x2223;<i>B<sub>y</sub></i>&#x2223; than for IMF <i>B<sub>z</sub></i><&#x2223;<i>B<sub>y</sub></i>&#x2223;. The field lines originating in the high-latitude flank of the far-tail plasma sheet map into the near-Earth tail lobes and to a strongly poleward displaced polar cap boundary. A comparison with observations suggests that an oval-aligned arc may occur on the high-latitude part of the polar cap boundary. </p><p style="line-height: 20px;"> An IMF <i>B<sub>y</sub></i> sign change causes large deformations of the tail. After the IMF <i>B<sub>y</sub></i> flip the near-Earth and far-tail plasma sheet regions are oppositely twisted which causes in the near-Earth tail a bifurcation of the closed field line region that moves from one flank to the other. The bifurcated part of the closed field line region maps to a bridge of closed field lines moving over the entire polar cap. This moving bridge may be interpreted as the mapped region of a moving transpolar arc. Based on earlier observations, such a type of polar arcs is expected to occur after an IMF <i>B<sub>y</sub></i> sign change.<br><br> <b>Key words. </b>Ionosphere (auroral ionosphere; ionospheremagnetosphere interactions). Space plasma physics (numerical simulation studies)https://www.ann-geophys.net/22/951/2004/angeo-22-951-2004.pdf
spellingShingle A. Kullen
P. Janhunen
Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation study
Annales Geophysicae
title Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation study
title_full Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation study
title_fullStr Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation study
title_full_unstemmed Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation study
title_short Relation of polar auroral arcs to magnetotail twisting and IMF rotation: a systematic MHD simulation study
title_sort relation of polar auroral arcs to magnetotail twisting and imf rotation a systematic mhd simulation study
url https://www.ann-geophys.net/22/951/2004/angeo-22-951-2004.pdf
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