Centrifugal trapping in the magnetotail

Particles leaving the neutral sheet in the distant magnetotail at times display adiabatic trajectory sequences characterized by an inflection toward the equator and subsequent mirroring in its vicinity. We demonstrate that this low-latitude mirroring results primarily from a centrifugal deceleration...

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Main Authors: D. C. Delcourt, R. F. Martin, J. A. Sauvaud, T. E. Moore
Format: Article
Language:English
Published: Copernicus Publications
Series:Annales Geophysicae
Online Access:http://www.ann-geophys.net/13/242/1995/angeo-13-242-1995.html
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author D. C. Delcourt
R. F. Martin
J. A. Sauvaud
T. E. Moore
author_facet D. C. Delcourt
R. F. Martin
J. A. Sauvaud
T. E. Moore
author_sort D. C. Delcourt
collection DOAJ
description Particles leaving the neutral sheet in the distant magnetotail at times display adiabatic trajectory sequences characterized by an inflection toward the equator and subsequent mirroring in its vicinity. We demonstrate that this low-latitude mirroring results primarily from a centrifugal deceleration due to the fast direction-changing <strong>E</strong>×<strong>B</strong> drift. This effect which we refer to as "centrifugal trapping" appears both in guiding centre and full particle treatments. It thus does not directly relate to nonadiabatic motion. However, pitch angle scattering due to nonadiabatic neutral sheet interaction does play a role in reducing the parallel speed of the particles. We show that centrifugal trapping is an important mechanism for the confinement of the slowest (typically below the equatorial <strong>E</strong>×<strong>B</strong> drift speed) plasma sheet populations to the midplane vicinity.
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spelling doaj.art-4629521be8734e9097375161636daab92022-12-22T02:38:03ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-0576133242246Centrifugal trapping in the magnetotailD. C. DelcourtR. F. MartinJ. A. SauvaudT. E. MooreParticles leaving the neutral sheet in the distant magnetotail at times display adiabatic trajectory sequences characterized by an inflection toward the equator and subsequent mirroring in its vicinity. We demonstrate that this low-latitude mirroring results primarily from a centrifugal deceleration due to the fast direction-changing <strong>E</strong>×<strong>B</strong> drift. This effect which we refer to as "centrifugal trapping" appears both in guiding centre and full particle treatments. It thus does not directly relate to nonadiabatic motion. However, pitch angle scattering due to nonadiabatic neutral sheet interaction does play a role in reducing the parallel speed of the particles. We show that centrifugal trapping is an important mechanism for the confinement of the slowest (typically below the equatorial <strong>E</strong>×<strong>B</strong> drift speed) plasma sheet populations to the midplane vicinity.http://www.ann-geophys.net/13/242/1995/angeo-13-242-1995.html
spellingShingle D. C. Delcourt
R. F. Martin
J. A. Sauvaud
T. E. Moore
Centrifugal trapping in the magnetotail
Annales Geophysicae
title Centrifugal trapping in the magnetotail
title_full Centrifugal trapping in the magnetotail
title_fullStr Centrifugal trapping in the magnetotail
title_full_unstemmed Centrifugal trapping in the magnetotail
title_short Centrifugal trapping in the magnetotail
title_sort centrifugal trapping in the magnetotail
url http://www.ann-geophys.net/13/242/1995/angeo-13-242-1995.html
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