The cusp: a window for particle exchange between the radiation belt and the solar wind

The study focuses on a single particle dynamics in the cusp region. The topology of the cusp region in terms of magnetic field iso-B contours has been studied using the Tsyganenko 96 model (T96) as an example, to show the importance of an off-equatorial minimum on particle trapping. We carry out...

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Main Authors: X.-Z. Zhou, T. A. Fritz, Q.-G. Zong, Z. Y. Pu, Y.-Q. Hao, J.-B. Cao
Format: Article
Language:English
Published: Copernicus Publications 2006-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/24/3131/2006/angeo-24-3131-2006.pdf
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author X.-Z. Zhou
X.-Z. Zhou
T. A. Fritz
Q.-G. Zong
Q.-G. Zong
Z. Y. Pu
Y.-Q. Hao
J.-B. Cao
author_facet X.-Z. Zhou
X.-Z. Zhou
T. A. Fritz
Q.-G. Zong
Q.-G. Zong
Z. Y. Pu
Y.-Q. Hao
J.-B. Cao
author_sort X.-Z. Zhou
collection DOAJ
description The study focuses on a single particle dynamics in the cusp region. The topology of the cusp region in terms of magnetic field iso-B contours has been studied using the Tsyganenko 96 model (T96) as an example, to show the importance of an off-equatorial minimum on particle trapping. We carry out test particle simulations to demonstrate the bounce and drift motion. The "cusp trapping limit" concept is introduced to reflect the particle motion in the high latitude magnetospheric region. The spatial distribution of the "cusp trapping limit" shows that only those particles with near 90° pitch-angles can be trapped and drift around the cusp. Those with smaller pitch angles may be partly trapped in the iso-B contours, however, they will eventually escape along one of the magnetic field lines. There exist both open field lines and closed ones within the same drift orbit, indicating two possible destinations of these particles: those particles being lost along open field lines will be connected to the surface of the magnetopause and the solar wind, while those along closed ones will enter the equatorial radiation belt. Thus, it is believed that the cusp region can provide a window for particle exchange between these two regions. Some of the factors, such as dipole tilt angle, magnetospheric convection, IMF and the Birkeland current system, may influence the cusp's trapping capability and therefore affect the particle exchanging mechanism. Their roles are examined by both the analysis of cusp magnetic topology and test particle simulations.
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spelling doaj.art-c9a7c43c659e46739f32c65ec32f02bb2022-12-21T18:10:28ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762006-11-01243131313710.5194/angeo-24-3131-2006The cusp: a window for particle exchange between the radiation belt and the solar windX.-Z. Zhou0X.-Z. Zhou1T. A. Fritz2Q.-G. Zong3Q.-G. Zong4Z. Y. Pu5Y.-Q. Hao6J.-B. Cao7Institute of Space Physics and Applied Technology, Peking University, Beijing 100871, ChinaKey Laboratory for Space Weather, Chinese Academy of Sciences, Beijing, ChinaCenter for Space Physics, Boston University, Boston, MA 02215, USAKey Laboratory for Space Weather, Chinese Academy of Sciences, Beijing, ChinaCenter for Atmospheric Research, University of Massachusetts, Lowell, MA 01854, USAInstitute of Space Physics and Applied Technology, Peking University, Beijing 100871, ChinaInstitute of Space Physics and Applied Technology, Peking University, Beijing 100871, ChinaKey Laboratory for Space Weather, Chinese Academy of Sciences, Beijing, ChinaThe study focuses on a single particle dynamics in the cusp region. The topology of the cusp region in terms of magnetic field iso-B contours has been studied using the Tsyganenko 96 model (T96) as an example, to show the importance of an off-equatorial minimum on particle trapping. We carry out test particle simulations to demonstrate the bounce and drift motion. The "cusp trapping limit" concept is introduced to reflect the particle motion in the high latitude magnetospheric region. The spatial distribution of the "cusp trapping limit" shows that only those particles with near 90° pitch-angles can be trapped and drift around the cusp. Those with smaller pitch angles may be partly trapped in the iso-B contours, however, they will eventually escape along one of the magnetic field lines. There exist both open field lines and closed ones within the same drift orbit, indicating two possible destinations of these particles: those particles being lost along open field lines will be connected to the surface of the magnetopause and the solar wind, while those along closed ones will enter the equatorial radiation belt. Thus, it is believed that the cusp region can provide a window for particle exchange between these two regions. Some of the factors, such as dipole tilt angle, magnetospheric convection, IMF and the Birkeland current system, may influence the cusp's trapping capability and therefore affect the particle exchanging mechanism. Their roles are examined by both the analysis of cusp magnetic topology and test particle simulations.https://www.ann-geophys.net/24/3131/2006/angeo-24-3131-2006.pdf
spellingShingle X.-Z. Zhou
X.-Z. Zhou
T. A. Fritz
Q.-G. Zong
Q.-G. Zong
Z. Y. Pu
Y.-Q. Hao
J.-B. Cao
The cusp: a window for particle exchange between the radiation belt and the solar wind
Annales Geophysicae
title The cusp: a window for particle exchange between the radiation belt and the solar wind
title_full The cusp: a window for particle exchange between the radiation belt and the solar wind
title_fullStr The cusp: a window for particle exchange between the radiation belt and the solar wind
title_full_unstemmed The cusp: a window for particle exchange between the radiation belt and the solar wind
title_short The cusp: a window for particle exchange between the radiation belt and the solar wind
title_sort cusp a window for particle exchange between the radiation belt and the solar wind
url https://www.ann-geophys.net/24/3131/2006/angeo-24-3131-2006.pdf
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