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Nonlinear Processes in Geophysics An interactive open-access journal of the European Geosciences Union

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Nonlin. Processes Geophys., 20, 163-178, 2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
21 Feb 2013
Ion motion in the current sheet with sheared magnetic field – Part 1: Quasi-adiabatic theory
A. V. Artemyev1,2, A. I. Neishtadt1,3, and L. M. Zelenyi1 1Space Research Institute, RAS, Profsouznaya st., 84/32, GSP-7, 117997 Moscow, Russia
2Laboratoire de physique et chimie de l'environnement et de l'Espace (LPC2E), UMR7328, CNRS – Université d'Orléans, 3A, Avenue de la Recherche Scientifique, 45071 Orleans cedex 2, France
3Department of Mathematical Sciences, Loughborough University, Loughborough LE11 3TU, UK
Abstract. We present a theory of trapped ion motion in the magnetotail current sheet with a constant dawn–dusk component of the magnetic field. Particle trajectories are described analytically using the quasi-adiabatic invariant corresponding to averaging of fast oscillations around the tangential component of the magnetic field. We consider particle dynamics in the quasi-adiabatic approximation and demonstrate that the principal role is played by large (so called geometrical) jumps of the quasi-adiabatic invariant. These jumps appear due to the current sheet asymmetry related to the presence of the dawn–dusk magnetic field. The analytical description is compared with results of numerical integration. We show that there are four possible regimes of particle motion. Each regime is characterized by certain ranges of values of the dawn–dusk magnetic field and particle energy. We find the critical value of the dawn–dusk magnetic field, where jumps of the quasi-adiabatic invariant vanish.

Citation: Artemyev, A. V., Neishtadt, A. I., and Zelenyi, L. M.: Ion motion in the current sheet with sheared magnetic field – Part 1: Quasi-adiabatic theory, Nonlin. Processes Geophys., 20, 163-178,, 2013.
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