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The Induced Magnetosphere of Mars: Asymmetrical Topology of the Magnetic Field Lines

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Dubinin,  E. M.
Department Planets and Comets, Max Planck Institute for Solar System Research, Max Planck Society;

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Fränz,  Markus
Department Planets and Comets, Max Planck Institute for Solar System Research, Max Planck Society;

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Woch,  Joachim
Department Sun and Heliosphere, Max Planck Institute for Solar System Research, Max Planck Society;

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引用

Dubinin, E. M., Modolo, R., Fränz, M., Päetzold, M., Woch, J., Chai, L., Wei, Y., Connerney, J. E. P., Mcfadden, J., DiBraccio, G., Espley, J., Grigorenko, E., & Zelenyi, L. (2019). The Induced Magnetosphere of Mars: Asymmetrical Topology of the Magnetic Field Lines. Geophysical Research Letters, 46(22), 12722-12730. doi:10.1029/2019GL084387.


引用: https://hdl.handle.net/21.11116/0000-0005-8663-4
要旨
An asymmetrical pileup of the interplanetary magnetic field leads to an additional draping of the field lines in the opposite direction to the motional electric field. Such a draping and the associated magnetic field forces push the ionosphere plasma in the transverse direction opening a passage for an ion trail which contains dense and slowly moving plasma. We found that wrapping of the field lines around Mars starts in the hemisphere pointing in the direction of the motional electric field and propagates to the opposite hemisphere where the cross‐flow component of the draped interplanetary magnetic field changes sign in a broad area accompanied by the formation of loops of closed field lines. Reconnection near Mars accompanied by the generation of plasma vortices imposes serious constraints on the ion dynamics and their escape through the tail. The existence of all these features is confirmed by hybrid simulations.