The Mie representation for Mercury’s magnetospheric currents
Abstract Poloidal–toroidal magnetic field decomposition is a useful application of the Mie representation and the decomposition method enables us to determine the current density observationally and unambiguously in the local region of magnetic field measurement. The application and the limits of th...
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2021
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oai:doaj.org-article:ba331abb47694682b97ccfe659a4127d2021-11-14T12:30:47ZThe Mie representation for Mercury’s magnetospheric currents10.1186/s40623-021-01536-81880-5981https://doaj.org/article/ba331abb47694682b97ccfe659a4127d2021-11-01T00:00:00Zhttps://doi.org/10.1186/s40623-021-01536-8https://doaj.org/toc/1880-5981Abstract Poloidal–toroidal magnetic field decomposition is a useful application of the Mie representation and the decomposition method enables us to determine the current density observationally and unambiguously in the local region of magnetic field measurement. The application and the limits of the decomposition method are tested against the Mercury magnetic field simulation in view of BepiColombo’s arrival at Mercury in 2025. The simulated magnetic field data are evaluated along the planned Mercury Planetary Orbiter (MPO) trajectories and the current system that is crossed by the spacecraft is extracted from the magnetic field measurements. Afterwards, the resulting currents are classified in terms of the established current system in the vicinity of Mercury. Graphical AbstractS. ToepferY. NaritaW. ExnerD. HeynerP. KolheyK. -H. GlassmeierU. MotschmannSpringerOpenarticlePoloidal–toroidal decompositionMagnetospheric current systemsCapon’s methodGeography. Anthropology. RecreationGGeodesyQB275-343GeologyQE1-996.5ENEarth, Planets and Space, Vol 73, Iss 1, Pp 1-14 (2021) |
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DOAJ |
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Poloidal–toroidal decomposition Magnetospheric current systems Capon’s method Geography. Anthropology. Recreation G Geodesy QB275-343 Geology QE1-996.5 |
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Poloidal–toroidal decomposition Magnetospheric current systems Capon’s method Geography. Anthropology. Recreation G Geodesy QB275-343 Geology QE1-996.5 S. Toepfer Y. Narita W. Exner D. Heyner P. Kolhey K. -H. Glassmeier U. Motschmann The Mie representation for Mercury’s magnetospheric currents |
description |
Abstract Poloidal–toroidal magnetic field decomposition is a useful application of the Mie representation and the decomposition method enables us to determine the current density observationally and unambiguously in the local region of magnetic field measurement. The application and the limits of the decomposition method are tested against the Mercury magnetic field simulation in view of BepiColombo’s arrival at Mercury in 2025. The simulated magnetic field data are evaluated along the planned Mercury Planetary Orbiter (MPO) trajectories and the current system that is crossed by the spacecraft is extracted from the magnetic field measurements. Afterwards, the resulting currents are classified in terms of the established current system in the vicinity of Mercury. Graphical Abstract |
format |
article |
author |
S. Toepfer Y. Narita W. Exner D. Heyner P. Kolhey K. -H. Glassmeier U. Motschmann |
author_facet |
S. Toepfer Y. Narita W. Exner D. Heyner P. Kolhey K. -H. Glassmeier U. Motschmann |
author_sort |
S. Toepfer |
title |
The Mie representation for Mercury’s magnetospheric currents |
title_short |
The Mie representation for Mercury’s magnetospheric currents |
title_full |
The Mie representation for Mercury’s magnetospheric currents |
title_fullStr |
The Mie representation for Mercury’s magnetospheric currents |
title_full_unstemmed |
The Mie representation for Mercury’s magnetospheric currents |
title_sort |
mie representation for mercury’s magnetospheric currents |
publisher |
SpringerOpen |
publishDate |
2021 |
url |
https://doaj.org/article/ba331abb47694682b97ccfe659a4127d |
work_keys_str_mv |
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