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Journal ArticleDOI

A time-averaged regional model of the Hermean magnetic field

TLDR
In this article, the authors presented the first regional model of the magnetic field of Mercury developed with mathematical continuous functions, which has a horizontal spatial resolution of about 830 km at the surface of the planet, and it is derived without any a priori information about the geometry of the internal and external fields.
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This article is published in Physics of the Earth and Planetary Interiors.The article was published on 2017-09-01. It has received 20 citations till now. The article focuses on the topics: Dipole model of the Earth's magnetic field & L-shell.

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Citations
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Investigating Mercury’s Environment with the Two-Spacecraft BepiColombo Mission

Anna Milillo, +79 more
TL;DR: The ESA-JAXA BepiColombo mission will provide simultaneous measurements from two spacecraft, offering an unprecedented opportunity to investigate magnetospheric and exospheric dynamics at Mercury as well as their interactions with the solar wind, radiation, and interplanetary dust.
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Mercury’s anomalous magnetic field caused by a symmetry-breaking self-regulating dynamo

TL;DR: A numerical dynamo model is presented that can re-produce both the axisymmetric and anomalously axially offset dipolar magnetic field of Mercury and produces magnetic fields similar in morphology and strength to that of Mercury.
References
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Journal ArticleDOI

International Geomagnetic Reference Field: the 12th generation

TL;DR: The 12th generation of the International Geomagnetic Reference Field (IGRF) was adopted in December 2014 by the Working Group V-MOD appointed by the International Association of Geomagnetism and Aeronomy (IAGA) as discussed by the authors.
Book

Foundations of geomagnetism

TL;DR: In this article, the Mie representation of the main field has been studied in the context of classical electrodynamics and spherical harmonics, as well as Gauss' theory of main field and hydromagnetics.
Journal ArticleDOI

The magnetic field of Mercury, 1

TL;DR: In this article, an updated analysis and interpretation of the magnetic field observations obtained during the Mariner 10 encounter with the planet Mercury on March 29, 1974 is presented, which leads to the conclusion that an internal planetary magnetic field exists with dipole moment approximately 5.1 × 1022 G cm³.
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