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ReportsThe Structure of Mercury's Magnetic Field from MESSENGER's First Flyby
During its first flyby of Mercury, the MESSENGER spacecraft measured the planet's near-equatorial magnetic field. The field strength is consistent to within an estimated uncertainty of 10% with that observed near the equator by Mariner 10. Centered dipole solutions yield a southward planetary moment of 230 to 290 nanotesla RM3 (where RM is Mercury's mean radius) tilted between 5° and 12° from the rotation axis. Multipole solutions yield non-dipolar contributions of 22% to 52% of the dipole field magnitude. Magnetopause and tail currents account for part of the high-order field, and plasma pressure effects may explain the remainder, so that a pure centered dipole cannot be ruled out.
1 Johns Hopkins University Applied Physics Laboratory, 11100 Johns Hopkins Road, Laurel, MD 20723, USA.
2 Solar System Exploration Division, NASA Goddard Space Fight Center, Greenbelt, MD 20771, USA. 3 Department of Earth and Ocean Sciences, University of British Columbia, Vancouver, BC V6T 1Z4, Canada. 4 Heliophysics Science Division, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA. 5 Department of Terrestrial Magnetism, Carnegie Institution of Washington, Washington, DC 20015, USA. * To whom correspondence should be addressed. E-mail: brian.anderson{at}jhuapl.edu
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Science. ISSN 0036-8075 (print), 1095-9203 (online)