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The magnetosphere of Neptune - Its response to daily rotationThe Neptunian magnetosphere periodically changes every eight hours between a pole-on magnetosphere with only one polar cusp and an earth-type magnetosphere with two polar cusps. In the pole-on configuration, the tail current sheet has an almost circular shape with plasma currents closing entirely within the magnetosphere. Eight hours later the tail current sheet assumes an almost flat shape with plasma currents touching the magnetotail boundary and closing over the tail magnetopause. Magnetic field and tail current sheet configurations have been calculated in a three-dimensional model, but the plasma- and thermodynamic conditions were investigated in a simplified two-dimensional MHD equilibrium magnetosphere. It was found that the free energy in the tail region of the two-dimensional model becomes independent of the dipole tilt angle. It is conjectured that the Neptunian magnetotail might assume quasi-static equilibrium states that make the free energy of the system independent of its daily rotation.
Document ID
19900065489
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Voigt, Gerd-Hannes
(Rice University Houston, TX, United States)
Ness, Norman F.
(Bartol Research Institute Newark, DE, United States)
Date Acquired
August 14, 2013
Publication Date
September 1, 1990
Publication Information
Publication: Geophysical Research Letters
Volume: 17
ISSN: 0094-8276
Subject Category
Lunar And Planetary Exploration
Accession Number
90A52544
Funding Number(s)
CONTRACT_GRANT: NAGW-1833
CONTRACT_GRANT: NSF ATM-87-01208
Distribution Limits
Public
Copyright
Other

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