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Magnetic field studies by Voyager 2 - Preliminary results at SaturnResults of Voyager 2 studies of the magnetosphere and planetary magnetic field of Saturn are presented. Magnetometer studies have confirmed the results obtained by Voyager 1, indicating the magnetic field to be that of a centered dipole of moment 0.21 gauss Saturn radii-cubed, tilted approximately 0.8 deg from the rotation axis and a maximum measured field intensity of 1187 nT at latitude 17.3 deg N just before periapsis. Voyager 2 observed multiple bow shock and magnetopause crossings during its inbound and outbound trajectories, which were complementary to those of Voyager 1, including magnetopause crossing at 18.5 Saturn radii on the inbound trajectory, and at 48.4-50.9 Saturn radii outbound indicative of magnetospheric expansion due to changing solar wind conditions. Throughout the outbound passage, the magnetospheric field was observed to be relatively steady and smooth, with no evidence for any azimuthal asymmetry or magnetic anomaly. Results thus are incapable of accounting for the observed periodic modulation of the Saturnian kilometric radio emissions.
Document ID
19820036472
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Ness, N. F.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Acuna, M. H.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Behannon, K. W.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Burlaga, L. F.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Connerney, J. E. P.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Lepping, R. P.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Neubauer, F. M.
(Braunschweig, Technische Universitaet Braunschweig, Germany)
Date Acquired
August 10, 2013
Publication Date
January 29, 1982
Publication Information
Publication: Science
Volume: 215
Subject Category
Lunar And Planetary Exploration
Accession Number
82A20007
Distribution Limits
Public
Copyright
Other

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