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Voyager 2 radio observations of UranusVoyager 2 detected continuous radio signals in the 40-100 kHz interval starting from 5 days before passage of Uranus. The radio signals reached 800 kHz within 4 days of closest approach and continued throughout the outward bound phase of flight. The signals were modulated with a period close to 17.24 days, the same period calculated for the rotation of the Uranus magnetosphere with other spacecraft data. The planet was also found to have an off-center magnetic field, and radio signals were strongest when the dipole center was on the nightside of Uranus. Dynamic spectral and burst events which were recorded indicated that Uranus, like the earth, has a strongly defined plasmasphere. It moves under the control of magnetic force tubes that interact with the magnetosphere boundary, producing a variety of MHD phenomena.
Document ID
19860059524
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Warwick, J. W.
(Radiophysics, Inc. Boulder, CO, United States)
Evans, D. R.
(Radiophysics, Inc. Boulder, CO, United States)
Romig, J. H.
(Radiophysics, Inc. Boulder, CO, United States)
Sawyer, C. B.
(Radiophysics, Inc. Boulder, CO, United States)
Desch, M. D.
(Radiophysics, Inc. Boulder, CO, United States)
Kaiser, M. L.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Alexander, J. K.
(NASA Headquarters Washington, DC United States)
Gulkis, S.
(Radiophysics, Inc. Boulder, CO, United States)
Poynter, R. L.
(California Institute of Technology Jet Propulsion Laboratory, Pasadena, United States)
Date Acquired
August 12, 2013
Publication Date
July 4, 1986
Publication Information
Publication: Science
Volume: 233
ISSN: 0036-8075
Subject Category
Lunar And Planetary Exploration
Accession Number
86A44262
Distribution Limits
Public
Copyright
Other

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