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Surface waves on Uranus' magnetopauseUranus' magnetosphere has a well-developed, thick magnetopause that was fully traversed twice by Voyager 2, once inbound to the planet and once outbound. This boundary appears to resemble earth's magnetopause in approximate shape and even to the extent of supporting surface waves which were observed on the inbound pass at a distance of 18.3 Uranus radii. There were apparently eight partial transitions from the magnetosheath into the current sheet of the magnetopause at this time, followed by a final complete transition to the magnetosphere. Six of the estimated normal vectors to the local boundary show clear evidence of oscillations in the slope with typical angular excursions, from one partial transition to the next, of about 90 deg. The vectors oscillated approximately in a plane that was severely tilted by about 49 deg with respect to Uranus' orbital plane.
Document ID
19880039616
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Lepping, R. P.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Burlaga, L. F.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Klein, L. W.
(Applied Research Corp. Landover, MD, United States)
Date Acquired
August 13, 2013
Publication Date
December 30, 1987
Publication Information
Publication: Journal of Geophysical Research
Volume: 92
ISSN: 0148-0227
Subject Category
Lunar And Planetary Exploration
Report/Patent Number
ISSN: 0148-0227
Accession Number
88A26843
Distribution Limits
Public
Copyright
Other

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