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The low energy plasma in the Uranian magnetosphereThe Plasma Science experiment on Voyager 2 detected a magnetosphere filled with a tenuous plasma, rotating with the planet. Temperatures of the plasma, composed of protons and electrons, ranged from 10 eV to about 1 keV. The sources of these protons and electrons are probably the ionosphere of Uranus or the extended neutral hydrogen cloud surrounding the planet. As at earth, Jupiter, and Saturn, there is an extended magnetotail with a central plasma sheet. Although similar in global structure to the magnetospheres of these planets, the large angle between the rotation and magnetic axes of the planet and the orientation of the rotation axis with respect to the solar wind flow make the Uranian magnetosphere unique.
Document ID
19880041975
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Mcnutt, R. L., Jr.
(Massachusetts Inst. of Tech. Cambridge, MA, United States)
Belcher, J.
(Massachusetts Inst. of Tech. Cambridge, MA, United States)
Bridge, H.
(Massachusetts Inst. of Tech. Cambridge, MA, United States)
Lazarus, A. J.
(Massachusetts Inst. of Tech. Cambridge, MA, United States)
Richardson, J.
(Massachusetts Inst. of Tech. Cambridge, MA, United States)
Sands, M.
(MIT Cambridge, MA, United States)
Bagenal, F.
(Imperial College of Science and Technology London, United Kingdom)
Eviatar, A.
(Tel Aviv University Israel)
Goertz, C.
(Iowa, University Iowa City, United States)
Ogilvie, K.
(NASA Goddard Space Flight Center Greenbelt, MD, United States)
Date Acquired
August 13, 2013
Publication Date
January 1, 1987
Publication Information
Publication: Advances in Space Research
Volume: 7
Issue: 12 1
ISSN: 0273-1177
Subject Category
Lunar And Planetary Exploration
Accession Number
88A29202
Funding Number(s)
CONTRACT_GRANT: JPL-953733
Distribution Limits
Public
Copyright
Other

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