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Wave-particle interactions in the Venus wake and tailThe first descriptions of combined tail measurements from the Pioneer Venus plasma analyzer, magnetometer, and plasma wave detector are presented. The analysis concentrates on those orbits which are representative of the first tail passage. Summary plasma analyzer parameters are used to show that waves occurring at the boundary of the magnetotail can be identified as Doppler-shifted ion acoustic oscillations. High-density plasma distributions in the magnetotail region usually appear to be non-Maxwellian at the highest time resolution. These distorted distribution functions are generally accompanied by enhanced plasma wave signals and magnetic field reversals indicative of electric currents. A different time for the spacecraft entrance into the magnetotail from that previously defined is identified. It is shown that the wave activity in the Venus tail appears similar to the broadband noise identified in the earth's tail, except that at Venus the levels are usually higher.
Document ID
19840034519
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Intriligator, D. S.
(Carmel Research Center Santa Monica, CA, United States)
Scarf, F. L.
(TRW Space and Technology Group Redondo Beach, CA, United States)
Date Acquired
August 12, 2013
Publication Date
January 1, 1984
Publication Information
Publication: Journal of Geophysical Research
Volume: 89
ISSN: 0148-0227
Subject Category
Lunar And Planetary Exploration
Accession Number
84A17306
Funding Number(s)
CONTRACT_GRANT: NAS2-10926
CONTRACT_GRANT: NAS2-9842
Distribution Limits
Public
Copyright
Other

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