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Nonlinear generation of whistler waves by an ion beamAn electromagnetic hybrid code is used to simulate a new mechanism for whistler wave generation by an ion beam. First, a field-aligned ion beam becomes unstable to the electromagnetic ion/ion right-hand resonant instability which generates large amplitude MHD-like waves. These waves then trap the ion beam and increase its effective temperature anisotropy. As a result, the growth rates of the electron/whistler instability are significantly enhanced, and whistlers start to grow above the noise level. At the same time, because of the reduced parallel drift speed of the ion beam, the frequencies of the whistlers are also downshifted. Full simulations were performed to isolate and separately investigate the electron/ion whistler instability. The results are in agreement with the assumption of fluid electrons in the hybrid simulations and with the linear theory of the instability.
Document ID
19900033704
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Akimoto, K.
(Los Alamos National Lab. NM, United States)
Winske, D.
(Los Alamos National Laboratory NM, United States)
Date Acquired
August 14, 2013
Publication Date
December 1, 1989
Publication Information
Publication: Journal of Geophysical Research
Volume: 94
ISSN: 0148-0227
Subject Category
Geophysics
Accession Number
90A20759
Funding Number(s)
CONTRACT_GRANT: NASA ORDER W-17002
Distribution Limits
Public
Copyright
Other

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