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Stability of H(+) beams in the polar windThe effect of energetic H(+) beams on the stability of the polar wind in the classical model is studied with regard to the excitation of electrostatic waves. Consideration is given to cases covering a wide range of electron-to-background temperature ratios and beam-to-background ion density ratios, assuming a relatively cold beam. The minimum beam drift velocity required to destabilize the plasma is determined by a combination of the Nyquist technique and a direct solution of the plasma dispersion equation. It is found that the plasma can be destabilized for relative drift energies less than about 1 eV. Also, it is shown that the plasma is less stable for large electron temperatures and for comparable ion and beam densities.
Document ID
19890041563
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Barakat, A. R.
(Utah State Univ. Logan, UT, United States)
Schunk, R. W.
(Utah State University Logan, United States)
Date Acquired
August 14, 2013
Publication Date
February 1, 1989
Publication Information
Publication: Journal of Geophysical Research
Volume: 94
ISSN: 0148-0227
Subject Category
Geophysics
Accession Number
89A28934
Funding Number(s)
CONTRACT_GRANT: F49620-86-C-0109
CONTRACT_GRANT: NAGW-77
Distribution Limits
Public
Copyright
Other

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