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Helium in the polar windThe coupled time-dependent continuity, momentum, and energy equations for four charged species (H(+), He(+), O(+) and electrons) moving through a stationary upper neutral atmosphere (composed of O2, N2, O, He, and H) were solved along open geomagnetic field lines using a modified version of the Gombosi et al. (1985) model. The thermospheric densities and temperatures, obtained from the MSIS-86 model (Hedin, 1987), were used to calculate neutral-ion sources, sinks, and collision frequencies. The various cross sections and conductivities employed by the Gombosi et al. model were also updated. The paper presents the first time-dependent solutions for the He(+) component of the polar wind. Special attention is paid to the solar cycle variation of the ion upflows.
Document ID
19920037273
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Gombosi, T. I.
(Michigan Univ. Ann Arbor, MI, United States)
Kerr, L. K.
(Michigan Univ. Ann Arbor, MI, United States)
Nagy, A. F.
(Michigan Univ. Ann Arbor, MI, United States)
Cannata, R. W.
(Michigan, University Ann Arbor, United States)
Date Acquired
August 15, 2013
Publication Date
January 1, 1992
Publication Information
Publication: Advances in Space Research
Volume: 12
Issue: 6 19
ISSN: 0273-1177
Subject Category
Geophysics
Report/Patent Number
ISSN: 0273-1177
Accession Number
92A19897
Funding Number(s)
CONTRACT_GRANT: NAGW-2162
CONTRACT_GRANT: NSF ATM-89-08183
Distribution Limits
Public
Copyright
Other

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