Abstract
GEOPHYSICAL RESEARCH LETTERS,
VOL. 13, NO. 4,
PP. 397-400, 1986
doi:10.1029/GL013i004p00397
Simulation of the solar wind interaction with the outer regions of the Coma
Institute of Geophysics and Planetary Physics University of California, Los Angeles
Los Alamos National Laboratory Los Alamos, New Mexico
Interaction of the solar wind with newly born cometary ions (O+) is studied through hybrid simulations (particle ions, fluid electrons). The results show that depending on the orientation of the interplanetary magnetic field (IMF) with respect to the solar wind velocity, two kinds of interaction are possible. When IMF is exactly or nearly parallel to the solar wind velocity, momentum transfer between the protons and the O+ ions takes place solely through the excitation of large amplitude electromagnetic waves. On the other hand, as IMF becomes more oblique to the solar wind velocity, momentum transfer occurs on a faster time scale through the motional electric field in the solar wind. This more rapid deceleration can lead to the formation of a shock.
Received 11 February 1986; accepted 6 March 1986; .
Citation: (1986), Simulation of the solar wind interaction with the outer regions of the Coma, Geophys. Res. Lett., 13(4), 397–400, doi:10.1029/GL013i004p00397.
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