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Zimbardo & Veltri 1996
Zimbardo, G. and Veltri, P. (1996). Spreading and intermittent structure of the upstream boundary of planetary magnetic foreshocks. Geophysical Research Letters 23: doi: 10.1029/96GL00660. issn: 0094-8276.

The fast particles in the electron foreshocks propagate along the magnetic field lines, so that the effect of low frequency magnetic fluctuations is to create both a broadening and a fine structure of the foreshock upstream boundary. This is studied by means of a 3-D numerical simulation of turbulent magnetic fields. Applications to Venus, Earth, and Mars magnetic foreshocks are done. It is found that a spacecraft can be magnetically connected to the bow shock even when it is upstream of the nominal magnetic foreshock boundary, and that the mixing of magnetic field lines can give an explanation for the broadband bursty electrostatic noise observed within the electron foreshock. ¿ American Geophysical Union 1996

BACKGROUND DATA FILES

Abstract

Keywords
Interplanetary Physics, Planetary bow shocks, Space Plasma Physics, Nonlinear phenomena, Space Plasma Physics, Shock waves, Space Plasma Physics, Transport processes
Journal
Geophysical Research Letters
http://www.agu.org/journals/gl/
Publisher
American Geophysical Union
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