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Title: Structure of the quasi-parallel bow shock: Results of numerical simulations

Journal Article · · J. Geophys. Res.; (United States)

Quasi-parallel bowshock structures are simulated by using a one-dimensional nonperiodic hybrid code in which the ion dynamics are treated exactly while the electron dynamics are omitted by neglecting the electron inertia (m/sub e/ = 0) and pressure. The simulations are initialized with the upstream condition specified by theta/sub 1/ = 10/sup 0/, ..beta../sub 1/ = 0.5, and M/sub A/1 = 2 to 4 with 0.5 increment while the downstream condition is obtained from the Rankine-Hugoniot relations, where theta/sub 1/ is the angle between the shock normal and the magnetic field, ..beta../sub 1/ is the ratio of kinetic to magnetic pressures, and M/sub A/1 is the Alfven Mach number. The main results of our simulations follow: (1) For M/sub A/1<3, the magnetic field profile of the shock is laminar or quasi-laminar. The upstream waves are right-hand polarized whistlers with ..omega..approx. =3.2..cap omega../sub n/i in the plasma frame, where ..cap omega../sub n/i is the ion gyrofrequency based on the normal field component B/sub n/. This corresponds to a wave frequency fapprox. =0.25 Hz and wavelength lambdaapprox. =310 km under solar wind conditions. The downstream waves are absent or low in amplitudes. (2) For M/sub A/1 >3, the magnetic field profile of the shock is turbulent. The upstream waves are again right-hand polarized whistlers with wavelengths varying from lambdaapprox.310 km upstream to lambda> or approx. =1250 km downstream. The downstream waves are predominantly the right-hand polarized fast magnetosonic waves (..omega..< or approx. =..cap omega../sub i/).

Research Organization:
Geophysical Institute, University of Alaska
OSTI ID:
5667779
Journal Information:
J. Geophys. Res.; (United States), Vol. 88:A9
Country of Publication:
United States
Language:
English