D. Kraussvarban et N. Omidi, PROPAGATION CHARACTERISTICS OF WAVES UPSTREAM AND DOWNSTREAM OF QUASI-PARALLEL SHOCKS, Geophysical research letters, 20(11), 1993, pp. 1007-1010
The propagation characteristics of waves upstream and downstream of qu
asi-parallel shocks are investigated by using two-dimensional hybrid s
imulations. At low Alfven Mach numbers M(A) less than or similar to 2,
the shock is initially associated with upstream phase-standing whistl
ers. At later times, backstreaming ions excite longer-wavelength whist
lers via the right-hand resonant ion/ion instability. As anticipated f
rom linear theory, these waves are found to propagate along the magnet
ic field. Their group velocity is larger than or comparable to the ups
tream flow speed, and as a result, the waves remain in the upstream re
gion. At higher M(A) greater than or similar to 3 these waves are conv
ected back into the shock, causing its re-formation and downstream per
turbations. Shock transmitted waves mode-convert into Alfven/ion-cyclo
tron waves which have a wavevector along the shock normal (pointing up
stream) and convect downstream. The two-dimensional simulation results
confirm our earlier suggestion that the upstream waves should be fiel
d aligned, and that their convection into the downstream is associated
with linear mode conversion into the Alfven/ion-cyclotron branch.