S. Ghosh et al., THE EVOLUTION OF SLAB FLUCTUATIONS IN THE PRESENCE OF PRESSURE-BALANCED MAGNETIC-STRUCTURES AND VELOCITY SHEARS, J GEO R-S P, 103(A10), 1998, pp. 23691-23704
The traditional view that solar wind fluctuations are well-described a
s a spectrum of parallel-propagating Alfven waves has been challenged
many times but is still a frequently encountered perspective. Here we
examine whether it remains consistent to view most of the fluctuation
energy as resident in parallel-propagating Alfven waves in situations
in which there are also present either transverse pressure-balanced (P
B) magnetic structures or transverse velocity shears. We address these
questions through direct simulation of compressible magnetohydrodynam
ics, with expansion effects neglected. We show that parallel-propagati
ng Alfven waves are redirected to large oblique angles after refractiv
e interactions with PB structures or advective interactions with veloc
ity shears, reflecting the nonequilibrium nature of the initial spectr
al distribution. The timescale for these processes ranges from 2-8 edd
y-turnover times or characteristic nonlinear times. Relatively small a
mounts of PB structure and/or shear energy can redirect initially para
llel-propagating Alfven waves to highly oblique angles. Velocity micro
streams appear to be particularly efficient at creating highly oblique
waves. Even though the excited wave vectors are eventually primarily
oblique, the magnetic variance ratios show a minimum variance in the m
ean magnetic field direction.