If
and
,
the flow around the
shock is entirely super-Alfvénic. Then all upstream Alfvén waves are convected
through the shock to become downstream Alfvén waves. Some waves are transmitted
retaining their propagation direction relative to the flow, but others get
reflected, i.e., assume the other propagation direction. Alfvén-wave
transmission through a parallel shock wave can be calculated by taking the
tangential magnetic-field and velocity components to be due to waves,
and
.
We shall first
investigate the transmission coefficients in a shock with a pre-described gas
compression ratio. Thus, by using the first four jump conditions,
Eqs. (8-9), together with
Eqs. (15-16) and assuming a
degenerate upstream cross helicity,
,
we find after an amount of straight-forward algebra
Let us, next, calculate the gas compression ratio for a shock propagating with
Mach number M into a gas with parallel plasma beta,
and firehose factor
One should also check for the physicality of the obtained shock solutions. We
will not analyze this in detail, but note only that if the analysis of the
entropy change across the shock is based on ideal gas law, we can write (Lyu &
Kan 1986)
The easiest way to analyze the compression ratio as a function of Mach number is
to solve for b or
in
Eqs. (22-23), regard it
as a function of two variables (r and M), and to contour plot it fixing
the values of other parameters. Thus, e.g.,
The Alfvén-wave transmission coefficients for the shocks in
Fig. 1 are given in
Fig. 2. We choose outwards-propagating (h=-1) upstream waves consistent with their generation by counter-streaming
particles. For the colder upstream gas, the transmission coefficients are
affected only a little by the pressure anisotropy, but for the hotter case we
see substantial effects; especially the reflection coefficient is substantially
increased in presence of anisotropies. Generally, T>R, for h=-1, but for
a marginally firehose-stable upstream plasma (
), the downstream
state tends to an equipartition between forward and backward propagating Alfvén
waves (
)
as
.
The most important parameter controlling the energy spectrum of cosmic rays
accelerated by a shock wave is the compression ratio of the scattering centers
that are responsible for the isotropization of the energetic particles. In case
of Alfvén waves generated in the upstream region, we may write
The results for the scattering-center compression ratio were also calculated for
the interesting case of
at several values of the
firehose factor (Fig. 4) to see, how large
anisotropies are needed for qualitative effects on particle acceleration from
pressure anisotropies. It is evident that relatively small values, below
,
are needed to produce large effects on particle
acceleration. But, for
the scattering-center compression
ratio is above 4 for all 1<r<4.
Perhaps the most unexpected result of our calculation is the ability of weakly
compressive (
)
shocks to accelerate particles efficiently in warm
plasmas. This result, however, depends crucially on the assumption of the shocks
ability to isotropize the fluid. If r differs considerably from unity, one can
probably safely assume that the small-wavelength magnetic turbulence generated
in the shock transition can be responsible for the isotropization. On the other
hand, the transverse magnetic field attains large values across the
shocks with
regardless of the compression
ratio. This can also add to the isotropization of the particles since the field
changes direction across the shock at scales comparable to the ion Larmor
radius. However, the shocks with small r do not contain large amounts of
energy to be given for accelerated particles. When at the same time the
test-particle spectral index is below 2, the pressure in accelerated particles
diverges without a cutoff in the spectrum. The less there is energy available,
the smaller value for the cutoff-momentum must be, and it may well turn out that
the weak shocks can not be described by the test-particle picture at all. The
confirmation of this requires non-linear analysis, which we shall undertake in
the future.
We will briefly discuss the pressure anisotropies created by the shock-related
non-thermal particles assuming non-relativistic particle speeds for
simplicity. For particles accelerated at the shock to speeds clearly exceeding
the shock-frame scattering-center speed, V1, particle scattering results in a
distribution function,
,
that is only weakly dependent on the pitch-angle,
.
In the upstream wave frame, the small anisotropic portion of the
distribution,
where
denotes angle averaging, is antisymmetric relative
to
if the net magnetic helicity of the waves is zero (e.g., Schlickeiser
1989), which we assume. Thus, the pressures due to these particles are
![]() |
![]() |
![]() |
(29) |
![]() |
![]() |
![]() |
(30) |
![]() |
(31) |
Another contribution to the pressure anisotropy comes from the particles that
have just been reflected by the shock and subsequently been picked up by the
upstream waves. Let us, for simplicity, consider a cold background plasma, and
assume that the shock reflects a small fraction of the incoming
background-plasma ions back to the upstream region. We model those particles as
a beam with a density of
propagating along the
magnetic field away from the shock and include also the particles that return to
the shock after their isotropization by the upstream waves. Specifically, in the
upstream wave frame we take the distribution function for the reflected and
returning particles to be
![]() |
(32) |
![]() |
(33) |
Copyright ESO 2001