SAIt 2011 c
MemoriedellaThe streaming instability: a review
Elena Amato
Istituto Nazionale di Astrofisica – Osservatorio Astrofisico di Arcetri, Largo E. Fermi 5, I-50125 Firenze, Italy, e-mail: amato@arcetri.astro.it
Abstract.
Streaming instabilities are thought to play a fundamental role in both acceleration and propagation of Cosmic Rays (CR) in the Galaxy. While work on this subject dates back to the ’70s, important progress has been made in recent years with the discovery of a non- resonant mode of the instability that may provide the large levels of turbulence required to account for particle acceleration up to the highest energies observed in Galactic CRs.
I will give a brief overview of our understanding of streaming instabilities and their role in Cosmic Ray physics, following the historical development of studies in this field, from the pioneering works by Skilling and Wentzel in the ’70s to the most recent works, both theoretical and numerical, on the non-resonant modes.
Key words.
Instabilities – Magnetic Fields – Shock Waves – Acceleration of Particles
1. Introduction
Historically, the interest of the CR physics community for streaming instability was moti- vated by the problem of explaining CR prop- agation through the Galaxy. Observations of CRs show that these particles are confined in the Galaxy for a time T
conf∼ 2 × 10
7E
GeV−αyr, with α ∼ 0.3 − 0.6 and E
GeVthe particle en- ergy in GeV. Most intriguing, an extremely low level of anisotropy is found, δ ∼ 1.5 × 10
−4, implying that these particles drift at a velocity v
D∼ cδ ∼ 50km/s. This speed is comparable with the Alfv´en velocity in the ionized ISM, v
A, leading to suggest, already in the ’70s (see Wentzel (1974) for a review), that isotropiza- tion could be provided by wave-particle inter- actions. The streaming of CRs along magnetic field lines at super-alfv´enic speeds generates magnetic turbulence at a wavelength corre- sponding to the particles’ gyroradius (Skilling
Send offprint requests to: E. Amato
1975): such turbulence could then provide ef- ficient scattering of the same particles so as to ensure a small diffusion coefficient and hence small anisotropy and large confinement times in the Galaxy.
Particle streaming is even more important
in the acceleration region. CRs up to the so
called ”knee”, namely up to the energy E
knee∼
3×10
15eV where the CR spectrum is observed
to steepen, are believed to be of Galactic ori-
gin, and Supernova Remnant (SNR) shocks are
the best candidate sources based on energetic
arguments. The best candidate mechanism is
the 1
storder Fermi process or Diffusive Shock
Acceleration (DSA), with an acceleration rate
that scales with the inverse of the diffusion co-
efficient in the surroundings of the shock: given
the finite lifetime of a SNR shock, reaching
E
kneerequires very effective particle scattering,
leading to infer a turbulent magnetic field in
the shock region much in excess of the average
field in the ISM. Such field amplification, of
which we recently acquired observational evi- dence (Bykov et al. 2011), is thought to be pro- vided by CRs streaming ahead of the shock.
In recent times, the streaming instability has been reconsidered to show that in addi- tion to the well known and long studied res- onant (res) mode, there is also a non-resonant (nr) mode in the dispersion relation, that might show in some situations very large growth rates, much larger than for the res one (Bell 2004, B04 hereafter). These nr waves lead to magnetic field strengths that could ensure, in principle, acceleration of particles up to the knee. The problem with these modes, in terms of their efficacy for particle diffusion (and hence acceleration), is that they are born as short wavelength modes and some inverse cas- cading is necessary before they can provide ef- fective particle scattering.
The latter issue can only be addressed by means of numerical studies of the instability, aimed at clarifying its saturation both in terms of strength and dominant wavelength.
2. Wave-particle interaction
Let us consider the interaction between a par- ticle propagating in a magnetic field B
0and an Alfv´en wave of wavelength λ. Alfv´en waves are perpendicular, low frequency waves, with dispersion relation ω = kv
Awhere k = 2π/λ and v
A= B
0/ √
4 π n
im
i(m
iand n
iare the mass and number density of the back- ground ions). When a particle of momentum p and charge e interacts with such a wave, the Lorentz force acting on the particle leads to a change in particle parallel momentum:
∆p
k= e Z
τ0
dt v ∧ B c
!
k
∝ Z
τ0
dt (A
++ A
−) (1) where A
±= cos
kv
k− ω ± Ω t + Φ
±, with Φ
±taking into account the relative phase be- tween particle and wave, Ω = EB
0/p is the relativistic particle cyclotron frequency and the subscripts k and ⊥ are with respect to the di- rection of B
0. For positive (negative) values of v
k, the integrand in Eq. 1 includes a high fre- quency term, A
+(A
−) that averages out over the duration of the interaction τ = 2π/(kv
k−ω),
and a low frequency term, A
−(A
+) that is max- imum when the resonance condition, kv
k≈ Ω, is satisfied. When this happens, Eq. 1 gives
∆p
k= πp
⊥(δB/B
0) cos Φ (2) which can be rewritten in terms of the par- ticle pitch angle θ (angle between the parti- cle propagation direction and B
0) as ∆θ =
−π(δB/B
0) cos Φ. If we then consider the ef- fect of interactions over a time t much larger than τ, we can define the pitch angle diffusion coefficient:
D
θθ= h(∆θ)
2i
t = π
8 Ω δB B
0!
2, (3)
and the associated spatial diffusion coefficient D(p) = c
26D
θθ= 4 3π
B
0δB
2cr
L(4)
where r
Lis the particle Larmor radius and v ∼ c has been assumed. Isotropy in the wave frame is reached in a time T
iso∼ D
−1θθ. Therefore the condition that CRs are isotropized in a time T
isoT
confrequires (δB/B
0) 10
−10E
GeV(1+α)/2at λ ∼ 10
12E
GeVcm.
The most natural way to have turbulence at the right scales is by having CRs injecting it.
The growth-rate of CR injected turbulence, γ
w, can be computed following a very simple rea- soning that provides a surprisingly accurate an- swer (see Kulsrud 2004). Let us consider mo- noenergetic CRs interacting with seed Alfv´en waves. Initially, the resonant particle momen- tum density is P
CR= n
∗CRm
iγ
CRv
D, with n
∗CR= n
CR(p > eB
0/ck), where k is the wavenumber.
After a time τ ≈ D
−1θθ: P
CR= n
∗CRm
iγ
CRv
A, and hence dP
CR/dt = (n
∗CRm
iγ
CR(v
D− v
A))/τ. This must correspond to the momentum density gained by the waves, which is readily written in terms of γ
was dP
w/dt = (1/v
A)(dE
w/dt) = (γ
w/v
A)(δB
2/8π), where v
A= ω/k relates the wave momentum and energy density, P
wand E
w. By equating dP
w/dt and dP
CR/dt, and us- ing the expression for D
θθin Eq. 3, we obtain γ
w≈ π
4 n
∗CRn
iΩ
0v
D− v
Av
A, (5)
with Ω
0= eB
0/(m
ic) the non-relativistic cy-
clotron frequency. Eq. 5 implies that super
-alfv´enic streaming of particles makes seed Alfv´en waves unstable.
While the expression of γ
win Eq. 5 is an excellent approximation for the growth rate of the res mode of the streaming instability, the nr mode can only be found through the stan- dard formal theory, which consists of the fol- lowing steps: take the unperturbed distribution functions of CRs and background plasma; as- sume that a small amplitude Alfv´en wave per- turbs them and find the perturbed distributions;
compute the resulting currents; use these in Maxwell’s equations to derive the linear evo- lution of waves with time. All of this trans- lates into writing a dispersion relation, that for circularly polarized Alfv´en waves reads:
h c
2k
2/ω
2− 1 − P
s
χ
si
= 0, where the sum is over all the species s and χ
sis the correspond- ing response. We will write all equations in the frame in which CRs are isotropic.
When the nr mode of the CR streaming in- stability was first highlighted by B04, a much debated topic was the form of the return plasma current J
retcompensating the CR current: one may assume that the charge non-neutrality in- duced by the streaming CRs is compensated by an equal number of negative charges that are cold and isotropic in the same reference frame (Zweibel 2003); or that a charge imbalance re- mains in the background plasma and translates into a different drift velocity between the ions and the electrons (Achterberg 1983). In the first scenario ions and electrons in the back- ground plasma have equal density and drift at v
D; while in the second: n
e= n
i+ n
CR, v
i= v
Dand v
e= (n
i/n
e)v
Din order to ensure charge and current neutrality. It is possible to show (Amato & Blasi 2009, AB09 hereafter) that both assumptions lead to the same dispersion relation to order O h
(n
CR/n
i)
2i .
The background plasma response is most easily computed in cold plasma theory, and one obtains (AB09) :
χ
p= − 4πe
2ω
2n
im
i"
ω + kv
Dω + kv
D± Ω
0i+ m
im
eω + kv
Dω + kv
D± Ω
0e+ n
CRn
im
im
eω ω ± Ω
0e# (6)
For the isotropic CRs (Krall & Trivelpiece 1973):
χ
CR= 4π
2e
2ω
Z
∞0
dpp
2v ∂ f
CR∂p Z
+1−1
dµ (1 − µ
2) ω − kvµ ± Ω
iwhere µ is the pitch angle cosine, f
CR(p) =
nCR
2
g(p) and g(p) is a power-law, normalized so that R
pmaxp0
dp p
2g(p) = 1. The integral in µ reduces to
−iπ Z
1−1
dµ(1 − µ
2)δ(−kvµ ± Ω
i)
+P Z
1−1
dµ (1 − µ
2)
−kvµ ± Ω
i. (7)
The first term in Eq. 7 is the classical resonant part:
since |µ| ≤ 1, this is non-zero only if Ω/kv ≤ 1, or p ≥ p
1= eB
0/ck. The second term is the nr contri- bution. In the end one can write:
χ
CR= c
2v
2AΩ
0ω n
CRn
i(iI
res∓ I
nr) (8)
I
res(k) = π 2
Z
∞p1
dppp
1g(p) I
nr(k) = − p
312 Z
∞ρmin