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P. Malovichko, Y. Voitenko, J. De Keyser, Compensated-current instability of kinetic Alfvén waves, Monthly Notices of the Royal Astronomical Society, Volume 452, Issue 4, 01 October 2015, Pages 4236–4246, https://doi.org/10.1093/mnras/stv1533
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Abstract
We study a non-resonant instability of kinetic Alfvén waves (KAWs) driven by compensated currents. Such currents set up in response to energetic ion beams occurring in many space and astrophysical plasmas, like foreshock regions in the solar wind and around supernova remnants. Kinetic effects of the background ion gyroradius make the KAW instability stronger than its magnetohydrodynamic (MHD) counterpart and shift its maximum to shorter wavelengths. The KAW growth time can be very short, approaching the proton gyroperiod in the terrestrial foreshock ahead of the quasi-perpendicular bow shock region. The oblique Alfvén instability driven by the cosmic rays in the interstellar and intergalactic plasmas develops mostly in the MHD regime and can extend in the KAW regime only at large fluxes of cosmic rays. Short cross-field wavelengths of growing Alfvén modes facilitate stochastic cross-field acceleration of cosmic rays.
INTRODUCTION
Compensated-current systems are often created in space and astrophysical plasmas by energetic ion beams. In particular, high-energy ion beams accelerated by shocks set up compensating (return) currents upstream of the terrestrial bow shock (Paschmann et al. 1981, and references therein), around supernova remnants (Bell 2005, and references therein), and in many other astrophysical environments (Zweibel & Everett 2010, and references therein). Helium ions streaming with respect to the protons in the solar wind (Marsch 2006, and references therein) also set up a kind of compensated-current system.
Several plasma eigenmodes can be driven unstable in such systems, directly by the ion beams (Sentman, Edmiston & Frank 1981; Winske & Leroy 1984; Gary 1985), and also by the neutralizing return currents set up in response to the beam currents (Winske & Leroy 1984; Bell 2004; Buchner & Elkina 2006; Chen & Wu 2012, and references therein). The wave generation involves both the resonant (Duijveman, Hoyng & Ionson 1981; Gary 1985; Buchner & Elkina 2006) and non-resonant (Winske & Leroy 1984; Bell 2004; Achterberg 2013) wave–particle interactions. Kinetic resonant instabilities of Alfvén, fast and slow modes, driven by the ion beams, have been studied extensively. Among them, the parallel-propagating Alfvén and fast modes (Gary 1985) appeared to be most unstable at beam velocities larger than several Alfvén velocities. At lower, slightly super-Alfvénic beam velocities, oblique Alfvén instabilities become stronger (Voitenko 1998; Daughton, Gary & Winske 1999; Gary et al. 2000; Voitenko & Goossens 2003). The ion-acoustic mode can be destabilized as well (Gary 1985) but is of minor importance.
In the context of high-energy streaming cosmic rays (CRs), the Bell instability (Bell 2004), its modifications and alternatives attracted recently a lot of interest (see e.g. Amato & Blasi 2009; Bret 2009; Zweibel & Everett 2010; Schure et al. 2012; Achterberg 2013, and references therein). Starting from Bell (2004), the primary focus of this research was on the magnetic field-aligned modes and on destabilizing effects produced by the parallel wave dispersion. These limitations were discussed and relaxed in our previous paper (Malovichko, Voitenko & De Keyser 2014, Paper I hereafter) where we found a new Alfvénic instability at oblique propagation driven by compensated currents. It is essential for this instability that its wavelength perpendicular to the background magnetic field |$\boldsymbol {B}_{0}$| is comparable to the beam gyroradius, which makes the beam kinetic effects important.
On the other hand, kinetic effects of the finite background ion gyroradius were neglected in Paper I, which may be justified only if the perpendicular wavelengths of unstable fluctuations are much longer than the background ion gyroradius. Consequently, the unstable fluctuations studied in Paper I were in fact oblique magnetohydrodynamic Alfvén waves (MHD AWs) modified only by the beam-driven compensated currents. However, the background plasma is in many cases not so cold (or the unstable wavelengths are not so large), in which cases kinetic effects of finite background ion gyroradius must be taken into account in oblique Alfvén waves. This is done in this paper, where we relax the limitation of the cold background and study a compensated-current instability of kinetic Alfvén waves (KAWs) – oblique Alfvén mode modified by kinetic effects of the thermal ion gyroradius.
KAWs have been extensively studied in view of their ability to interact with particles kinetically via Cherenkov (Voitenko 1995, 1998) and ion–cyclotron (Winske & Leroy 1984; Daughton et al. 1999; Voitenko & Goossens 2003; Verscharen & Chandran 2013) resonances. These resonant interactions provide generation and dissipation mechanisms for KAWs and make them important mediators for energy transport and release in many laboratory and space plasmas. Non-resonant aperiodic KAW instability can be driven by (non-compensated) electric currents flowing across |$\boldsymbol {B}_{0} $| (Siversky, Voitenko & Goossens 2006) and along |$\boldsymbol {B}_{0}$| (Malovichko & Iukhimuk 1992; Malovichko 2007), and by neutral plasma flows along |$\boldsymbol {B}_{0}$| with velocity shears (Siversky, Voitenko & Goossens 2005). Our present study shows that the KAW branch can be made unstable non-resonantly in the compensated-current systems.
MODEL
SOLUTION FOR KINETIC ALFVéN MODE
Equation (8) contains KAW mode (first parentheses in the left-hand side) and fast mode (second parentheses), coupled by the kinetic effects in the beam (right-hand side). If there is no beam, |$\bar{j}_{\rm b}=0$|, or the beam gyroradius is negligible, |$\mu _{\rm b}^{2}=0$|, then the coupling term in equation (8) vanishes and we recover the decoupled KAW, ω = ωA, and fast mode, ω = ωF. In the MHD limit for the background ions (|$\mu _{\rm i}^{2}\rightarrow 0$|), but with still kinetic beam ions (|$\mu _{\rm b}^{2}\ne 0$|), we have KF = KA = 1 and equation (8) reduces to the dispersion equation derived by Malovichko et al. (2014).
INSTABILITY ANALYSIS
Threshold
At the same time, as we will see later, the effects of finite μi modify significantly the instability growth rate and the position of its maximum in the unstable range.
Wavenumber dependence of the instability growth rate
The growth rate (14) dependent on the parallel and perpendicular wavenumbers is shown in Fig. 1, where the beam and plasma parameters are chosen to be compatible with those in the quasi-perpendicular foreshock region: Tb/Ti ≃ 25, |$V_{\rm A}^{2}/V_{Ti}^{2}\simeq 1$|, |$\bar{j} _{\rm b}\simeq 1.5$|. To allow the comparison with the previous results, we also plot the growth rate (15) for MHD Alfvén waves. The solid contours with shadowing show the growth rate (14) accounting for the finite background ion gyroradius, whereas the dashed contours are used to show equation (15) describing MHD AWs.

Contour plot of the KAW growth rate in the (kz, k⊥) plane (solid lines and shading). The parallel (kz) and perpendicular (k⊥) wavenumbers are normalized by the ion inertial length and the beam ion gyroradius: |$\mu _{\rm i}=k_{\perp } \rho _{\rm i}$| and |$ \nu _{\rm i}=k_{z} \delta _{\rm i}$|. The normalized beam current |$\bar{j}_{\rm b}=1.5$| and the beam temperature Tb = 25Ti. The growth rate of the MHD AW instability is shown for comparison by dashed lines. The corresponding maximal growth rates are indicated by small circles (solid line for KAWs and dash line for MHD AWs).
Surprisingly, corrections introduced by the effects of finite background ion gyroradius become significant at still very low background ion temperature as compared to the beam ion temperature, Ti/Tb ∼ 0.04, which implies a relatively small dispersive parameter |$\mu _{\rm i}^{2}\approx 0.04\mu _{\rm b}^{2}$| that describes the finite-μi effects. It appears that, in general, the impact of the finite background ion gyroradius is twofold: (i) to increase the growth rate at all wavenumbers (this follows from the fact that all solid contours in Fig. 1 encircle corresponding dash contours), and (ii) to shift the growth rate towards higher perpendicular wavenumbers μi (solid contours are shifted to higher μi). Note that the solid contour γ/ωBi = 0.7 does not have its dashed counterpart, which means that γ is significantly larger than γMHD. With the mentioned above values of the plasma parameters the finite-μi effects roughly double the wavenumber at maximum and make the corresponding growth rate about 10 per cent larger. The KAW growth rate has a maximum γm ≃ 0.76 attained at μim ≃ 0.6 and νim ≃ 0.7, indicated in the figure by the small circle. For comparison, the ‘MHD approximation’ μi = 0 for the background ions would give a lower maximum γm(MHD) ≃ 0.68 at the smaller perpendicular wavenumber μim(MHD) ≃ 0.37 and about the same parallel wavenumber νim(MHD) ≃ 0.7 (see the small dashed circle in Fig. 1). On the other hand, as we already mentioned in the previous section, the range of unstable wavenumbers does not change.
In Fig. 1 (and in several other figures below), the instability growth rate near maximum is not much smaller than the ion gyrofrequency. Such large growth rates result from the large values chosen for the beam current to emphasize that the increment can be large, approaching to the gyrofrequency. The next-order terms |$\sim \gamma ^{4}/\omega _{Bi}^{4}$| may come into play and reduce γ2, but not as much as to remove the instability. That the instability does not vanish is insured by the extended unstable wavenumber range surrounding the maximum, in which the condition |$\gamma ^{2}/\omega _{Bi}^{2}\ll 1$| is satisfied (see e.g. outer contours in Fig. 1).
As in Paper I, we can find the maximum of equation (14) with respect to the parallel wavenumber |$\gamma _{\mu }\left( \mu _{\rm b}\right) =\max _{\nu _{\rm i}}$| γ(μb, νi). This procedure is straightforward but in the case of finite μi the resulting analytical expression becomes quite cumbersome and will not be written down explicitly. For the reference, the graphical representation of this maximum as function of μi is shown in Fig. 2 together with the same maximum but neglecting kinetic background effects of finite μi. The beam temperature and current are the same as in Fig. 1, Tb/Ti = 25 and |$\bar{j}_{\rm b}=1.5$|. This plot provides a straightforward comparison and evidence for the strong influence of the background kinetic effects on the growth rate: the growth rate increases and the maximum shifts to higher μi. At low values of μi, in the region of increasing growth rate in Fig. 2, the growth rates with and without effects of background ion gyroradius are almost the same, γ ≈ γMHD. But when approaching the growth rate maximum the difference becomes significant and increases further at larger μi, up to about factor 2. Again, the KAW growth rate is about two times larger than the MHD one at μi > 1.2, where condition |$\gamma ^{2}/\omega _{Bi}^{2}\ll 1$| is well satisfied.

The growth rate |$ \gamma _{ \mu }/ \omega _{Bi}$| for KAWs (solid line) and for MHD AWs (dashed line) as function of the normalized perpendicular wavenumber |$ \mu _{\rm i}=k_{\perp } \rho _{\rm i}$| for the beam/background temperature ratio Tb/Ti = 50 and the beam current |$\bar{j}_{\rm b}=1.5$|.
Properties of the compensated-current KAW instability
Let us turn to the instability growth rate, which can be found as the absolute maximum of the wavenumber-dependent growth rate, |$\gamma _{\mathrm{m }}=\max _{\mu _{\rm b}}\gamma _{\mu }\left( \mu _{\rm b}\right)$|. This maximum of γμ(μb) is attained at certain perpendicular wavenumber μb = μbm (the corresponding parallel wavenumber νi = νim is already fixed in γμ(μb)). For the plasma parameters used in Figs 1 and 2, this maximum γm ≃ 0.76 is attained at μim ≃ 0.6 (νim ≃ 0.7.
Now we can vary plasma parameters and investigate how the growth rate γm varies in response. The contour plot Fig. 3 shows how the instability growth rate γm depends on the most critical beam parameters, the normalized beam current |$\bar{j}_{\rm b}$| and the beam/ion temperature ratio Tb/Ti. In general, similarly to the instability of MHD AWs (Malovichko et al. 2014), the KAW growth rate increases with increasing |$\bar{j}_{\rm b}$| and Tb. However, the finite-μi effects make this increase faster, and larger values of the instability growth rate γm are attained at every particular |$\bar{j}_{\rm b}$| and Tb/Ti. It is seen that the difference between γm and γm(MHD) is small near the threshold values of |$\bar{j}_{\rm b}$| and VTb/VA defined by equation (13), but becomes significant when |$\bar{j}_{\rm b}$| and/or VTb/VA depart from the threshold. Consequently, the finite-μi effects become much stronger for the well over-threshold beam currents.

Contour plot of the maximum KAW growth rate |$ \gamma _{ \mathrm{m}}/ \omega _{Bi}$| (solid lines and shading) as function of the normalized beam current |$\bar{j}_{\rm b}$| and the beam/background temperature ratio Tb/Ti. The maximum growth rate |$ \gamma _{ \mathrm{m}}^{\left( {\rm MHD}\right) }$|, based on the non-kinetic treatment of the background ions, is shown for comparison by dash lines.

The wavevector tilt angle |$ \phi _{\mathrm{m}}$| (values are in degrees) as function of the normalized current |$\bar{j}_{\rm b}$| for the beam/background temperature ratios Tb/Ti = 50, 250 and 750 (solid and dashed lines from top to bottom). More oblique waves are generated in the hotter backgrounds and/or cooler beams.
The effects introduced by the finite gyroradius of the background ions make the anisotropy more pronounced (solid lines) than it would be in the case of MHD AWs (dashed lines). Together with the fact that the finite-μi effects shift the maximum towards larger perpendicular wavenumbers, this confirms that the unstable Alfvénic mode is in fact the KAW mode in a wide range of beam and plasma parameters.
The ratio |$\mu _{\rm i}^{2}/\mu _{\rm b}^{2}$| can be used to estimate the relative importance of the finite-μi effects. In the cases where the beam and background ions are of the same type (in this paper protons), |$\mu _{\rm i}^{2}/\mu _{\rm b}^{2}=T_{\rm i}/T_{\rm b}$|. Say, for Ti/Tb = 0.3, the tilt angle ϕm ≃ 52° in the case |$\bar{j}_{\rm b}=0.3$| and VTb/VA = 20, which is significantly larger than the corresponding tilt angle of MHD AW instability, ϕm ≃ 32°. From Fig. 4 we see that, in general, more oblique fluctuations are generated by the KAW instability. In the near-threshold regime, where the generated perturbations are very oblique in both the MHD and kinetic AW cases, 45° < ϕm < 90°, the tilt angle is not much affected by the μi effects. On the contrary, with growing |$\bar{j} _{\rm b}$| and/or Tb/Ti in the well over-threshold regime, where the MHD AW tilt angle becomes very small, the KAW tilt angle remains relatively large, ϕm ≳ 50°.
OBLIQUE ALFVéN INSTABILITY IN COMPENSATED-CURRENT SYSTEMS
Terrestrial foreshock regions
There are three types of proton beams in the terrestrial foreshock regions (Paschmann et al. 1981; Tsurutani & Rodriguez 1981): (i) beams created by ‘reflected’ protons associated with the quasi-perpendicular shocks; (ii) beams created by ‘diffusive’ protons associated with the quasi-parallel shocks; (iii) ‘intermediate’ beams associated with the oblique shocks. For the fast ‘reflected’ beams we will use the characteristic temperature Tb/Ti = 50 and velocity Vb/VA = 20, for the diffusive beams Tb/Ti = 750 and Vb/VA = 5, and for the intermediate beams Tb/Ti = 250 and Vb/VA = 10. The beam number densities are similar in all three cases and vary in the range nb/n0 = 0.01–0.1. To make the comparison straightforward, we assume nb/n0 = 0.04 in all three cases. Recent observations of the foreshock waves (Narita et al. 2006; Hobara et al. 2007) and their possible relations with the compensated-current instability of MHD AWs were discussed in the previous paper (Paper I). Here we focus on the new effects introduced in the Alfvénic instability by the effects of finite gyroradius for the background ions, which make the instability essentially the KAW instability.
The KAW growth rate in the quasi-perpendicular, intermediate and quasi-parallel foreshock regions is shown in Fig. 5 as function of the normalized perpendicular wavenumber μi. The instability tends to be strongest in the quasi-perpendicular foreshock region, where kinetic effects of background ion gyroradius are most pronounced. The largest perpendicular wavenumbers μi are generated in this region, which emphasizes the importance of the background kinetic effects and hence KAWs there. Intermediate and diffusive beams generate Alfvén waves with significantly smaller perpendicular wavenumbers, which can be well described by the MHD approximation for the background ions, μi = 0.

The instability growth rate as function of the perpendicular wavenumber in the plasma conditions typical for the quasi-perpendicular foreshock (beam currents |$\bar{j}_{\rm b}=1.5$| and beam temperature Tb = 50Ti, solid line), intermediate foreshock (|$\bar{j}_{\rm b}=0.7$| and Tb = 250Ti, dashed line) and quasi-parallel foreshock (|$\bar{j} _{\rm b}=0.3$| and Tb = 750Ti). The finite-|$ \mu _{\rm i}$| effects are most pronounced in the quasi-perpendicular foreshocks.
In comparison to our previous results on the MHD AW instability (Paper I), we see that the effects of background μi make the ion beams more unstable in the quasi-perpendicular foreshocks. This fact supports the ‘evolutionary model’ of the foreshock ion beams, in which the quasi-perpendicular foreshock beams are relaxed by some instability and then convected by the solar wind and contribute to the beams in intermediate and quasi-parallel foreshocks. The waves generated in the quasi-perpendicular foreshocks follow the same evolution: they are also convected by the solar wind and contribute to the oblique wave spectra observed in the intermediate and quasi-parallel foreshocks.
The bimodal wavenumber distribution has been reported for the waves observed upstream of the bow shock (see fig. 9 by Narita et al. 2006). In terms of the thermal ion gyroradius scale, the waves observed in the quasi-perpendicular foreshock are grouped around two peaks at μi1 ≃ 0.06 and μi2 ≃ 0.4. As is seen from Fig. 5, the dominant group of the waves around μi2 ≃ 0.4 can be easily generated by the compensated-current KAW instability studied here. On the other hand, the sub-dominant group around μi1 ≃ 0.06 do not require the kinetic treatment for background ions and can be generated by the MHD AW instability (Paper I). Then the reason for this bimodal wave distribution can be bimodal distributions of the beam currents and/or ion temperatures because of the different conditions in the slow versus fast solar winds. The quasi-perpendicular foreshock waves are relatively more oblique than the waves in the quasi-parallel foreshock, which can be explained by the KAW nature of the instability in the quasi-perpendicular foreshocks (see Fig. 4).
Cosmic rays
Since cosmic rays (CRs) are much more energetic than the terrestrial foreshock ions, the ratio of their gyroradius ρCR ∼ c/γrωBi to the thermal ion gyroradius ρi is much higher in most astrophysical environments. We consider here three examples: (i) CRs in the relatively cool interstellar medium around supernova remnants (background ion temperature Ti ∼ 104 K, magnetic field B0 ∼ 10−5 G and number density ni ∼ 1 cm−3), (ii) in the hotter superbubbles (Ti ∼ 106 K, B0 ∼ 5 × 10−6 G and ni ∼ 10−2 cm−3); and (iii) in the hot background plasma of the galaxy clusters (Ti ∼ 107 K, B0 ∼ 10−6 G and ni ∼ 10−3 cm−3) (see e.g. Zweibel & Everett 2010, and references therein). The CR/background ion gyroradius ratios are ρCR/ρi ≃ 3 × 104, 3 × 103, and 103 for three above cases, respectively.
In Fig. 6, we present the k⊥-dependence of the growth rate of the instability driven by the well over-threshold CR current |$\bar{j}_{\rm b}=1.7$| around supernova remnants, in superbubbles, and in the intercluster medium. It appears that the instability with shortest perpendicular wavelengths λ⊥ = 2πρCR/2.2 × 10− 4 ≃ 1.7 × 108 cm is generated around the supernova remnants and with longest, λ⊥ = 2πρCR/2.2 × 10− 4 ≃ in the intercluster plasma. On the other hand, the normalized growth rate at maximum is the same in all three cases, γm/ωBi ≃ 0.9, and this maximum is achieved at the same perpendicular wavenumber normalized by the background ion gyroradius, k⊥ρi ≃ 0.75. These properties indicate that the most unstable perturbations have the characteristic length-scales close to ρi and are therefore controlled by effects of the thermal ion gyroradius rather than the CR gyroradius. Consequently, the KAW mode is generated by such strong CR currents.

The growth rate of the KAW instability driven by the strong flux of CRs |$\bar{j}_{\rm b}=1.7$| around supernova remnants, in superbubbles and in intercluster medium. The background plasma conditions are: Ti ∼ 104 K, B0 ∼ 10−5 G and ni ∼ 1 cm−3 around supernova remnants; Ti ∼ 106 K, B0 ∼ 5 × 10−6 G and ni ∼ 10−2 cm−3 in superbubbles; and Ti ∼ 107 K, B0 ∼ 10−6 G and ni ∼ 10−3 cm−3 in intercluster medium.
On the contrary, the more realistic weaker CR currents |$\bar{j}_{\rm b}<1$| drive the instability with much longer perpendicular wavelengths controlled by the CR gyroradius rather than the thermal ion gyroradius. The MHD Alfvén instability is driven in such cases, for which the perpendicular wavenumbers are already essential to make kinetic effects of finite CR gyroradius possible, but the background response still remains MHD-like. Indeed, assuming the background magnetic field B0 ∼ 3 × 10−6 G and the CR flux nCRVb ∼ 104 cm−2 s−1 (Zweibel & Everett 2010), we estimate |$\bar{j}_{\rm b}=1.53\times 10^{-2}$| around supernova remnants, which gives rise to the oblique MHD Alfvén instability with the maximum growth rate γm/ωBi ≃ 0.007 65 attained at k⊥ρCR ≃ 8. Taking into account ωBi ≃ 0.03 s−1 and ρCR ≃ 3 × 1012 cm, we get γm ≃ 2.2 × 10−4 s−1 in absolute numbers.
Since |$\bar{j}_{\rm b}\gg \bar{j}_{\mathrm{thr}}\simeq 3\times 10^{-5}$|, we are in the asymptotic well over-threshold regime, where oblique and field-aligned (Bell) instabilities have the same growth rate γm ≃ 2.2 × 10−4 s−1 (compare with maximum in fig. 3 by Zweibel & Everett 2010). It means there are two unstable ranges in the wavenumber space, one at k⊥ρCR ≃ 8 (oblique instability) and another at k⊥ρCR ≃ 0 (Bell instability). In addition, the Bell instability requires that the background plasma and CRs are uniform in across |$\boldsymbol {B}_{0}$| (the non-uniformity scale |$L_{\perp }k_{\rm Bell}=0.5\delta _{\rm i}^{-1}\bar{j}_{\rm b}$|).
DISCUSSION
In the present study, we focused on the analytical investigation of the KAW instability. Several well-known instabilities, including Bell and Weibel, do not appear in our analysis because we used specific approximations designed to capture the oblique Alfvén instability. Detailed comparative study of the KAW instability with other instabilities in parameter space is subject for future studies. Here we shortly discuss the oblique Alfvén instability in comparison to extensively studied Bell instability, and some observational consequences of the former.
Oblique Alfvén instability versus Bell instability
Oblique AW instability is closest by nature to the extensively studied Bell instability. Both instabilities are made possible by demagnetization of one or several plasma components streaming along B0 (it is the ion beam in our case). Demagnetization here means that the response of some plasma component to the sufficiently small-scale fluctuations is reduced (and vice versa). The principal difference between two is in the physical mechanism thereby the beam/CR ions (or any other species streaming along B0) are demagnetized. In the oblique AW instability the beam ions are demagnetized not by the small parallel wavelength of perturbations 1/k∥ < VTb∥/ωBi (or 1/k∥ < Vb0∥/ωBi if the beam is cold) as in the Bell instability (Bell 2004; Achterberg 2013), but by the small perpendicular wavelengths 1/k⊥ < VTb⊥/ωBi (cf. Malovichko et al. 2014). That is why our instability is essentially oblique and maximizes at large perpendicular wavenumbers, whereas the Bell instability attains maximum at parallel propagation at large parallel wavenumbers. Consequently, the beam-ion gyroradius effects destabilize the essentially oblique (kinetic) Alfvén mode, whereas the quasi-parallel Alfvén mode is driven by the Bell mechanism.
Essentially the same effect, preferential ion demagnetization at short perpendicular wavelengths, makes Alfvén waves unstable in the neutral plasma flows with velocity shears (Siversky et al. 2005). As the demagnetization effects arise due to finite ion gyroradius (finite k⊥ρi), the velocity-shear-generated Alfvén waves are not MHD but kinetic (i.e. KAWs).
It is often stated that effects of large beam-ion gyroradius (as compared to the parallel wavelength) make the Bell instability possible, which is strictly speaking incorrect. The reference scale for the parallel wavelength is the parallel transit scale VTb∥/ωBi (or Vb0∥/ωBi if the beam is cold) rather than the (perpendicular) ion gyroradius VTb⊥/ωBi . Achterberg did took into account the ion gyroradius terms ∼k⊥V⊥/ωBi (up to the first order) but only for the background ions, not for the beam. In the Achterberg approximation the KAW mode exists but its compensated-current instability cannot be captured.
To illustrate further principal differences between two instabilities, let us consider a plasma model used by Bret (2009). This model comprises two electron components counter-streaming |$\parallel \boldsymbol {B}_{0}$| on the steady ion background. It is easy to see that our instability does not exist in this setting whereas the Bell instability exists. The reason is that both electron components remain equally magnetized at any cross-B0 scale of trial perturbations (hence our instability is absent), but the differential streaming of the electrons ∥B0 can lead to their different demagnetizations, and hence the Bell instability is possible.
Our growth rate in the supernova remnant (γm ≃ 2.2 × 10−4 s−1) is obtained for |$\bar{j}_{\mathrm{CR}}=1.53\times 10^{-2}$|, which is more than two orders larger than the instability threshold |$\bar{j}_{\mathrm{thr}}\approx 3\times 10^{-5}$|. In this well over-threshold regime our growth rate is the same as the Bell growth rate and both instabilities should develop. However, they develop in different wavenumber domains, which in certain circumstances (thermal anisotropies, plasma inhomogeneity, etc.) may affect their growth rates in different ways. For example, the background thermal effects at high temperatures reduce the Bell growth rate (e.g. Achterberg 2013, and references therein) but increase ours (the KAW effect).
Polarization of the kinetic Alfvén mode is variable and can be right- or left-handed elliptic depending on the wavenumber, propagation angle (with respect to |$\boldsymbol {B}_{0}$|), and plasma beta (Zhao et al. 2014). Adding also the beam and plasma currents makes this dependence even more complicated and requires further analysis in the parameter space, which will be subject for a separate study.
Some observational consequences
Observational consequences and effects produced by the oblique AW instability are quite different from those of the (parallel) Bell instability. The most straightforward is the different orientation of generated magnetic filaments. Namely, magnetic filaments oriented across the initial background magnetic field |$\boldsymbol {B}_{0}$| would indicate the Bell instability, whereas magnetic filaments elongated along |$\boldsymbol {B} _{0}$| are typical for the oblique Alfvén instability.
Cross-|$\boldsymbol {B}_{0}$| stochastic acceleration of CRs is another important effect that can be introduced by the oblique AW instability. This acceleration is made possible by small cross-|$\boldsymbol {B} _{0}$| scales of generated oblique AWs, comparable to (or sometimes even much smaller than) the CR gyroradius. Actually, oblique instability is naturally designed for stochastic CR acceleration because its perpendicular scale is linked to the CR gyroradius. The required (threshold) magnetic AW amplitudes and their consistency with the free energy available in the system will be analysed in future.
Electric field component |$\boldsymbol {E}_{z}\parallel \boldsymbol {B}_{0}$| arises in AWs at oblique propagation. Due to |$\boldsymbol {E}_{z}$|, oblique AWs undergo kinetic wave–particle interactions at Cherenkov resonances, which should lead to the plasma pre-heating in astrophysical foreshocks.
An admixture of the jitter-like radiation (due to the presence of small-scale AWs), in addition to the synchrotron (due to the presence of large-scale |$\boldsymbol {B}_{0}$|), can be produced in our setting and, if observed, used for diagnostic purposes. We are not aware of such observations.
CONCLUSIONS
Accounting for the perpendicular dispersive effects introduced by the finite ion gyroradii in the beam and in the background plasma, we investigated a non-resonant instability of kinetic-scale Alfvén waves (KAWs) in compensated-current systems. The instability emerges on the KAW dispersion branch due to the coupling with the fast mode via the current term proportional to |$\bar{j}_{\rm b}$|. Thus we extended the applicability limits of Paper I, where only for MHD Alfvén waves have been taken into account. The kinetic Alfvénic dispersion branch is made aperiodically unstable by the mismatch between the wave responses to the demagnetized ion beam current and the magnetized background electron current. We found that the effects of finite background ion gyroradius play a destabilizing role.
The main properties of the compensated-current KAW instability are summarized as follows.
The KAW instability is driven by the same effects as the MHD AW instability – perpendicular dispersive effects of finite beam gyroradius (terms ∼k⊥ρb). Effects of the finite background gyroradius (terms ∼k⊥ρi) enforce the instability (the KAW effect).
The threshold beam current is the same as for the oblique MHD AW instability, |$\bar{j}_{\mathrm{thr}}\simeq 1.33V_{\rm A}/V_{Tb}$|. The increasing beam current and temperature play a destabilizing role.
At well above-threshold currents the KAW effect increases the instability growth rate significantly, about two times in the vicinity of the upper boundary of the instability μi ≲ μi2. The most unstable perpendicular wavenumbers in this case tend to be controlled by ρi rather than ρb.
The KAW instability is more oblique than the MHD AW instability.
Short cross-field wavelengths of generated KAWs make them available for stochastic cross-field acceleration of the beam ions.
Fluctuations with varying obliquity, regularly observed in the terrestrial foreshock, can be explained in terms of the MHD AW instability in the case of less oblique propagation with small μi ≪ 1, and by the KAW instability in the cases of more oblique propagation with μi ∼ 1. The obliquity is difficult to explain by competing instabilities, left-/right-hand resonant (Gary 1985), fire-hose (Sentman et al. 1981), ‘antiparallel non-resonant’ (Winske & Leroy 1984), and ‘parallel non-resonant’ (Bell 2004, 2005), all of which are magnetic field-aligned. To this end we note that the oblique dispersion equation derived by Bell (2005) and discussed by Schure et al. (2012) is dominated by the parallel dispersive effects rather than the perpendicular ones and is maximized at parallel propagation. As we already discussed in Paper I, the previous studies did not take into account the perpendicular dispersion effects of the finite ion gyroradius proper.
CRs in typical astrophysical environments drive the oblique Alfvén instability in the MHD regime. For the well over-threshold CR currents |$\bar{j}_{\rm b}\gg \bar{j}_{\mathrm{thr}}$|, the asymptotic scaling of the oblique AW growth rate is |$\gamma _{\mathrm{m}}\sim 0.5\bar{j}_{\rm b}\omega _{Bi}$|, which is the same scaling as for the Bell instability. Moderate CR fluxes nCRVb ∼ 104 cm−2 s−1 (Zweibel & Everett 2010) are already well over-threshold and hence should drive both the oblique AW and Bell instabilities with the same growth rate γm ≃ 2.2 × 10−4 s−1. In this case we expect two distinct components of magnetic fluctuations in different wavenumber domains, generated by oblique (at large k⊥) and parallel (at large kz) Alfvén instabilities. The large-k⊥ component can accelerate CRs stochastically, converting energy of parallel flows into cross-|$\boldsymbol {B}_{0}$| energy of CRs. The growth rates of two instabilities become different in the near-threshold regime and/or in a hot background, which will be subject of future comparative studies.
This research was supported by the Belgian Science Policy Office (through Prodex/Cluster PEA 90316 and IAP Programme project P7/08 CHARM), and by the European Commission (through FP7 Program project 313038 STORM).
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