On Kinetic Slow Modes, Fluid Slow Modes, and Pressure-balanced Structures in the Solar Wind
Daniel Verscharen (UNH), Christopher H. K. Chen (Imperial College),, Robert T. Wicks (MSSL/UCL)

TL;DR
This paper investigates the nature of slow modes in solar wind turbulence, deriving kinetic dispersion relations, comparing them with fluid models, and analyzing observational data to understand plasma behavior.
Contribution
It provides analytical gyrokinetic expressions for ion-acoustic wave dispersion and compares kinetic, MHD, and observational results, highlighting discrepancies and fluid-like behavior.
Findings
Kinetic and MHD models show major differences at high plasma beta.
Observations align better with MHD predictions than kinetic theory.
Solar wind plasma exhibits more fluid-like behavior than kinetic models suggest.
Abstract
Observations in the solar wind suggest that the compressive component of inertial-range solar-wind turbulence is dominated by slow modes. The low collisionality of the solar wind allows for non-thermal features to survive, which suggests the requirement of a kinetic plasma description. The least-damped kinetic slow mode is associated with the ion-acoustic (IA) wave and a non-propagating (NP) mode. We derive analytical expressions for the IA-wave dispersion relation in an anisotropic plasma in the framework of gyrokinetics and then compare them to fully-kinetic numerical calculations, results from two-fluid theory, and MHD. This comparison shows major discrepancies in the predicted wave phase speeds from MHD and kinetic theory at moderate to high . MHD and kinetic theory also dictate that all plasma normal modes exhibit a unique signature in terms of their polarization. We…
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On Kinetic Slow Modes, Fluid Slow Modes, and Pressure-balanced Structures in the Solar Wind
Daniel Verscharen1, Christopher H. K. Chen2, and Robert T. Wicks3
1Space Science Center and Department of Physics, University of New Hampshire, Durham, NH 03824, USA; [email protected]
2Department of Physics, Imperial College London, London SW7 2AZ, UK; [email protected]
3Mullard Space Science Laboratory, University College London, London WC1E 6BT, UK; [email protected]
(Received 2017 March 6; accepted 2017 March 28; published 2017 May 12)
Abstract
Observations in the solar wind suggest that the compressive component of inertial-range solar-wind turbulence is dominated by slow modes. The low collisionality of the solar wind allows for nonthermal features to survive, which suggests the requirement of a kinetic plasma description. The least-damped kinetic slow mode is associated with the ion-acoustic (IA) wave and a nonpropagating (NP) mode. We derive analytical expressions for the IA-wave dispersion relation in an anisotropic plasma in the framework of gyrokinetics and then compare them to fully kinetic numerical calculations, results from two-fluid theory, and magnetohydrodynamics (MHD). This comparison shows major discrepancies in the predicted wave phase speeds from MHD and kinetic theory at moderate to high . MHD and kinetic theory also dictate that all plasma normal modes exhibit a unique signature in terms of their polarization. We quantify the relative amplitude of fluctuations in the three lowest particle velocity moments associated with IA and NP modes in the gyrokinetic limit and compare these predictions with MHD results and in-situ observations of the solar-wind turbulence. The agreement between the observations of the wave polarization and our MHD predictions is better than the kinetic predictions, which suggests that the plasma behaves more like a fluid in the solar wind than expected.
Subject headings:
plasmas – solar wind – turbulence – waves
††journal: The Astrophysical Journal, 840:106 (8pp), 2017 May 10
1. Introduction
According to the magnetohydrodynamic (MHD) approximation, a collisional plasma supports four types of linear modes: the Alfvén wave, the fast-magnetosonic wave, the slow-magnetosonic wave, and the entropy mode. While the Alfvén wave is noncompressive, the two magnetosonic waves exhibit changes in the density and the magnetic-field strength , which are positively correlated in the case of the fast wave and anticorrelated in the case of the slow wave. According to the more generally valid kinetic theory, a plasma supports an infinite number of linear modes. With a few exceptions, these modes are heavily damped. The Alfvén wave and the magnetosonic solutions can still be identified in kinetic theory by their polarizations and dispersion relations (Stix 1992; Gary 1993; Klein 2013).
The solar wind is a turbulent, and often collisionless, magnetized plasma that carries a minor component of compressive fluctuations (Tu & Marsch 1995). In situ observations indicate that density and field-strength fluctuations in the inertial range are anticorrelated (Bavassano & Bruno 1989; Yao et al. 2011; Howes et al. 2012; Klein et al. 2012; Yao et al. 2013a, b), which suggests that the compressions can be usefully modeled as slow modes under the assumption that strong plasma turbulence retains certain characteristics of linear plasma modes (Klein et al. 2012; Salem et al. 2012; Chen et al. 2013; Howes et al. 2014). Observations also show that the compressive fluctuations are more anisotropic than the Alfvénic fluctuations, with (Chen et al. 2012; Chen 2016), where () is the perpendicular (parallel) component of the wave vector with respect to the background magnetic field. Some literature interprets part of the compressive fluctuations as pressure-balanced structures (PBSs) (i.e., structures in which the variation in the thermal pressure and the variation in the magnetic pressure balance so that the total pressure stays constant Burlaga & Ogilvie 1970; Vellante & Lazarus 1987; Burlaga et al. 1990; Zank et al. 1990; Zank & Matthaeus 1993; Marsch & Tu 1993; Tu & Marsch 1994; McComas et al. 1995; Ghosh et al. 1998; Reisenfeld et al. 1999; Bavassano et al. 2004; Yao et al. 2011; Verscharen et al. 2012; Narita & Marsch 2015; Yang et al. 2017). The large collisional mean free paths in the solar wind suggest that a kinetic description of these fluctuations that incorporates effects due to deviations from thermodynamic equilibrium, such as the commonly observed temperature anisotropies with respect to the background magnetic field, is necessary (Marsch et al. 1982; Kasper 2002; Kasper et al. 2002; Hellinger et al. 2006; Bale et al. 2009; Chen et al. 2016; Verscharen et al. 2016).
In kinetic theory, the two modes that are most similar to the slow-magnetosonic mode are the ion-acoustic (IA) wave and a nonpropagating (NP) mode depending on the plasma parameters (Howes et al. 2006). We refer to these modes as kinetic slow modes. The purpose of this work is to discuss the dispersion relations and the polarization properties of the IA wave, the NP mode, and the MHD slow mode. We use the fluctuations in the three lowest particle velocity moments (density, velocity, and pressure) as observable markers for the polarization of the compressive component of the solar-wind turbulence. By comparing our predictions for these markers with in-situ solar-wind observations, we distinguish between IA-mode-like, NP-mode-like, and MHD-slow-mode-like behavior. For more details on the IA and NP modes, and a comprehensive derivation of their dispersion relations, we recommend the extensive treatments by Howes et al. (2006), Schekochihin et al. (2009), and Kunz et al. (2015).
2. Dispersion Relations and Damping Rates of Kinetic Slow Modes
Assuming large wavelengths (), low frequencies (), and in an electron–proton plasma, where is the proton gyroradius, is the real part of the frequency , and is the proton gyrofrequency, the gyrokinetic dispersion relation (see Appendix A for a sketch of the derivation) contains two distinct types of slow modes (Howes et al. 2006; Schekochihin et al. 2009). In the limit of low111We make the assumption that all interspecies temperature ratios, as well as all and , are much less than . and low , the slow-mode part of the dispersion relation describes IA waves. In the limit of high and high , the slow-mode part of the dispersion relation describes NP modes, where , , is the background density of species , and is the Boltzmann constant. We define the temperature anisotropy of species as , where , and () is the perpendicular (parallel) temperature of species with respect to the background magnetic field .
According to our derivation in Appendix A, IA waves fulfill the dispersion relation
[TABLE]
where (Stix 1992; Gary 1993; Narita & Marsch 2015)
[TABLE]
is the IA speed, and is the particle mass of species . As pointed out by Gary (1993), a comparison between Equation (2) with two-fluid theory, in which and
[TABLE]
implies that—to the degree to which an adiabatic behavior applies to the kinetic solution—the specific heat ratios in IA waves fulfill and for protons and electrons, respectively. From this point of view, protons behave like a one-dimensional adiabatic component due to their degree of freedom along , while electrons behave like an isothermal component due to their large thermal speed compared to the wave phase speed. The imaginary part of the IA-wave frequency is given by
[TABLE]
where is the parallel thermal speed of the protons. The derivation of Equations (1) and (4) requires the assumption that so that , although a comparison with numerical results in Figure 1 will show that Equation (1) is a good approximation for even . Equation (4) reduces to the result given by Howes et al. (2006) for an isotropic plasma with . The approximated IA dispersion relation in Equations (1) and (4) does not depend on since the restoring force in the IA wave is solely due to the parallel pressure gradients of the protons and electrons (also see Basu 2008).
According to our derivation in Appendix A, NP modes fulfill the dispersion relation (also see Foote & Kulsrud 1979; Howes et al. 2006; Kunz et al. 2015) and
[TABLE]
where is the proton Alfvén speed. The NP mode can become unstable () according to Equation (5) if
[TABLE]
which is the mirror-mode instability criterion.
For the sake of brevity, we limit ourselves to the isotropic case for the following numerical evaluations of the dispersion relation. In Figure 1, we compare Equation (1) with numerical results of the fully kinetic hot-plasma dispersion relation obtained with the numerical code NHDS (Verscharen et al. 2013). For reference, we show the MHD slow-mode dispersion relation,
[TABLE]
where
[TABLE]
is the slow-magnetosonic speed, is the ratio of thermal to magnetic pressure, and is the specific heat ratio. We set and . We denote the angle between and as .
While the numerical and the analytical dispersion relations for the IA wave agree well with each other (even at high ), the MHD solution shows a significant deviation from the kinetic solutions, especially at high .
In Figure 2, we compare Equations (4) and (5) with NHDS solutions. For this parameter set, the analytical results and the numerical results agree well for the NP mode at high , as assumed in the derivation of Equation (5). Even at low , Equation (4) and the numerical IA solution deviate from each other, which is attributed to finite- effects. Using this parameter set, the numerical damping rates of both modes are equal at .
3. Polarization Properties and Relation to Pressure-balanced Structures
We use the distinct polarization properties of the IA, NP, and MHD slow modes to identify the dominating mode in the solar wind. For that purpose, we define the dimensionless quantities , , , and as the normalized observable amplitudes of fluctuations in the three lowest velocity moments:
[TABLE]
where is the amplitude of fluctuations in the particle number density;
[TABLE]
where is the amplitude of fluctuations in the -parallel bulk velocity; and
[TABLE]
where () is the amplitude of fluctuations in the thermal pressure in the direction that is perpendicular (parallel) to , and . We derive expressions for , , , and in the gyrokinetic limit in Appendix B and give the MHD equivalents in Appendix C. Although all of these fluctuating moments are observable identifiers for the underlying plasma modes, the fluctuations in the total pressure play a decisive role due to the prominent observations of PBSs in the solar wind. Therefore, we define the normalized amplitude of fluctuations in the thermal pressure as
[TABLE]
With , we find
[TABLE]
In MHD, PBSs are associated with the MHD slow mode in the quasi-perpendicular limit (Tu & Marsch 1995; Kellogg & Horbury 2005; Klein 2013), which suggests that the IA wave and the NP mode are associated with the kinetic counterparts of PBSs. All wave solutions in the gyrokinetic approximation fulfill the perpendicular pressure balance according to Equation (B1). However, the pressure balance commonly associated with PBSs implies that the sum of the total thermal pressures and the magnetic pressure remain constant:
[TABLE]
where . Linearizing Equation (15) leads to
[TABLE]
With , pressure balance according to Equation (15) is then achieved if
[TABLE]
The quantities , , , , , and are complex quantities. For their comparison with observations in Section 3.2, we express them in terms of their magnitude and phase angle .
3.1. Observational Methods
For the observational analysis, we use data from the WIND spacecraft (Acuña et al. 1995) in the solar wind at 1 au. We use magnetic-field data from the MFI instrument (Lepping et al. 1995) at 3 s resolution. For the particles, we use the ground-calculated moments from the 3DP instrument (Lin et al. 1995), at 24 s resolution for the ions and at 98 s resolution for the electrons. We split the data from the period 2004 July 1 to 2014 December 31 into non-overlapping 1 hr intervals and then linearly interpolate data gaps. We exclude intervals with data gaps greater than 5% from the analysis.
In each 1 hr interval, we determine the mean and fluctuating values in order to calculate the polarization properties , , and , as defined in Section 3. We determine and as averages over each interval and determine and from those averages. We also determine from the average density, magnetic field, and parallel temperature of the interval. For the amplitudes of , , and , we calculate the rms values of each quantity. For the phases of , , and , we calculate the wavelet coherence spectrum (Torrence & Compo 1998),
[TABLE]
for each quantity , where is the continuous Morlet-wavelet transform of at scales and positions , and is a smoothing operator in time and scale. The phase is defined as the coherence phase,
[TABLE]
We then take the average over scales between 1 hr and 15 minutes. At shorter timescales, instrument noise would contaminate our results. In our data analysis, we use instead of in the definitions of , , and in order to reduce uncertainties in the determination of the -parallel direction. In the limit in which our linear analysis is valid, . We then create two-dimensional histograms in the -, -, and - planes, and then bin the data logarithmically in and , and linearly in and . Last, we normalize each column of data in the histogram at a constant by the peak counts in that column so that each column is independently normalized to show the peak in the variable at a fixed .
3.2. Results
According to observations (e.g., Kasper 2002; Kasper et al. 2002; Hellinger et al. 2006; Bale et al. 2009; Chen et al. 2016), the mirror-mode and firehose thresholds set approximate upper and lower limits on . Therefore, we set the maximum and minimum values of in our calculations to the values that fulfill Equation (6) (labeled as “IA/NP mirror”) or Equation (A23) (labeled as “NP firehose”), after replacing the inequality signs with equality signs. These curves identify the extreme values for , , and in an anisotropic plasma. For a comparison, we also include the results from isotropic MHD as derived in Appendix C.
We show the numerical and observational results for the zeroth velocity moment () as functions of in Figure 3.
Our theoretical results indicate that the vast majority of the data exhibit phase angles of , which shows a strong anticorrelation between and . The MHD prediction is shown for . Although the NP-mode prediction agrees better with the observations at large than the IA-wave prediction and vice versa, the MHD solution shows the best agreement overall with the observations of in both the magnitude and phase. In the highly oblique limit, Equation (C5) leads to . A best fit to the data in Figure 3 using this limit shows that the observed -behavior of the large-scale compressive fluctuations in the solar wind corresponds to the MHD behavior of highly oblique slow modes with
[TABLE]
where the error margin represents the statistical error of the fit only.
We compare our predictions for the first velocity moment () with observations in Figure 4.
Our theoretical results show that is much greater in the IA wave than in the NP mode. While the theoretical NP-mode solutions for and at the firehose threshold exhibit a -phase shift between and , the observations predominantly exhibit a phase shift of and . As in the case of , the MHD solution shows the best agreement with the observations of in both the magnitude and phase. We note, however, that the measurement of is prone to Alfvénic leakage, which increases the uncertainty of this observation. Alfvénic leakage is a result of the dominant Alfvénic fluctuations and their characteristic (anti-)correlation between and . Fluctuations on time scales comparable to the time scale we use in defining introduce inaccuracies to our projections of and onto the -parallel direction. Consequently, some of the strong transversal Alfvénic fluctuations in and appear as partly field-parallel. Alfvénic leakage creates signals at phases of both and .
Lastly, we show our results for in Figure 5.
The IA wave and the NP mode do not fulfill Equation (17). The MHD prediction exhibits a full pressure balance and a reasonable agreement with the observations, especially at .
4. Discussion and Conclusions
The long-wavelength kinetic slow mode is associated with two types of compressive modes: the IA wave and the NP mode, both of which exhibit an anticorrelation between and . A comparison of the damping rates of the IA mode and the NP mode suggests that the IA mode is the dominating kinetic slow mode at low , while the NP mode is the dominating kinetic slow mode at high . Temperature anisotropies alter the dispersion relations and the damping behavior of slow modes in kinetic plasmas, and can drive the NP mode (i.e., the mirror mode) to be unstable.
While MHD does not account for the NP mode222We note that the MHD entropy mode shares certain characteristics with the NP kinetic slow mode; however, there are significant differences between these modes. For example, the MHD entropy mode does not have fluctuations in . or the kinetic damping of slow modes, the -dependence of for the IA wave is roughly represented by the MHD dispersion relation at low . At high , however, the MHD approximation does not agree with the dispersion relations of either type of kinetic slow modes. Our careful comparison of theoretical predictions for the three lowest particle velocity moments associated with IA, NP, and MHD slow modes with observations suggests that the compressive component of the solar-wind fluctuations is not IA-wave- or NP-mode-like. Our MHD slow-mode calculation predicts the observed -dependence of well, which corroborates the notion that the MHD slow mode is a potential candidate for PBSs observed in the solar wind (Kellogg & Horbury 2005; Yao et al. 2013a, b).
Klein et al. (2012) compare the normalized correlation between and in a synthetic spacecraft dataset based on a combination of slow and fast modes with observations. In their analysis, the synthetic data based on a superposition of critically-balanced IA waves explain the observed -dependence of the normalized correlation for better than the synthetic data based on a superposition of MHD waves. Applying Klein et al.’s (2012) synthetic spacecraft data method to our markers , , and over a wider -range using a composition of IA, NP, and other kinetic and MHD modes may lead to observable predictions that clarify the nature of the compressive component of the solar-wind turbulence. In addition, appropriate fully nonlinear turbulence simulations can determine the behavior of slow modes in a turbulent background. However, these studies are beyond the scope of our work.
Although the large collisional mean free paths in the solar wind suggest a preference of kinetic models over MHD models, our observations agree better with the MHD solutions than with the IA-wave or NP-mode solutions. Our study, therefore, suggests that the large-scale compressive fluctuations in the solar wind behave more fluid-like than kinetic-slow-mode-like. Even the restriction of our data to measurements with low collisional age, (Kasper et al. 2008; Bourouaine et al. 2011), or a reduction of the average time from 1 hr intervals to 10 minute intervals does not change this result (plots for these restrictions are not shown). This discovery suggests that some fundamental process, which remains to be identified, creates an effective collisionality and thus the requirements for the application of the MHD framework. Possible candidates for such processes include the inhibition of the development of fine structures and damping due to anti-phasemixing (see Section 5.3 in Schekochihin et al. 2016), scattering by wave–particle collisions and kinetic instabilities (Riquelme et al. 2015; Kunz et al. 2016; Riquelme et al. 2016; Verscharen et al. 2016; Yoon 2016), or the isotropization due to the dissipation of electric fluctuations (Bale et al. 2005). These processes may be scale-dependent, so that a faster measurement cadence could reveal a more kinetic-slow-mode-like behavior on short time scales. The instrumentation on the upcoming missions Solar Orbiter and Solar Probe Plus will provide appropriate measurements for such a scale-dependent study.
We thank Ben Chandran and Kris Klein for very helpful discussions. D.V. is supported by NSF/SHINE grant AGS-1460190 and NASA grant NNX16AG81G. C.H.K.C. is supported by an STFC Ernest Rutherford Fellowship.
Appendix A Appendix A
Derivation of the Dispersion Relation in the Gyrokinetic Approximation
In this appendix, we sketch the derivation of the gyrokinetic slow-mode dispersion relation in an anisotropic plasma combining the derivations given by Howes et al. (2006) and Kunz et al. (2015) and using their notation. For simplicity, we assume a bi-Maxwellian background distribution function:
[TABLE]
where . In the gyrokinetic ordering (), the distribution function is decomposed as
[TABLE]
where
[TABLE]
is the Boltzmann response, is the gyrokinetic response, is the charge of species , is the electrostatic potential, is the vector potential, and is the speed of light. The collisionless gyrokinetic equation to first order in is then given by
[TABLE]
where , and is the Poisson bracket. The symbol indicates the ring average at the fixed gyrocenter of species .
Applying a plane-wave ansatz to allows us to express the ring average in terms of Bessel functions of order , , which yields
[TABLE]
The three lowest velocity moments of the fluctuating gyrokinetic distribution function to first order (i.e., the Boltzmann response and the gyrokinetic response) describe the fluctuations in density, bulk velocity, and the perpendicular and parallel thermal pressures as:
[TABLE]
[TABLE]
[TABLE]
[TABLE]
where we evaluate the integrals over in terms of the modified Bessel functions with , , , , and with the argument . We express the integrals over in terms of the standard plasma dispersion function (Fried & Conte 1961)
[TABLE]
along the Landau contour , where .
With these relations, the condition of quasi-neutrality, the parallel component of Ampère’s law, and the perpendicular components of Ampère’s law (), where is the fluctuating part of the current density, yield:
[TABLE]
and
[TABLE]
As shown by Howes et al. (2006), we can write Equations (A11) through (A13) as
[TABLE]
for , where
[TABLE]
and . Setting the determinant of the matrix in Equation (A14) to zero leads to the nontrivial solutions of the gyrokinetic dispersion relation, which fulfill
[TABLE]
The term on the right side of Equation (A21) represents coupling terms that can be neglected for long wavelengths. In the long-wavelength limit (), we apply the approximations , , and . Furthermore, we neglect all terms given the assumed constrains on the temperature ratios.
The first term on the left side of Equation (A21) represents the Alfvén solution, and the second term represents the slow-mode solution. In the long-wavelength limit, the Alfvén branch reduces to , which leads to the Alfvén dispersion relation
[TABLE]
If the expression in parentheses in Equation (A22) becomes negative, this root of the dispersion relation describes the firehose instability with the instability criterion
[TABLE]
The slow-mode branch can be analytically simplified in two limits. In the low- limit, the slow-mode dispersion relation becomes . Using the expansion
[TABLE]
and leads to
[TABLE]
Under the assumption that and , the real part of Equation (A25) leads to Equation (1), and the imaginary part of Equation (A25) leads to Equation (4).
In the high- limit, the slow-mode dispersion relation becomes . Using the expansion and , this solution leads to the dispersion relation of the NP mode, and Equation (5).
Appendix B Appendix B
Derivation of Moment Fluctuations in the Gyrokinetic Approximation
The perpendicular component of Ampère’s law in gyrokinetics implies a pressure balance in the form of
[TABLE]
where
[TABLE]
is the perpendicular pressure tensor and is the ring average at fixed position .
For a given solution to the dispersion relation, Equation (A14) provides the polarization relations that connect the three amplitudes , , and :
[TABLE]
where
[TABLE]
and
[TABLE]
With Equations (A6) through (A9), (B4), and (B5), we find for the normalized fluctuations in the three lowest velocity moments:
[TABLE]
[TABLE]
[TABLE]
[TABLE]
where
[TABLE]
We then calculate the factor with Equation (14). We evaluate Equations (B6) through (B9) after solving Equation (A14) numerically (i.e., without approximating and ) for , , and . In the marginally stable case for the mirror-mode instability, the NP mode fulfills , , , and Equation (6), after replacing the inequality sign in Equation (6) with an equal sign.
Appendix C Appendix C
MHD Polarization Relations
Linearizing the ideal adiabatic MHD equations for a proton fluid,
[TABLE]
[TABLE]
[TABLE]
[TABLE]
where is the fluid velocity and is the pressure, leads to slow-magnetosonic wave solutions with the dispersion relation given by Equations (7) and (8). Combining Equations (C1) through (C4) with Equations (9), (10), and (13) leads to (Verscharen et al. 2016)
[TABLE]
[TABLE]
and
[TABLE]
We note that describes the effect of the total isotropic pressure instead of the proton partial pressure alone.
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