A&A 384, 1086-1097 (2002)
DOI: 10.1051/0004-6361:20011841
P. S. Joarder
Physics Division, Variable Energy Cyclotron Centre (VECC), 1/AF Bidhan Nagar, Kolkata, 700064, India
Received 2 June 2000 / Accepted 28 November 2001
Abstract
Propagating magnetosonic waves in the observed fine structures of
high-speed solar wind streams are theoretically examined, taking into account the non-parallel
propagation of such waves. It is found that non-parallel propagation introduces new
magnetoacoustic wavemodes, such as the forward-propagating slow
surface modes and the backward-propagating fast surface modes that propagate outward in a direction
away from the Sun; and the oppositely-propagating (slow and fast) body and surface modes
that propagate towards the Sun in a frame co-moving with the ambient flow external to the solar
wind flow-sheet. Such a wide variety of wavemodes
is not available in a case where the propagation is purely parallel to the axis of the
solar wind fine structure. It is argued here that the frequencies (in the satellite frame) of the outwardly propagating waves, that may transport photospheric/chromospheric oscillations into
the heliospheric space, possibly lie in the range 6-100 mHz. Such a high-frequency band has not so far been explored for the detection of magnetosonic waves in the high-speed solar wind.
Particularly interesting in the present study is the appearance of the sunward-propagating magnetosonic fast body waves. When viewed in a satellite (or solar) frame, such waves propagate towards the Sun provided that their angle of
propagation exceeds a certain critical value, so that their propagation-vector is nearly normal to
the solar equatorial plane. More high-resolution, multi-point in-situ observations are necessary
to detect such sunward-propagating magnetoacoustic fast body waves in the fine flow structures of the solar wind at a distance of 1 AU from the Sun.
Key words: Sun: solar wind - magnetohydrodynamics - waves
Recent observations made by two HELIOS spacecrafts have confirmed the existence of fine structures in high-speed solar wind flows. These structures are in the form of thin flow-sheets (or tubes) that are adjacent to each other with differences in their plasma parameters, such as their steady flow-speed along the magnetic field (Thieme et al. 1990). The structures may be separated by tangential discontinuities (TDs) in the magnetic field, across which the total (gas + magnetic) pressure is continuous. Such structures, therefore, are also called pressure balance structures (PBS; e.g. Tu & Marsch 1995) in the literature. In fact, Parker (1963; see also McCraken & Ness 1966; Mariani et al. 1973; Naugebauer 1981) first predicted the existence of such long and thin, coherent, spaghetti-like stream-structures as the constituent units of solar wind high-speed streams. These structures originate in the Sun, from where they spread out in the heliosphere, thus maintaining their identity even at a distance of 1 AU from the Sun.
Recently, Nakariakov et al. (1996; which is a corrected version of Mann et al. 1992) have shown that the fine solar wind flow-structures may serve as waveguides for magnetoacoustic waves that may be excited by motion of the structures' foot points that are possibly anchored in the photospheric/chromospheric layer of the Sun. These authors modelled an individual flow-structure as a finite-width slab (or sheet) with a reduced Alfven speed inside the slab and with an enhanced flow directed along the magnetic field parallel to the axis of the slab. This axis of the model flow-sheet was assumed to lie on the solar equatorial plane (see, for example, Burlaga 1995) pointing outwards from the position of the Sun. Nakariakov et al. (1996; referred hereafter as NRM96) then demonstrated that such a flow-sheet can sustain certain hydromagnetic wavemodes, namely, the backward, slow and fast body (kink and sausage) modes propagating along the sheet-axis in a direction away from the Sun. Such waves propagate backward relative to the flow inside the sheet with their phase-speed being smaller than the steady flow in the sheet (Nakariakov & Roberts 1995). Identification of such backward-propagating waves is important as these waves are also the negative energy waves (Joarder et al. 1997b) that may introduce new instabilities, such as the dissipative, resonant or explosive instabilities (Cairns 1979; Craik & Adam 1979; Craik 1985; Ryutova 1988; Hollweg et al. 1990; Ruderman & Goossens 1995; Ruderman et al. 1996; Tirry et al. 1998; Ruderman & Wright 1998; Andries et al. 2000) in solar wind fine structures. Such instabilities may play dominant role in the amplification of waves and in the excitation of MHD turbulence in solar wind.
In their calculations, NRM96 did not consider
the possibility of oblique propagation of waves; i.e. they ignored the component of propagation-vector
in a direction normal to
the solar equatorial plane containing both the axis and the direction of inhomogeneity
of the model flow-sheet. Such oblique propagation has recently been considered by Joarder & Satya Narayanan (2000)
in the context of the propagation of hydromagnetic surface waves in solar magnetic structures in the presence
of steady shear flows. It was shown there that the inclusion of an oblique propagation-vector
may introduce new surface waves that were not allowed by
the shear-flow to propagate in a direction purely parallel to the
field and the flow vectors. A similar property of non-parallel propagation of hydromagnetic waves was pointed out earlier
by several authors (e.g. Uberoi 1982; Somasundaram & Uberoi 1982; Rae & Roberts
1983; Jain & Roberts 1991; Joarder & Roberts 1992) in different contexts and in the absence of shear flows. We also note that Tirry et al. (1998)
and Andries et al. (2000) have recently analysed resonant flow
instability of obliquely propagating hydromagnetic surface waves in a finite-width transition region between two uniform, zero plasma-
magnetic media.
In view of continuing interest among the observers in the detection of hydromagnetic waves in solar wind (see the review by Tu & Marsch 1995) as an important agent for heating and accelerating the solar wind plasma and for exciting solar wind MHD turbulence, we here extend the analysis of NRM96 by incorporating the important effect of oblique propagation of waves on the magnetoacoustic spectrum of a model solar wind flow-slab. The normal modes of a fine-stream structure that we here examine have a component of their wavevector in a direction normal to the solar equatorial plane. We find that, in addition to considerably modifying the backward waves reported by NRM96, oblique propagation also allows for new forward and backward propagating hydromagnetic body and surface modes that yield further complexity in the dynamics of solar wind fine structures. Specially, an oblique propagation-vector allows some of the magnetoacoustic waves of the solar wind flow-sheet to propagate in a direction opposite to that of the plasma flow, i.e. in a direction towards the Sun, when viewed in a frame co-moving with the ambient solar-wind flow external to the model flow-sheet. Such oppositely propagating magnetoacoustic body and surface waves were entirely absent in the analysis of NRM96. It is here argued that some of the oppositely propagating body waves, with their propagation-vector nearly normal to the solar equatorial plane, may propagate towards the Sun even in a satellite frame (or, equivalently, in a frame fixed on the Sun; e.g. Kuijpers 1992; Cravens 1997). The existence of such sunward-propagating magnetoacoustic body waves is an important feature of the present calculation.
The plan of the paper is as follows. In Sect. 2, we describe an infinite slab (or sheet) model of the solar wind flow-structure and derive its magnetohydrodynamic dispersion relations. The properties of these dispersion relations are discussed in Sect. 3. The nature of waves and oscillations in a solar wind flow-sheet that may be relevant to observations, are presented in Sect. 4.
Following NRM96, we model the solar wind
flow structure as a plane magnetic slab of width 2a. The slab is infinitely
extended in the y- and the z-directions with the slab boundaries being
at .
Both the magnetic fields (inside
and outside
)
and the steady flows (inside
and outside
)
are directed along the long-axis (the z-axis) of the slab. The sound speeds are
inside the slab and
outside; and the Alfven speeds are
and
.
The unperturbed gas densities (
inside the slab
and
outside) are related by the condition of total pressure
balance
![]() |
(1) |
In this idealised model of a solar wind substructure, we may consider the plane
containing the x- and the z-axes to represent the solar equatorial plane with
the negative z-direction being the direction towards the position of the Sun. The y- axis is then directed along the
normal to the solar equatorial plane and is parallel to the axis of rotation
of the Sun. The effect of solar rotation, which is known to align the solar wind flow-tubes (or sheets)
along an Archimedean spiral (Parker 1963) with the spiralling angle subtended with the z-direction
at 1 AU being
around
for the fast solar wind stream-tubes, has however been ignored
in the present calculations. We expect that such a curvature of the flow-sheet may not have much bearing
on the approximate propagation properties of the magnetohydrodynamic waves in a long and
coherent fine structure of the fast solar wind stream. We note that
similar idealisations have earlier been successfully employed to analyse the approximate
properties of magnetoacoustic wavemodes in various solar magnetic structures, such as
the solar coronal plasma loops (e.g. Edwin & Roberts 1982, 1983; Roberts et al. 1984;
Nakariakov et al. 1999)
or the solar quiescent prominences (e.g. Joarder & Roberts 1993; Joarder et al. 1997a).
We now linearise the ideal MHD equations about the above equilibrium with
disturbances assumed to be of the form
![]() |
(2) |
Elimination from the linearised equations of all variables except
vx(x),
the amplitude of the x-component of velocity, yields the second order
ordinary differential equation (e.g. Joarder & Roberts 1992; Joarder & Satya Narayanan
2000)
![]() |
(3) |
![]() |
(4) |
![]() |
(5) |
![]() |
(6) |
In the following, we restrict ourselves only to the normal modes of oscillations (Rae & Roberts 1983) of the slab (or sheet) with the velocity amplitudes vx(x) supposed evanescent away from the slab (in
), implying
.
Considering further that both the normal component of
displacement and the perturbation in total (gas + magnetic) pressure are
continuous across the structure boundaries
,
we finally arrive at
the dispersion relations
![]() |
(7) |
We also note that Eqs. (6) and (7) can describe wavemodes propagating either in the direction
of the solar wind flow
(with kz > 0) or in a direction opposite to the flow (with kz < 0), as viewed in a frame co-moving with the external flow
.
The angle of propagation
may be given by the acute (
)
angle between the direction of
the wavevector
and the z-axis in both the cases. In the following,
we further assume ky > 0 simply for the sake of convenience, although
the results that we obtain remain equally valid in the case ky < 0 for waves
propagating in a direction opposite to the solar rotation vector along the normal
to the solar equatorial plane.
To describe the nature of normal modes that are the solutions of the
dispersion relations (7), we first choose a convenient frame of reference
co-moving with the external flow, so that
,
.
In this particular frame, the solutions of Eq. (7) that satisfy the
condition of lateral evanescence (
)
must have their field-aligned
phase-speed c such that either
,
or,
.
Following Roberts (1981a,b), we further classify these normal modes as the
surface (M20 > 0) and body (M20 < 0) modes. Equation (4) then
suggests that the modes with
,
or,
,
or,
are surface modes. Similarly, modes with
,
or,
,
or,
are body modes.
For surface mode solutions of Eq. (7), the
field-aligned phase-speed c satisfies an additional criterion that the factors
and
must be of opposite signs (Nakariakov & Roberts 1995).
It is convenient to define here six critical angles of propagation
to
that are given as the solutions of the equations
![]() |
= | ![]() |
(8a) |
![]() |
= | ![]() |
(8b) |
![]() |
= | ![]() |
(8c) |
![]() |
= | ![]() |
(8d) |
![]() |
= | ![]() |
(8e) |
![]() |
(8f) |
To discuss the behaviour of solutions of the dispersion relations (7), we first
note that the observed average values of various physical speeds in and out of the
solar wind flow-structure at a distance of 1 AU and in the aforesaid frame of
reference (co-moving with the external flow at a speed of 655
)
are
given as
,
,
and
(Thieme et al. 1990). These
values have also been considered by
NRM96 (see also, Mann et al. 1992) in their calculations for purely parallel propagation of
magnetoacoustic waves in a solar wind flow-structure. We simply consider these observed values
to examine the effect of oblique propagation on the wavemodes. In such a case, Eqs. (1) and (8) give
,
,
,
,
,
and
,
respectively. The observed values
for the physical speeds satisfy the condition
.
For this ordering of parameters,
normal mode solutions of Eq. (7) exist only in certain intervals of the longitudinal phase velocity c, depending on whether the direction of the longitudinal propagation-vector is parallel (implying kz > 0) or antiparallel (implying kz < 0) to the flow-vector
.
These two cases of longitudinal propagation are examined in detail in the following.
![]() |
Figure 1:
Variation of the field-aligned phase-speed c (in units of
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
Waves belonging to this category propagate in a direction away from the Sun. Normal mode solutions of Eq. (7),
that consist of such outwardly propagating waves, exist only in three propagation windows, namely, (i)
,
(ii)
and (iii)
.
We now proceed to briefly discuss the nature of wavemodes in these three intervals of the longitudinal phase-speed c.
(i)
:
when
,
so
that
(see Eq. (8)), only
one band of surface modes consisting of the (externally fast) magnetoacoustic slow (kink and sausage)
surface modes exists in this region that owes its existence solely to a
non-zero angle of propagation
.
These surface modes are shown in Fig. 1
for two different values of
,
namely,
and
,
respectively. This figure shows that, for
,
the field-aligned phase-speed c of the (externally fast)
slow surface modes satisfy a condition
.
For such
an angle of propagation
,
two new bands of modes, namely,
the (externally fast) magnetoacoustic slow body (kink and sausage) modes and the (externally fast) magnetoacoustic fast (kink and sausage) surface modes appear with their phase-speed c lying in the
intervals
and
,
respectively. Figure 2 shows the
fundamental, (externally fast) slow body (kink and sausage) modes and the (externally fast) fast sausage
surface mode, all for a particular angle of propagation
.
We may add here that the
fundamental, slow body kink mode transforms into an (externally fast) fast kink surface mode for
wavenumber
,
for which the field-aligned phase-speed c of the
mode satisfies a condition
.
Such large values of the dimensionless wavenumber kza is out of the range shown in Fig. 2.
As
approaches
,
the propagation band for the slow body waves
collapses to a single line
;
whereas the propagation band
for the fast surface waves changes to
in this limit of near-normal propagation with respect to the axis of the slab (sheet).
![]() |
Figure 2:
Field-aligned phase-speed c vs. dimensionless wavenumber kzafor the fundamental, (externally fast) magnetoacoustic slow body kink mode (continuous curve), the fundamental, (externally fast)
magnetoacoustic slow body sausage mode (lower broken curve) and the (externally fast) magnetoacoustic fast sausage surface mode (upper broken curve) in the flow-sheet for an angle of propagation
![]() |
Open with DEXTER |
(ii)
:
modes
appearing in this propagation band are the backward-propagating, magnetoacoustic slow body (kink and
sausage) modes that were found by NRM96 in a propagation-window
in the case of a purely parallel
propagation
along the direction of the flow. Such
backward body modes are shown in Fig. 3 for two different angles of propagation
.
The propagation-band for these slow body modes narrows down with the
increase of the angle
to ultimately collapse to a single line
as
approaches
.
![]() |
Figure 3:
Field-aligned phase-speed c vs. dimensionless wavenumber kzafor the fundamental, backward-propagating, magnetoacoustic slow body kink mode (denoted by the continuous curves) and the fundamental, backward-propagating, magnetoacoustic slow body
sausage mode (denoted by the broken curves) for two different values of the angle of
propagation ![]() ![]() ![]() |
Open with DEXTER |
(iii)
:
magnetoacoustic modes that are available in this interval of
phase-speed c are all displayed in Fig. 4 for different values of the angle of propagation
with respect to the direction of the steady flow
.
This figure shows that, for
,
we obtain the
backward-propagating, magnetoacoustic fast body (kink and sausage) modes and the backward-propagating, magnetoacoustic fast (kink and sausage)
surface modes with their phase-speeds lying in the propagation-regions
and
,
respectively. We note here that only the backward-propagating, fast body modes
were obtained by NRM96 in the propagation region
in the case of a purely parallel propagation
with
.
These body modes have critical wavenumbers
at which their phase-speed c drops to zero. Such critical wavenumbers are given by:
![]() |
(9a) |
![]() |
(9b) |
![]() |
(9c) |
![]() |
Figure 4:
Field-aligned phase-speed c vs. dimensionless wavenumber kzafor magnetoacoustic modes appearing inthe propagation window
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
The phase-speed c of the backward-propagating, fast body sausage modes approaches
as kza approaches infinity; whereas, the fundamental, backward-propagating, fast
body kink mode transforms into the backward-propagating, fast kink surface mode at
an intermediate value of the wavenumber kza, at which the longitudinal
phase-speed c for the kink mode equals
.
As
increases through its critical value
,
so that
,
the backward-propagating fast body modes disappear leaving only
the backward-propagating, fast (kink and sausage) surface modes in the propagation window
.
This situation is also shown in
Fig. 4 for
an arbitrarily-chosen angle of propagation
.
Note that the
fast kink surface mode is a backward-propagating mode only for wavenumbers
greater than a certain critical wavenumber
at which the phase velocity of this kink surface mode drops to zero. This critical
wavenumber is
given by the relation for the kink mode in Eq. (9) after replacing
N0 by
M0 = iN0 and
by
,
respectively.
As
exceeds the critical angle
,
the backward-propagating kink surface mode completely disapears. Only the backward mode, that survives such an angle of propagation
in the propagation window
,
is the fast sausage surface mode that now possesses
a critical wavenumber
;
see the curve in Fig. 4 that corresponds to
.
For a wavenumber
greater than this critical wavenumber, the backward fast sausage surface mode transforms
itself into an oppositely-propagating, magnetoacoustic fast sausage surface mode discussed
in Sect. 3.2. This critical wavenumber for the backward fast sausage surface mode
may again be obtained from the relation for the sausage mode in Eq. (9) after replacing N0 by
and
by
,
respectively.
In their calculations with a purely longitudinal wavevector (i.e. with ky = 0), NRM96 did not obtain magnetoacoustic waves
propagating in the negative z-direction in a frame co-moving with the external flow
.
This result seems to be an artifact of their choice of
physical speeds inside a solar wind substructure, so that
.
Although
we here choose the same set of values for the physical parameters as the one considered
by NRM96, the inclusion of a non-parallel propagation vector that yields
in our calculations allows for the existence of oppositely-propagating
magnetosonic wavemodes that propagate in a direction opposite to the direction
of the flow in a solar wind substructure with respect to a frame in which
.
The various
propagation windows for such oppositely-propagating magnetoacoustic modes are discussed
in the following.
(i)
:
when
,
so that
,
the wavemodes that appear in this propagation window are the oppositely-propagating,
(externally slow) magnetoacoustic fast body (kink and sausage) modes that are shown in Fig. 5 for a particular angle
of propagation
with respect to the vector
.
For such an angle of propagation
,
both the fast
body
modes possess critical wavenumbers
that are numerically the same as the critical wavenumbers pertaining to the backward-propagating, magnetoacoustic fast body (kink and sausage) modes displayed in
Fig. 4 in Sect. 3.1. Figures 4 and 5 together demonstrate that, for a magnitude of the wavenumbers larger than
critical wavenumbers, the oppositely-propagating, (externally slow) fast body modes are dragged along with the internal flow
so that the kink and sausage body modes
change their direction of propagation with respect to the direction of the flow to become
backward-propagating, fast body kink and fast body sausage modes, respectively.
![]() |
Figure 5:
Field-aligned phase-speed c vs. the magnitude of the dimensionless wavenumber |kza| for
various oppositely-propagating, magnetosonic wavemodes that appear in the
propagation-window
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
Such a critical wavenumber for the fast body sausage mode is
removed for
(see Eq. (8)), so that the longitudinal phase velocity cof the mode asymptotically approaches
for arbitrarily large magnitude of the
dimensionless wavenumber |kza|. For such an angle of propagation
,
the fundamental, fast body kink mode transforms into an oppositely-propagating,
(externally slow) fast kink surface mode at an intermediate value of |kza|, for which the phase velocity of the kink mode equals
.
Such behaviour of the oppositely-propagating, fast magnetosonic body and surface modes are displayed in Fig. 5 for an arbitrarily-chosen
angle of propagation
.
This figure further shows that,
for
,
the fundamental, fast body sausage mode possesses lower cut-off with the cut-off wavenumber
given by
![]() |
(10a) |
![]() |
(10b) |
As the angle of propagation
increases further, so that
(see, Eq. (8)), the
fast body modes completely disappear leaving only an oppositely-propagating, (externally slow) magnetoacoustic fast kink surface mode
with its longitudinal phase-speed c lying in the range
.
As
exceeds its critical value
,
both the oppositely-propagating, (externally slow) magnetoacoustic fast kink and fast sausage surface modes
appear in this propagation window with the sausage mode
having a critical wavenumber
.
For wavenumbers smaller than this critical wavenumber, the sausage mode
changes into a backward-propagating, magnetoacoustic fast sausage surface mode that was shown in Fig. 4.
Figure 5 shows such oppositely-propagating, (externally slow) fast (kink and sausage) surface waves
for an arbitrarily-chosen angle of propagation
.
![]() |
Figure 6:
Field-aligned phase-speed c vs. the magnitude of the dimensionless wavenumber |kza| for
various oppositely-propagating modes, that appear in the interval of phase-speed
![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Open with DEXTER |
(ii)
:
when
,
so that
(cf. Eq. (8)),
the wavemodes that are available in this propagation window are the oppositely-propagating,
(externally fast) magnetoacoustic fast body (kink and sausage) modes. This particular case is shown in Fig. 6 for
an arbitrarily-chosen angle of propagation
.
This figure shows that, for
,
both the kink and sausage fast body modes
have upper cut-offs with the cut-off wavenumbers given by
![]() |
(11a) |
![]() |
(11b) |
for the fundamental sausage mode, respectively. Here N0 = iM0 (see Eq. (4) in Sect. 2).
As
exceeds its critical value
,
so that
implying
,
the upper cut-offs for the (externally fast) fast body modes are removed. The phase-speed c of the fundamental, fast body
sausage mode now approaches
for
arbitrarily large magnitude of the wavenumber |kza|; whereas the fundamental,
fast body kink mode transforms itself into an oppositely-propagating (externally fast) magnetoacoustic fast kink surface mode
as its phase-speed c exceeds (
). In addition, we obtain an oppositely-propagating, (externally fast) magnetoacoustic fast sausage surface mode with its longitudinal phase-speed
lying in the interval
.
Such body and surface modes
are displayed in Fig. 6 for an angle of propagation
.
![]() |
Figure 7:
Field-aligned phase-speed c vs. magnitude of the dimensionless wavenumber |kza| for
the oppositely-propagating modes appearing in the propagation interval
![]() ![]() ![]() ![]() |
Open with DEXTER |
Finally, in Fig. 7, we display the oppositely-propagating, (externally fast) fast magnetoacoustic body and surface modes as the angle exceeds its critical value
.
We find that the propagation bands for the body and surface modes
are now distinctly separated with the body modes propagating in the region
and
the surface modes propagating in the region
.
We also note that the fundamental, fast body kink mode now has a lower cut-off with the
cut-off wavenumber given by:
![]() |
(12) |
Given thus the expected periods of outwardly-propagating waves in solar wind flow-sheets, our aim here is to theoretically identify such waves and
to calculate the approximate frequencies (which is also a measure of the wavelength in the z-direction; see for example, Kuijpers 1992; Cravens 1997)
Hz of these waves, that
may be measured in the in-situ observations by a spacecraft, or equivalently, by an observer fixed
in the frame of the Sun.
To perform such a task, it is required that we first examine the constraints
that may be imposed on the possible magnitudes of such wavelengths from various
physical and/or observational considerations.
Following a similar work by Hollweg (1982; see also discussions above) on
surface waves in solar wind tangential discontinuities (TDs), we here
assume that the waves are generated by motions in the x-y plane in the
photosphere/chromosphere of the Sun. In that case, the wavenumber ky can be
regarded as determined by the spatial-scales of the solar granular/supergranular motions. Hollweg (1982) considered a transverse wavelength
AU that was obtained
by extrapolating the mean distance between solar magnetic flux-tubes (Spruit
1981) out to 1 AU under the assumption that the distance scales as
,
with B being the magnetic field-strength. We here consider
this value
for the wavenumber
in the y- direction. For the maximum wavelength of magnetosonic
waves in the z-direction, we again emperically consider a value 0.01 AU, as this is
the approximate value for the observed correlation length of the fluctuating
(or, wave) part of the magnetic field in solar wind (Barnes 1979; see also
Cravens 1997). Although an explaination for the origin of such a correlation length cannot be given within the simple theoretical framework of the present paper, we still adapt this length as an upper limit for the magnitude of the longitudinal wavelength
in our calculations without any further justification. With the observed average value for the half-width "a'' of the flow-sheets
at 1 AU being also approximately 0.01 AU (Thieme et al. 1990), we thus obtain (see Sect. 2)
![]() |
(13) |
With the above bounds on the wave-parameters, we now turn to the numerical
solutions of Eq. (7) to calculate the frequency bands (in the satellite frame)
pertaining to various outwardly-propagating wavemodes that may present
periodicities in the above range. Our numerical results suggest that the
wavelengths (in the z-direction) of such waves are sufficiently small, so that, the angle of propagation for these waves are smaller than the critical angle
defined in Eq. (8) of Sect. 3. Waves that
exist in this situation are (i) the forward-propagating
magnetoacoustic slow surface waves (Fig. 1), (ii) the backward-propagating
magnetoacoustic slow body waves (Fig. 3) and (iii) the backward-propagating magnetoacoustic fast body
and fast surface waves (Fig. 4). We here note that the forward-propagating slow surface waves and the backward-propagating fast surface waves were
absent in the analysis of NRM96 as they confined themselves to the discussion of purely parallel propagation of waves in the flow-sheet.
In the satellite (or solar) frame and for periodicities in the range 3-20 min, the forward-propagating magnetoacoustic slow surface waves present frequencies in a range
mHz, while the
backward-propagating magnetoacoustic (slow and fast) body and surface waves present frequencies in a range 20-100 mHz. The frequency band of 6-100 mHz that we thus obtain are higher than
the frequency band (
Hz; see the review by Tu
& Marsch 1995) explored so far in search of magnetosonic waves in the
high-speed solar wind streams. The results of such observations
have often been negative, mostly showing the signatures of "PBS''s in solar wind
(e.g. Roberts 1990; Bavassano & Bruno 1989, 1991; Tu & Marsch 1991;
Marsch & Tu 1993). We however note, that Tu & Marsch (1994) have
recently attempted to explain some of the observed compressible fluctuations in
(
Hz frequency range in terms of a linear superposition of the "PBS''s
with large-scale, transverse, fast magnetosonic waves in solar wind. In this paper, we consider a much simpler problem of the guided magnetosonic waves in an individual solar wind flow-sheet. The frequency range of
(
Hz may be presented in our calculations by the forward and backward-propagating surface and body waves with
and
that have periods in the range 3 hrs to 3 days. Such long period waves may not be of solar origin, but may perhaps be generated in-situ by some istabilities, such as the
parametric instabilities (e.g. Tu et al. 1989) or the instabilities pertaining to the backward-propagating, negative energy waves (see references in Sect. 1). We here note that obliquely propagating magnetosonic waves may also be generated non-linearly by Alfven wave phase mixing
in an inhomogeneous plasma such as the solar wind flow-sheet with their rate of excitation being further modified in presence of steady shear flows; cf. Nakariakov et al. (1997, 1998).
In their calculations, NRM96 obtained
standing magnetosonic body waves in the frame of the external flow with wavelengths that
correspond to the critical wavenumbers
(see Eq. (9), Sect. 3.1) at which the field-aligned phase-speed c of the fundamental,
backward-propagating, fast body kink and sausage waves drops to zero. In our numerical calculations, with
for example, we obtain only one such stationary body mode that corresponds to the fundamental, backward-propagating, fast body sausage mode with a wavelength of about
km along the axis of the solar wind flow-sheet. We here note that, for
,
the numerical value of the critical wavelength pertaining to the fundamental, backward-propagating, fast body kink mode is always longer than 0.01 AU, i.e. longer than the observed coherence length of magnetic fluctuations in solar wind flow (see discussions above). We therefore leave any further examination of such stationary fast body kink mode out of the present discussion. We however note, that in addition to the abovementioned stationary fast body sausage mode, two standing (kink and sausage) fast surface modes also appear in our calculations with
that correspond to the backward-propagating, fast (kink and sausage) surface modes (see Fig. 4) with their critical wavenumbers
.
Alongwith the standing fast body sausage wave, such stationary fast surface waves may possibly be detected in a frame co-moving with the ambient flow
of the solar wind flow-sheet.
For extremely large longitudinal wavenumber
,
but for a finite value of
thus leading to
,
we obtain a situation similar to the one discussed by NRM96, where the only surviving modes are the backward-propagating,
magnetoacoustic slow and fast body (kink and sausage) modes (Figs. 3 and 4). Such backward body modes propagate in an outward direction with a common longitudinal phase-speed
in the frame of the Sun. All such backward body waves, however, propagate in a
sunward (i.e., negative z-) direction with a common phase-speed of
as viewed in a frame co-moving with the internal flow
of the flow-sheet.
If, on the other hand, we consider an extremely large angle of propagation
with respect to the flow vector
,
while considering
to be finite thus implying
,
the only outwardly-propagating wavemodes that we obtain are the forward-propagating (externally fast) magnetosonic slow and fast surface modes (Figs. 1 and 2). The phase-speed c for both the kink and sausage slow surface modes is given by
![]() |
(14) |
In the case of an arbitrarily small angle of propagation
with the transverse wavenumber
remaining finite, the existence of various cut-offs and critical wavenumbers ensure that no surface or fundamental body waves propagate in the flow-sheet in an inward direction in a frame co-moving with the external flow
.
If, on the other hand, we consider a very large angle of propagation
,
while keeping the magnitude for the longitudinal wavenumber |kza|
to be finite thus leading to a very large transverse wavenumber
,
we obtain three classes of oppositely-propagating fundamental wavemodes, namely, (i) the (externally slow) magnetoacoustic fast surface modes (Fig. 5), (ii) the (externally fast) magnetoacoustic fast surface modes (Fig. 7), and (iii) the (externally fast) magnetoacoustic fast body modes (Fig. 7).
Consider first the oppositely-propagating, (externally slow) fast surface modes. The longitudinal phase-speed c for both these kink and sausage surface modes are given by
![]() |
(15) |
As
with
,
the longitudinal phase speed c for
the oppositely-propagating (externally fast) fast surface modes approaches a limit
that yields a numerical value of
in the
frame of the Sun.
The oppositely-propagating, (externaly fast) magnetosonic, fast body kink and fast body sausage modes are of particular
interest. For
with |kza| remaining finite, the longitudinal phase-speed c of these inward-propagating fast body modes can be given (in a frame co-moving with the external flow) by the following approximate formulae:
![]() |
(16a) |
![]() |
(16b) |
![]() |
(16c) |
![]() |
(16d) |
Finally, it should be borne in mind that the linear magnetohydrodynamic wave theory, that we here apply to describe waves in a solar wind flow-structure, may not provide an accurate description for the solar wind plasma at a distance of 1 AU from the Sun. A collisionless plasma theory employing Vlasov-Maxwell equations seems, on the other hand, to be more appropriate to describe fluctuations in plasma variables in solar wind flows (Barnes 1979). Such a kinetic description of solar wind plasma predicts strong "Landau damping'' of certain wavemodes that is not captured in the MHD description of waves presented here. An appropriate description of the complex interaction of magnetosonic waves with the solar wind pressure balance structures, that are believed to give rise to the observed compressible fluctuations in solar wind (e.g. Tu & Marsch 1994, 1995), is also complicated. Various specialised techniques, such as the "Pseudosound Theory'' and the "NI-MHD Theory'' (e.g. Montgomery et al. 1987) accompanied by computer simulations, are generally used to study the nature of such compressible fluctuations in solar wind.
In this paper, we, on the other hand, considered a simpler theoretical problem of propagation of linear magnetosonic waves in an isolated, model solar wind flow-sheet. The wavemodes that we find here must have their counterparts, perhaps in a much modified form, in more sophisticated theoretical treatments of the fluctuations of plasma variables in solar wind high-speed flows. Our analysis, therefore, may serve as a useful preliminary step towards the development of a more advanced theory to understand waves and turbulence in the inhomogeneous solar wind.
Acknowledgements
The author is indebted to Dr. V. M. Nakariakov for many helpful discussions and continuous encouragement. He also acknowledges useful comments of an anonymous referee on an earlier version of the paper that helped him in improving the content and presentation of the present version. He takes this opportunity to thank Dr. A. V. Thampan, Dr. Sonjoy Majumder and Mr. Baba Varghese for their help in the preparation of the manuscript. The earlier version of this paper was communicated by the author from the Indian Institute of Astrophysics, Bangalore, India-560034. Most of the revisions, leading to the present version, have been carried out during December, 2000 to July, 2001 when the author was a visiting scientist at the Inter-University Centre for Astronomy and Astrophysics (IUCAA), Pune, India -411007. The author thanks the Director, the scientists and the staff of IUCAA for providing much needed help and facilities. He is also thankful to the Director, VECC for offering him a fellowship for continuing research in solar magnetohydrodynamics.