A&A 482, 1009-1014 (2008)
DOI: 10.1051/0004-6361:20078980
O. V. Arkhypov1 - H. O. Rucker2
1 - Institute of Radio Astronomy, National Academy of Sciences of Ukraine,
Chervonopraporna 4, 61002 Kharkiv, Ukraine
2 -
Space Research Institute, Austrian Academy of Sciences,
Schmiedlstrasse 6, 8042 Graz, Austria
Received 2 November 2007 / Accepted 1 February 2008
Abstract
There are theoretical and experimental arguments for a modulation of
Jovian decametric S-emission by standing Alfvén waves in the
regions of radio sources. One effect of such modulation is the
concentration of S-burst emission around certain frequencies
(S-bands) in dynamic spectra of radio emission. It is argued that
S-bands are generated at the local electron cyclotron frequencies,
around nodes of a standing Alfvén wave. To test this hypothesis,
we derived several verifiable predictions: the anti-correlation of
radio-flux in adjacent S-bands at short time scales (<0.1 s); the
correlation of frequency shifts of S-bands at long time scales
(>0.1 s); and the transformation of the broadband S-storm into
S-bands. We searched for and found these effects experimentally.
Because the predictions are confirmed, the standing wave modulation
of Jovian S-emission appears valid.
Key words: planets and satellites: individual: Jupiter - magnetohydrodynamics (MHD) -
plasmas - magnetic fields - waves -
radiation mechanisms: non-thermal
Short (S) bursts of Jovian decametric emission (DAM) with the time
scale of
s form trains or bands near certain
frequencies in dynamic spectra. Previous studies focused mainly on
the microstructure of such trains with a time scale of
s and a frequency band of
MHz
(see references in Litvinenko et al. 2004).
However, previous studies did not focus on the trains'
macrostructure (
s and/or
MHz), and obtained
different interpretations.
Leblanc & Genova (1981) found that the S-burst
emission in dynamic spectra is arranged into a pattern of repetitive
features, drifting to low frequencies with time. These features were
interpreted as incomplete arcs with late vertex which reflect the
radiation pattern in the form of thin conical sheets. Analogical
arcs of long (L;
s) DAM bursts show certain frequency
drift at f>20 MHz: positive in Io-B storms and negative in Io-AC spectra (Leblanc 1981). However, the S-structures,
drifting to high- or low-frequencies or without any drift, were
observed in the Io-B storm of January 4, 1993 by three observatories
simultaneously (Boudjada et al. 1995). Moreover,
after averaging many S-storms it was found that S-emission
concentrates near certain frequencies (Ryabov et al. 1985). Hence, the macrostructure of S-emission is more complicated than the arc pattern.
Some authors considered S-trains as a system that reflects wave disturbances of the radio-source's magnetic lines. Quasi-periodic bulbs moving along the Io-flux tube (Ryabov et al. 1997) or magnetohydrodynamic waves on its border (Boev et al. 1993) were suggested. The standing Alfvén wave in the Jovian ionospheric resonator is considered as a stimulus for S-burst generation (Ergun et al. 2006). In previous paper, we confirmed that average oscillations of S-emission probability with frequency corresponds to a standing Alfvén wave (Arkhypov & Rucker 2006).
We test here new predictions of the standing Alfvén wave hypothesis on the micro-structural (Sect. 2) and macro-structural (Sect. 3) levels. The results are in favor of the connection of S-bands with nodes of standing modulation waves (Sect. 4).
According to the standard model (e.g., Zarka 1998),
S-bursts are generated on the active magnetic lines, which are
activated by the Io satellite ( 1). The
frequency f of each component of the emitted band is approximately
equal to the local electron cyclotron frequency
at the
point of the active line from which it was emitted. Hence, the
decametric sources are localized in the subpolar magnetosphere, at
altitudes
,
where
km is Jupiter's
equatorial radius. Io stimulates emission with some time delay.
Accordingly, during this delay Io's orbital longitude increases on
the lead angle
in the frame of the Jovian
magnetic field.
Usually, we found from 1 to 3 S-trains or S-bands at different frequencies simultaneously in a dynamic spectrum of DAM ( 2). If there are arc emissions from different active magnetic tubes at various longitudes, any correlation between radio fluxes in microstructures of adjacent S-trains is not expected.
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Figure 1: The scheme of S-burst source localization and its radiation pattern according to the standard model (not to scale). |
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Figure 2:
The sample of S-bands at
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However, the standing Alfvén wave can make quasi-periodical regions of maximal parallel electric currents and maximal transversal magnetic disturbances along one magnetic tube. Such regions coincide with wave nodes, where the transversal plasma motion is minimal, but the magnetic deflection from undisturbed direction is maximal. Sometimes we observe S-burst emission, mainly from these regions, as S-band illusions, if the Alfvén wave sufficiently alters the direction of narrow radio beams in the same regions ( 3).
Such alteration is possible in terms of electron-cyclotron maser
instability, which is considered the most promising explanation of
S-bursts (Zarka 1998; Hess et al. 2007b). A
resonant interaction between a radio wave and a spiralling electron
occurs when, in the frame where the electron's center of gyration is
stationary, the cyclic frequency of the wave (
)
is equal to
the gyrofrequency
,
where
is the Lorentz factor (v and c are
the electron and light velocities, respectively). A resonant
interaction occurs when the Doppler condition is satisfied,
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Figure 3: Modulation of S-emission flux by the radiation pattern swinging in the nodes of standing Alfvén wave. The maximal curves (not to scale) of the active magnetic line and the directions of connected radio beams are shown with half-period time interval (solid and dashed). Periodical orientation of radio beams to the Earth from several nodes forms the S-bands in dynamic spectrum at corresponding electron cyclotron frequencies (squares). Note the anti-correlation between radio beam directions or squares in adjacent S-bands. |
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As
,
the approximation
for
in Eq. (1) gives the equation of resonant curve in the
plot,
The parallel electric field of the Alfvén wave accelerates
electrons in the radio source. Hence, the electron distribution is
shifted along the
axis with
.
As a result, the
variation of radio beam direction is
,
where
is the shift of the center of optimal
resonant curve. It is found, experimentally, that the cone mantle
thickness of S-burst radiation pattern is
,
especially in Io-B radio storms (Ellis 1982;
Ryabov 1994; Zarka 1998). Presumably, such
a narrow radio beam can be a result of some compact detail of
unknown electron pattern on the
plot, e.g., a
narrow horseshoe feature or an electron beam (Fig. 3 in Hess et al.
2007b). Therefore, the radio beam could be turned
away from the Earth if
rad. This
estimation
corresponds to the variation of electron energy of
keV, where
keV and
are the mean parallel energy and corresponding
parallel velocity of electrons emitting S-bursts at f=20 to 25 MHz
(Fig. 3d in Hess et al. 2007a). Sufficient electric
potential jumps of 0.7 to 3 keV are found experimentally from the
analysis of the frequency drift rate of individual S-bursts (Fig. 6 in Hess et al. 2007a). These jumps are localized at quasi-stable altitudes, and they could be associated with nodes of the standing Alfvén wave.
Alternative models with strong S-burst refraction (
in
the radio source; Boev et al. 1993; Zaitsev et al.
1986) predict that narrow radio beam is
quasi-perpendicular to the local magnetic field. If the amplitude of
magnetic deflection exceeds the cone mantle thickness of S-burst
radiation pattern, the Alfvén wave can turn the radio beam away
from the Earth as is shown in 3. It is
possible with
,
where
mT is the magnetic induction at
MHz, and
mT is the sufficient amplitude of the Alfvén wave. Unfortunately, the amplitude of magnetic pulsations in the regions of DAM sources is not measured yet.
Therefore, the cyclotron maser instability and alternative mechanisms assume the control of S-burst visibility by the standing Alfvén wave. The regions of easy observation of S-bursts coincide with the standing wave nodes. As the nodes are positioned quasi-periodically in space, corresponding S-trains must be quasi-periodical with frequency in dynamic spectrum. It is important that the parallel electric currents and transversal magnetic disturbances have opposite directions in adjacent nodes. Correspondingly, the radio beams must deviate in opposite directions, independent of emission mechanism. Such modulation in the standing wave model leads to the anti-correlation of radio fluxes in adjacent S-trains or to the correlation with next (after adjacent) S-band ( 3). This correlation pattern is a good test for the model.
To verify this test, we used the record of DAM spectral intensity at fixed frequencies in the centers of S-bands registered during 59.148 s with resolution of 6 ms at August 2, 2002, 9:30 UT (see part of these observations in 2).
The null hypothesis (no correlation) may be verified with the
standard transformation of correlation coefficient
into
the value
,
which
has the normal distribution (e.g., Bendat & Piersol
1986). If no correlation exists between spectral
intensity in two frequency channels, the average of w distribution
is zero, and its dispersion is
,
where
N=9983 is the number of measurements in one channel. The
probability (
)
of deviation
is well
known for the normal distribution:
.
Hence, the confidence interval with
-significance is
,
where
.
In our
case (
and
)
we have
and
.
Hence,
the confidence interval of the null hypothesis can be approximated
as
.
Its borders (
0.038) are calculated with
and
.
Correspondingly, the null hypothesis predicts
that
,
with the probability of
.
However, our experimental estimations of
show
systematical deflections from the null prediction ( 4). Moreover, there are significant spikes (arrowed) far
out the confidence interval. Therefore, the null hypothesis is not
valid, and some correlation pattern is present.
It is important that the found correlation details agree with the
prediction of the standing wave model. There is a slight, but
significant anti-correlation between adjacent S-bands up to
0.01 at f=20.5 and 23.1 MHz with the time
shift of
s; and
0.01 at
f=23.1 and 25.25 MHz with
s. However, there is a
positive correlation up to
0.01 between the
extreme S-bands (20.5 and 25.25 MHz) with
s.
The mentioned time shift
of maximal correlation
corresponds to the drift rate of
MHz/s. Obviously this is the drift rate of S-bursts that typically equals
from -10 to -30 MHz/s (Hess et al. 2007a). Apparently,
there is radio flux modulation along space trajectories of S-sources.
Figure 5 demonstrates other examples of anti-correlation of fine structure in adjacent S-bands at August 9, 2002. Hence, the model prediction is formally confirmed.
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Figure 4:
Correlation coefficient (
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Apparently, the low level of anti-correlation in Figs. 4 and 5 is a result of the following interference factors.
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Figure 5: Other examples of anti-correlation (arrowed) of microstructure in adjacent S-bands at August 9, 2002, 11:00 UT ( a)) and 11:15 UT ( b)). The dynamic spectrum was recorded with the UTR-2 radio telescope with an observation campaign within the frame of the INTAS project 03-51-5727. Marked like 4. |
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The average frequencies of S-bands show variations with the time scale of a few minutes (Boudjada et al. 1995). From the standing wave model it follows that the drift in frequency of the S-band reflects the spatial motion of the node (see Sect. 2). As the node is part of a standing wave, its motion must be in coordination with displacements of other nodes. Hence, the frequency variations of S-bands must be correlated.
Moreover, the simple relation between frequency displacements of two
S-bands can be predicted. We consider the short (i.e.,
quasi-homogenous) part of an Alfvénic resonator with X length
that is equal to N Alfvén semi-wavelengths along the active
magnetic line, above the low border of the Jovian ionosphere. Then,
the distance between adjacent nodes is d=X/N; and the coordinate
of the node is
x=(n+1/2) X/N, where n=0, 1, 2 is the node's
number. The 1/2-addition takes into account the boundary condition
of zero electrical current at the low border of ionosphere, which is
between the wave nodes. If the resonator length is variable, their
variations are
and
.
Accordingly, the variation ratio of these parameters is
.
In case of
and
(where
is the Jovian radius), the linear
approximation could be used to change over to the frequency scale:
and
.
Therefore, the variation of frequency
interval between adjacent S-bands
must be
connected with the variation of S-band frequency (
):
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Figure 6: Macrostructure of S-bands in dynamic spectrum of March 30, 2000 (UTR-2; INTAS 03-51-5727). |
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Figure 7:
The scheme of maximal intensity in S-bands from
6 ( a)) and the corresponding relation between the S-band
distance ( |
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To verify this prediction, we used the dynamic spectrum of DAM spectral intensity (F) with two S-bands, which was recorded with the resolution of 0.1 s March 30, 2000, 12:01-14 UT ( 6). We calculated the average gradient
in the band of 0.56 MHz (20 pixels) around each pixel
of the spectrum. At the same time,we excluded the intensity bursts
at fixed frequencies as a terrestrial interference. As a result, the
scheme of maximal S-burst intensity in S-bands is constructed
( 7).
The correlation coefficient between frequencies of different S-bands
in 7a is
.
Hence, the first
prediction on correlation between frequency shifts of different
S-bands is confirmed.
The second prediction Eq. (3) is verified with the
diagram ( 7b), which is constructed from
7a data. The correlation coefficient between
and f is
.
The regression is found with
the method of least-squares for 185 estimations:
The variability of S-band frequency could be interpreted in terms of a variable length of ionospheric Alfvén resonator near Jupiter. As it is near the Earth, this resonator could operate in a vertical direction with shear Alfvén waves, which are trapped between the ionosphere bottom and the peak of the Alfvén phase speed (Su et al. 2006).
The altitude of Alfvén speed maximum is controlled by the plasma mass density in the resonator. However, the parallel electric fields deplete the plasma density in flux tubes by about an order of magnitude. Such field-aligned cavities are found in the Io torus (Russel et al. 2005; Chust et al. 2005) and predicted theoretically in the connected regions of DAM sources (Su et al. 2003). It is generally accepted to associate plasma cavities with DAM and its analogs on other planets (e.g., Zarka 1998). As S-bursts are stimulated by Io satellite (Zarka 1998), the S-source follows behind Io through various cavities in the low magnetosphere. Hence, the longitudinal variations in plasma density could modulate in time the length of the radio-active part of the Alfvén resonator, without physical variation of the length of the Alfven resonator. We receive S-bursts from various resonators one after another with different longitudes and lengths.
We calculate Alfvén speed (
)
at various altitudes along
the active magnetic field line to find its maximal value
numerically:
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Figure 8:
The calculated
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The border of the resonator or
at the altitude of
maximal
is calculated with Eqs. (5)-(7) for
various
and
with the VIP4 magnetic model (Connerney
1998) and a northern radio source. The result curves
are shown in 8. It is follows from 8 that f variations of S-bands (2-3 MHz in 7a) correspond to a variation of about a factor 10 in
or ![]()
in
or T. Such plasma caverns have
been found in the Io plasma torus (Russell et al.
2005) and in the terrestrial polar magnetosphere
(Zarka 1998).
Alfvénic oscillations in the radio source can modify the DAM radiation pattern ( 3). After averaging the standing wave period, the conical sheet of radiation is thickening near the wave nodes. However, the radiation pattern is practically not modified at the wave maxima. As a result, we can see S-bands in the dynamic spectrum. This S-band pattern evolves with the motions of the observer and the active magnetic line.
To model such evolution for a certain time interval, we tracked the
active magnetic line numerically from the bottom of the Jovian
ionosphere. We calculated the angle
between the local
magnetic field and the Earth direction at various points on the
line. Ideally, we receive S-emission if
,
where
and
are the borders of undisturbed S-radiation pattern. As the radiation
pattern is thickening by the Alfvén standing wave, the condition
of observability is
.
The harmonic (simplest) disturbance of active line is
assumed. Hence, the Alfvén widening of the radiation pattern is
suggested in the form of
,
where
is the amplitude of
;
x is the distance from the ionosphere bottom along the active line;
is the Alfvén wavelength.
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Figure 9:
The sample model of S-band evolution in the dynamic
spectrum of March 30, 2000, 12:01 to 12:20 UT (
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After calculations for different consecutive time moments with the VIP4 model (Connerney 1998), we find the sample distribution of S-emission in the dynamic spectrum ( 9). In 9, broadband S-storm transforms into several S-bands. Such transformations were indeed described with real S-storm spectra (Riihimaa 1991).
There are theoretical and experimental arguments for a modulation of S-emission by standing Alfvén waves in the regions of Jovian decametric radio sources. One effect of such modulation is the phenomenon of S-bands in the dynamic spectra of DAM. We argue that S-bands are generated around nodes of a standing Alfvén wave. To test this hypothesis, we derive the following predictions for empirical verification.
Acknowledgements
We used the dynamical spectra of S-storms, which have been recorded by an observation compaign within the frame of the INTAS project 03-51-5727 (A. Lecacheux, H. O. Rucker, A. A. Konovalenko and Yu. Tokarev) with the UTR-2 radio telescope. We thank Dr. V. E. Shaposhnikov for fruitful discussions.