Z. Ning1,2 - M. D. Ding 1 - H. A. Wu 2 - F. Y. Xu 2 - X. Meng 2
Department of Astronomy, Nanjing University, Nanjing 210093, PR China - Purple Mountain Observatory, Nanjing 210093, PR China
Received 3 September 2004 / Accepted 8 March 2005
Abstract
We analyse 22 continuous microwave reverse slope (RS) type III and 21 microwave pulsation groups observed by the Purple
Mountain Observatory (PMO) spectrometer over the frequency range of 4.5-7.5 GHz from 1999-2003. The
RS type III groups have an average of 12 bursts per group, a mean duration of 0.1-2 s around 6 GHz, a mean quasi-period
of
s and a mean drift rate of 7.0 GHz s-1. The shortest quasi-period is measurable down to 0.05 s thanks to the high time
resolution of this instrument. The microwave pulsation groups have an average of 22 events per group, a mean duration of 3-4 s
and a mean quasi-period of
s. The RS type III bursts have the same quasi-period as the upward type III bursts
documented before. We discuss two possible origins of the quasi-periodicity of type III bursts. One is
the quasi-periodic process in magnetic reconnection at the same site, and the other is spatially unresolved stochastic processes in
solar flares.
Key words: Sun: radio radiation
It is widely accepted that the energy released in solar activity comes from the magnetic field.
Magnetic reconnection is thought to be the basic process of energy dissipation.
More and more observations have shown evidence to support this viewpoint.
Masuda et al. (1994) first observed a loop-top hard X-ray source in a compact flare and interpreted it as
evidence for magnetic reconnection above the loop top. Sui et al. (2003) found that the altitude distribution
of temperature in both loop-top
and corona hard X-ray sources indicates the formation of a large-scale current sheet in the solar flare
that occurred on 2002 April 15.
Yokoyama & Shibita (1995) observed X-ray jets and H
surges that are thought to be produced by reconnection.
Innes et al. (1997a) showed that
the transition region explosive events are consistent with bi-directional jets produced by magnetic reconnection. They
presented the time variation and spatial structure of the magnetic reconnection process for the first time. Recently, Ning et al. (2004)
reported that transition region explosive events have a 3-5 min quasi-period, which suggests that the magnetic reconnection
repeatedly takes place at the same site with a quasi-periodicity
on the quiet Sun. Sui et al. (2003) found observational evidence of continuous reconnection at a flare loop top
because both loop-top and corona hard X-ray sources smoothly move upward with various
speeds. Liu et al. (2004) showed that the footpoint
and loop-top hard X-ray sources gradually move
outside and upward respectively during a flare that occurred on 2003 November 3, which also indicates continuous reconnection in a flare.
Therefore, it is an interesting question as to whether there is a quasi-periodicity in the continuous reconnection in solar
active regions, and if there is, how long it lasts.
In the classical reconnection model for solar flares (e.g. Sturrock 1964), the released magnetic energy is quickly
converted to thermal and kinetic energy of plasma and
particles, which is reflected from the emission at various wave-bands. Aschwanden et al. (1995) and Ning et al. (2000) showed that
the solar type III burst pairs, both an upward-propagating type III burst (with a negative frequency-time drift rate,
)
and
a downward-propagating reverse slope (RS) type III burst (with a positive frequency-time drift rate,
), are consistent with
bi-directional electron beams produced by magnetic reconnection in flares. The quasi-periodicity of type III bursts could be helpful to
understand the energy dissipation process, especially the quasi-periodicity of magnetic reconnection in the active region. Aschwanden et al.
(1994) has statistically studied the quasi-periodicity of type III bursts in order to clarify the coherent-phase or random-phase acceleration
of electron beams in solar flares. They found a total of 260 continuous type III groups observed by Ikarus (Zurich) in the frequency range
of 100-500 MHz, during 359 flares in the years 1980-1983. On average, there are
bursts per group, with a mean
duration of
s per group, and a mean quasi-period of
s. They mainly studied the upward type III bursts and their sub-classes,
type J and type U bursts in the metric wavelength.
They concluded that the electron beams are accelerated upward by coherent-phase reconnection and with a quasi-period of 2.0 s during solar
flares. It is an interesting question as to whether the downward electron beams, which generally produce
microwave bursts (frequency > 1 GHz), especially RS type III bursts,
have a quasi-period as well. The quasi-period of RS type III bursts, which appear preferentially above 500 MHz (Aschwanden et al. 1997),
is still not well known. In this study, we attempt to determine the quasi-period of RS type III
bursts around 6 GHz.
Mangeney & Pick (1989) and Zhao et al. (1991) previously found that the quasi-periodicity ranges between 1 and 6 s in the type III bursts using Fourier transformation. They also concluded that this kind of quasi-periodicity occurs because of the quasi-periodic process in solar flares. Contrary to these investigations, Isliker (1996), who studied stochastic processes in flares, suggested that the interpretation of these empirical results not as simple as these authors suggest. It is possible that the quasi-periodic behaviour of type III bursts can be the signature of the stochastic process in solar flares. Isliker & Benz (1994) did not find any hint of quasi-periodic behaviour for type III and narrow-band spike events. We will discuss these two kinds of interpretation for RS type III burst groups in this paper.
Table 1: The data set used in this paper obtained at PMO (China) in 1999-2003.
The data described here were obtained with the 4.5-7.5 GHz radio spectrometer of the Purple Mountain Observatory (PMO) in China.
It has 300 frequency channels of 10 MHz bandwidth each and a time resolution of 5 ms. This spectrometer has obtained much valuable data
during the last solar maximum cycle.
It can detect more than 150 active events each year. Its daily working time is between 1:00-9:00 UT.
Description of this instrument can be found in Xu et al. (2003). According to our observations,
the main form of radio emission at this band is microwave type IV burst, which is the counterpart of
decimetric (DCIM) bursts around 6 GHz.
These type IV bursts are generally produced by solar flares that can also be detected in H
or
X-ray wavelengths. We observed fewer microwave type III bursts than type IV bursts.
We analyze a total of 22 groups of continuous microwave type III bursts and 21 groups of
microwave pulsations observed by the PMO spectrometer during 40 solar flares in the years 1999-2003.
Table 1 presents all
the events studied in this paper. We classify the events into three types, RS-III, Blips and Pulsation,
based on the 1-3 GHz solar radio catalogue (Isliker & Benz 1994).
The corresponding X-Ray flares are presented
if the bursts take place during the flare. All of the RS type III group or blips appear in the impulsive phase of X-ray
flares, which is consistent with statistical studies in the metric wavelength (e.g. Kane 1974).
According to the Solar Geophysical Data (SGD), one RS type III on 2002 April 14 and two pulsation
groups on 1999 September 11 and December 16 occurred without any flares detected in H
and X-ray. Possibly,
the flares were too faint
to be detected by present instruments. We also note that pulsations took place 20 min later in the B8.3 flare of 2003 June 21.
We identify the individual RS type III bursts based on the criterion used by Isliker & Benz (1994) 1n the 1-3 GHz band. They showed that type III bursts have a duration of the order of 0.1-1 s. The narrow band (<100 MHz) type III bursts are called blips. We first identify the individual RS type III burst dependence in a mean duration of 0.1-2 s around 6 GHz, which is slightly longer than that at 1-3 GHz (Isliker & Benz 1994). Secondly, RS type III groups are identified by visual inspection of the broad-band dynamic spectra in the frequency range of 4.5-7.5 GHz and by the measurement of the frequency-time drift rate. The frequency drift rate of each individual RS type III burst is calculated over its bandwidth, and the mean value of all RS type III bursts in Table 1 is about 7.0 GHz s-1 (in the range of 2.5-13 GHz s-1), which is much faster than metric type III bursts (-100 kHz s-1). Furthermore, we identified microwave pulsation events, which generally exhibit a more regular flux amplitude, a higher frequency drifting rate and a mean duration of 3-4 s around 6 GHz.
The RS type III and pulsation peaks often overlap a gradual component. Thus these peaks have a higher value than the background
emission of the quiet sun. However, some peaks lie very near the noise level. As shown in Fig. 1, the burst peaks have to
be larger than 3 times the standard deviation (
)
of the noise, which is computed by the average profile in two windows
on either side of the radio bursts, for example, between time period 05:15-05:25 and 05:45-05:55
(top panel in Fig. 1),
(arbitrary units)
for the event on April 14 2002. Then,
we estimate the quasi-period P in RS type III and pulsation groups from the formula as follows (Aschwanden et al. 1994)
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Figure 1:
An example of RS blips (narrow-band type III bursts) on 2002 April 14, around 0536 UT observed by PMO, without any flare detected
by H |
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Figure 2:
A unique example has RS type III groups preceding microwave type V continuum for the flare of 1999 August 25.
26 individual RS type III bursts are identified by solid lines with a mean quasi-period of
|
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Figure 3 shows a sample of RS type III groups in the impulsive phase of microwave type IV bursts for an M2.2 flare on 2002 September 11. There are two RS type III groups each of four bursts. They have a quasi-period of 1.4 s and a mean drift rate of 7.0 GHz s-1. Figure 4 shows an example of an RS type III group in the decay phase of microwave type IV bursts for an M2.0 flare on 2000 April 8. Note that the bursts are still in the impulsive phase of the X-ray flare. There are in total 37 individual RS type III bursts with a quasi-period of 1.5 s and a mean drift rate of 15.0 GHz s-1. Figure 5 shows an RS type III group without any other microwave radio emission for a C5.3 flare on 1999 October 27. There are 5 RS type III bursts with a quasi-period of 1.0 s and a mean drift rate of 5.0 GHz s-1.
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Figure 3:
An example of two RS type III groups in the impulsive phase of microwave type IV bursts for the flare of 2002 September 11.
Two groups of four individual RS type III bursts each are identified by solid lines with a mean quasi-period of
|
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Figure 4:
An example of RS type III group in the decay phase of microwave type IV bursts for the flare of 2000 April 8.
37 individual RS type III bursts are identified by solid lines with a mean quasi-period of
|
| Open with DEXTER | |
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Figure 5:
An example of an RS type III group without any other microwave emission for the flare of 1999 October 27.
5 individual RS type III bursts take place and the last 3 identified by solid lines have a mean quasi-period of
|
| Open with DEXTER | |
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Figure 6:
An example of microwave pulsation group in the impulsive phase of microwave type IV bursts for the flare of 1999 December 16.
8 individual pulses occur and the last 6 identified by solid lines have a mean quasi-period of
|
| Open with DEXTER | |
The pulsation bursts have dynamic spectra almost without any frequency drift. This is because either the pulsation emission is simultaneously generated on a wide bandwidth or that the pulsation is a special sub-class of type III bursts with a very rapidly drifting rate which cannot be detected by the present instruments. We identify the pulsation groups as well as microwave type III burst groups. Isliker & Benz (1994) showed that the pulsation bursts have a shorter duration (less than 0.1 s) than type III bursts over the 1-3 GHz band. In our data, we identify a individual pulsation with a mean duration of 3-4 s, which is longer than RS type III bursts around 6 GHz. In Table 1, we present 21 groups of microwave pulsations. They have a mean quasi-period of 3.7 s (in the ranges of 1.2-6.0 s). Figure 6 shows an example of a pulsation group in the impulsive phase of microwave type IV bursts without any detected flare on 1999 December 16 (from SGD). It has in total 8 pulsations, the latter 6 having a quasi-period of 3.0 s. Figure 7 presents another pulsation group in the decay phase of microwave type IV bursts for an M1.5 flare on 2002 June 1. It has a 19 individual pulsations with a quasi-period of 3.0 s.
Although the physical reason for pulsations is still controversial, it is interesting that these pulsation groups show a quasi-period of 3.7 s, which is similar to the behaviour of RS type III groups around 6 GHz.
Figure 8 shows a special microwave type III group. Although the individual burst shows a very short life time (less than 0.05 s) at a fixed frequency, we still regard the group as type III bursts due to their frequency drift. There are more than 9 RS type III bursts (solid lines) preceding the upward type III bursts (dashed lines) during the flare on 2002 March 18. In order to determine the frequency drifting, the event is plotted in two different frequencies. Three drifting structures are plotted with dotted lines. RS type III bursts, as well as the following upward type III bursts, have a short mean quasi-period of up to 0.05 s. It is interesting that upward type III bursts follow the RS type III bursts in time. They could be the fine structures around 7 GHz, which correspond to the fast evolution process of plasma in the low corona. It is possible that the following upward type III bursts might be produced by the same electron beams that first generate RS type III bursts before the mirror effect. From our observations, it is difficult to support or rule out this possibility.
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Figure 7:
An example of a microwave pulsation group in the decay phase of microwave type IV bursts for the flare of 2002 June 1.
19 individual pulses are identified by solid lines with a mean quasi-period of
|
| Open with DEXTER | |
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Figure 8: A special microwave type III group mixed RS type III burst (solid lines) preceding the upward type III bursts (dashed lines) for the flare of 2002 March 18. Both RS and upward type III bursts have a very short quasi-period of 0.05 s. The 7.3 Ghz profile is overplotted after subtracting 700 flux units. One RS type III and two upward type III bursts are shown with dotted lines. The illustration is similar to Fig. 1. |
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We have presented the quasi-periodicity of RS type III bursts and pulsations around 6 GHz in this paper.
We found 22 continuous RS type III groups with an
average of 12 bursts per group, a mean duration of 0.1-2 s per bursts, a mean drifting rate of 7.0 GHz s-1
and a mean quasi-period of
s. As shown in Table 1, the longest quasi-period is 4.4 s and the shortest is 0.05 s. The 21 continuous microwave pulsation groups
have an average of 12 events per group, but a mean duration of 3-4 s per bursts, and a mean quasi-period of
s.
Here, the standard deviation is the average value of the standard deviation for the individual estimated quasi-period, which is computed
for each event in Table 1 with the formula noted earlier.
The issue of whether the energy release in a solar flare is triggered at a critical place and spreads randomly, or whether the energy disspation is controlled by a global condition with a quasi-period, is still controversial. As mentioned earlier, Mangeney & Pick (1989) and Zhao et al. (1991) searched for quasi-periodic behaviours in type III events by estimating the power-spectrum (using Fourier transforms), and they found that the typical quasi-periodicities are between 1 and 6 s. Later, Aschwanden et al. (1994) made a statistical study of a total of 260 continuous type III groups. They found upward type III bursts with a 2.0 s quasi-period. These authors concluded that the electron beams are accelerated upward through the corona by the coherent-phase instead of random-phase during flares. The present observations of RS type III bursts with a 2.0 s quasi-period indicate that the electron beams are accelerated downward with a quasi-period as well. This is reminiscent of magnetic reconnection to accelerate the electron beams upward and downward simultaneously with a quasi-period of 2.0 s in active regions.
On the other hand, there is also an argument that the solar flare processes could be random, without a quasi-period (e.g. Isliker 1996). What has been found in the observations and termed as "periodic'' or "almost periodic'' can as well be the signature of temporal correlations in a stochastic flare model. At present, it is very hard to establish whether the solar flare processes are random or quasi-periodic from the available observations.
In active regions, solar flares represent an explosive conversion of stored magnetic energy by reconnection into other forms. Sui et al. (2003) and Liu et al. (2004) found evidence of continuous reconnection in solar flares because of continuous outward motion of hard X-ray footpoint sources and upward motion of the loop top source. As mentioned earlier, both upward and RS continuous type III bursts have a quasi-period of 2.0 s in each group, which is also evidence that continuous reconnection accelerates the electron beams upward and downward by coherent-phase reconnection quasi-periodically. Although our radio observations provide no source images on the solar surface, both upward and RS type III bursts show similar dynamic spectra in each group. This phenomenon implies the possibility that continuous magnetic reconnection repeatedly takes place at the same site with a quasi-period of 2.0 s during solar flares. The dynamic spectra of type III bursts could be random instead of quasi-period when the electron beams are from various sites in active regions.
Nakajima et al. (1983) reported that the significant systematic differences between the times of peak intensities
of microwave, hard X-ray and
-ray line emissions
suggest that two kinds of acceleration take place successively and repeatedly within a few seconds. They found that
the bursts were composed of seven successive pulses on 1980 June 7 and four successive pulses on 1980 June 21, both with a quasi-periodicity
of
8 s. The authors suggest that two kinds of acceleration take place repeatedly during the impulsive bursts, in
order to interpret the quasi-periodicity of pulses and systematic differences between the peak times of microwave,
hard X-ray and
-ray line emissions. Both electrons and
ions are preferentially accelerated with a quasi-periodic of
8 s which is the same order as the
time interval between successive hard X-Ray pulses.
Transition region explosive events are one of the best-studied dynamic phenomena in quiet regions of the Sun
(e.g. Brueckner & Bartoe 1983; Dere et al. 1989; Dere 1994; Chae et al. 1998). They are
detected most frequently in transition region lines formed typically around 105 K, and rarely in lines formed below
K or above
K (e.g. Innes et al. 1997b). Explosive events are characterized
by broad line profiles with high velocity components of typically
100 km s-1, a special size of
2 arcsec
(
1500 km), and an average lifetime of
1 min. Since they were discovered, explosive events were considered to be a
manifestation of magnetic reconnection occurring in the quiet Sun (e.g. Porter & Dere 1991; Dere et al. 1991; Dere 1994).
Base on the joint observations with the Solar Ultraviolet Measurement
of Emitted Radiation (SUMER) spectrograph on board the Solar and Heliospheric Observatory (SOHO) and the Big Bear Solar
Observatory (BBSO), Chae et al. (1998) found that explosive events tend to occur above regions with weak and mixed
polarity magnetic flux on the photosphere, which further prove that explosive events represent magnetic
reconnection in the transition region of the quiet Sun. From the observations of SUMER, Innes et al. (1997a) showed that the
time variation and spatial structure of explosive events are consistent with the bi-directional plasma jets produced by
magnetic reconnection. Quite recently, Ning et al. (2004) reported that explosive events repeatedly take place at the
same site with a 3-5 min quasi-period, which suggests that magnetic reconnection has a quasi-period of 3-5 min in the transition
region of the quiet Sun.
The observations show that magnetic reconnection takes place repeatedly with a quasi-periodicity at the same site in both quiet and active regions. This property suggests that magnetic reconnection has a memory of its site. The following magnetic reconnection prefers to occur at the same site as the previous one. However, it is interesting to ask why the quasi-period is different in the transition region of the quiet Sun to that in the corona of the active region. This implies that the magnetic reconnection quasi-periodicity might be modulated by its surrounding environments. There are two types of oscillations (e.g. Lites et al. 1993) in the transition region of the quiet Sun, which are generally thought to be due to propagation of waves with a quasi-period of 3- or 5-min (e.g. Lou 1995; Banerjee et al. 2001). These waves might be able to modulate the quasi-period of magnetic reconnection there. Sakai & Washimi (1982) and Sakai et al. (1984) proposed a theoretical model of forced reconnection caused by fast magnetosonic waves. However, it is unclear what effect modulates continuous reconnection with a quasi-period of 2 s or 8 s in solar flares. The quasi-periodicity of continuous reconnection needs to be checked further by observations with spatial resolution in the future.
A quasi-periodicity in both upward and RS type III groups implies a quasi-periodicity in the acceleration mechanism if all these type III bursts originate from the same site. We cannot simply conclude that these electron beams for quasi-periodic type III bursts originate from the same site on the Sun, because the present observations provide poor spatial resolution. On the other hand, this interpretation relies on the model of a large scale current sheet, which is generally thought to be highly unstable and to be immediately fragmented into small current sheets. Emission from solar flares is fragmented in space and time, which favors the picture of multiple, small-scale (spatially unresolved) reconnections, called elementary bursts (e.g. LaRosa & Moore 1993; Ding et al. 2001). It is possible that the quasi-periodicity of type III events is an observational artifact due to the overlapping of a large number of elementary bursts from different sites.
Isliker (1996) has studied the stochastic flare model in detail. He reported that the stochastic models for solar flares are compatible with the past and present observational results with high temporal resolution. Isliker thought that the many isolated peaks in the power spectra form differentiated time series of type III events, which Mangeney & Pick (1989) considered to be indicative of quasi-periodic process, and suggested that they can be explained as the signature of a stochastic process. The empirical results of Aschwanden et al. (1994) can also be reproduced by the stochastic flare model. Isliker & Benz (1994) find no hint for quasi-periodic behaviours and for finite dimensions in the power-spectrum and correlation-dimension estimates for type III and narrow-band spikes events. Therefore, it is alsopossible that the present observations of RS type III groups are signatures of the stochastic processes around 6 GHz. In order to discriminate between the two possible scenarios, we need to perform observations with a much longer time interval and an improved time resolution.
Acknowledgements
We would like to thank the referee for many valuable comments, which led to an improvement of the paper. This work was also supported by NKBRSF under grant G20000784, by NSFC under grant 10025315, 10221001, 10333030, 10279025 and 10333040, a grant form TRAPOYT, a JIANG-SUN-SHENG (2004) postdoctoral fund 0201003401 and a postdoctoral grant 0201003005.