A&A 461, 1115-1119 (2007)
DOI: 10.1051/0004-6361:20065754
C. Li1 - Y. H. Tang1 - Y. Dai1 - W. G. Zong2 - C. Fang1
1 - Department of Astronomy, Nanjing University, Nanjing 210093, PR
China
2 -
National Center for Space Weather Monitoring and Warning,
Meteorological Administration, Beijing 100081, PR China
Received 2 June 2006 / Accepted 9 August 2006
Abstract
Aims. In large gradual solar energetic particle (SEP) events, especially the ground-level enhancement (GLE) events, where and how energetic particles are accelerated is still a problem.
Methods. By using imaging data from TRACE, Yohkoh/HXT, SOHO/MDI and SOHO/EIT, along with the data from the GOES, Apatity NM, and SOHO/LASCO CME catalog, the evolution of the X5.7 two-ribbon flare and the associated SEP event on 14 July 2000 are studied.
Results. It is found that the magnetic reconnection in this event consists of two parts, and the induced electric field
is temporally correlated with the evolution of hard X-ray and
-ray emission. In particular, the first hard X-ray and
-ray emission peak occurred at 10:22 UT, corresponding to the magnetic reconnection in the western part of the flare ribbons and the maximum
of
9.5 V/cm; the second emission peak at 10:27 UT, corresponding to the eastern part and the maximum
of
13.0 V/cm. We also analyze the SEP injection profiles as functions of time and CME-height, and find two-component injection which may result from different acceleration mechanisms.
Conclusions. A reasonable conclusion is that reconnection electric field makes a crucial contribution to the acceleration of relativistic particles and the impulsive component of the large gradual SEP event, while CME-driven shocks play a dominant role in the gradual component.
Key words: acceleration of particles - Sun: particle emission - Sun: flares - Sun: coronal mass ejections (CMEs)
In 1992, Kallenrode et al. found the most common energetic proton
events are those exhibiting both an impulsive phase and shock
emission, the "pure gradual'' events are relatively rare. They
suggest that between these two classes there should be "mixed'' or
"hybrid'' events with both impulsive and shock acceleration.
Cliver et al. (1995) then expanded the two-type
classification to include the "mixed'' events, in which the SEP
event contains a mixture of flare-accelerated and
CME/shock-accelerated particles. Recent observations and studies
provide more and more evidence of the existence of mixed SEP
events. Cohen et al. (1999) found that the charge states
of 12 elements with energies of 12-60 MeV/nucl and source
temperatures of (3-6)
106 K, are significantly
higher than at lower energies. It rules out acceleration out of
the ambient material (Kallenrode 2003). In
addition, Cane et al. (2003) find that in some intense
SEP events, the time-intensity profiles exhibit two peaks: the
earlier one with a high Fe/O ratio, the later one a low Fe/O
ratio. A much simpler interpretation is that the earlier one is
flare-related and the later one is CME-driven shock related. Dai
et al. (2005) find that some large gradual SEP events have
an initial impulsive component, which may stem from flare
acceleration. Shocks could also add substantial protons and
contribute to the gradual component (Cane et al. 1986).
And a recent simulation of mixed particle acceleration by Li &
Zank (2005) indicated that the SEP time-intensity profile
has an initial rapid increase followed by a plateau similar to a
pure shock case.
An outstanding solar event occurred on 14 July 2000, "Bastille Day'', comprising an X-class flare, a fast halo CME, and a large particle intensity enhancement in interplanetary space. It offers an excellent opportunity to extend our knowledge about the acceleration and transport process of solar energetic particles. The GOES X5.7/3B two-ribbon flare, which occurred in the NOAA region 9077 (N22W07) at 10:03 UT, has been thoroughly studied by Aschwanden & Alexander (2001), Fletcher & Hudson (2001), and Masuda et al. (2001). Their studies mainly focus on the generation of EUV and hard X-ray sources and on the corresponding magnetic structure. One of their important results is that flare ribbons map the footprints of magnetic field lines newly linked by reconnection, along which nonthermal particles bombard the lower atmosphere and lose their energy.
In this paper, we go on to use high-cadence observations from the Transition Region and Coronal Explorer (TRACE), along with the longitudinal magnetic field from the Michelson Doppler Imager (MDI) on board SOHO, to evaluate the magnetic reconnection electric field. This enables us to estimate a charged particle's energy gain in the active region. Because this event was associated with a fast halo CME, we also analyzed the SEP injection profiles as the functions of time and the CME-height. We then discuss the roles of flare and CME-driven shock in producing energetic particles. This paper is organized as follows: in Sect. 2, we analyze the reconnection electric field, comparing it with hard X-ray emission, and investigate the SEP injection profiles. Section 3 is dedicated to discussions, and conclusions are drawn in Sect. 4.
We used the high-cadence (
1 min) 171
TRACE
observations covering the time interval of 10:11 UT-10:59 UT to
measure the ribbon separation of the flare. To enhance the spatial
structure of the flare ribbons, we applied a high-pass filter by
subtracting a smoothed image (smoothed by
pixels) from
the original images. Figure 1 shows six of these images of the
active region at different times. It is clear that the separation
of the flare ribbons occurred first in the western part and then
in the eastern part.
To overlay the positions of the flare ribbons on the magnetogram,
we first resized the TRACE white light image (at 09:35:16 UT) to
the same pixel size as an MDI continuum image (at 09:35:31 UT),
and cross-correlated the two images. This procedure returns a
value for the offset between the TRACE and MDI images. With this
offset correction, the positions of the flare ribbons for each
TRACE 171
image can be traced and overlaid on the MDI
magnetogram. Since the time interval we studied is
50 min, the solar rotation must be taken into account. We also
reconstructed hard X-ray images (M2 channel) made during the two
peaks of the flare emission (10:22:45-10:23:10 UT and 10:26:58-10:27:04 UT), and overlaid them on the MDI magnetogram. Figure 2 shows the positions of EUV ribbons and hard X-ray sources
overlaid on the MDI magnetogram.
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Figure 1:
High-pass filtered TRACE
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Figure 2: Positions of the EUV ribbons and hard X-ray sources at the two peaks of flare emission (blue: 10:22:45-10:23:10 UT and green: 10:26:58-10:27:04 UT) overlaid on the magnetogram. Different color lines indicate the EUV ribbons at different times, and a white background indicates positive longitudinal magnetic field, and black negative. |
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As Fig. 1 shows, the eruption of the flare is divided into two
stages. The first eruption occurred in the western part of the
flare ribbons between 10:11 UT and 10:24 UT, and then it triggered
the second eruption at the eastern part after 10:24 UT. This
indicates that the reconnection current sheet should consist of
two parts, corresponding to the evolution of the two parts of the
flare ribbons. Comparing the electric field
inferred
from the two parts with flare nonthermal emission at hard X-ray,
we find good temporal correlation between them, as shown in Fig. 3. In particular, the first hard X-ray emission peaks at 10:22 UT,
corresponding to the magnetic reconnection in the western part of
the flare ribbons and the maximum
of
9.5 V/cm and
the second one occurred at 10:27 UT, corresponding to the magnetic
reconnection in the eastern part and the maximum
of
13.0 V/cm. Two
-ray emission peaks were also
reported at 10:22 UT and 10:27 UT (Share et al. 2001).
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Figure 3:
Reconnection electric field
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From Fig. 2, we can also find that the hard X-ray sources, in
which energetic particles precipitated along magnetic field lines
newly linked by reconnection, are just located at the area where
the flare ribbons have the most rapid separation. The good
temporal and spatial correlation indicates a physical link between
magnetic reconnection and energy release in flares, and also
suggests that reconnection electric field
plays an
important role in accelerating nonthermal particles.
Assuming that energetic particles travel along the IMF lines at a
speed of
with no scattering, we usually estimate the
proton solar release time relative to CME white light observation,
by subtracting
from observed time at 1 AU, where
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Figure 4:
SEP injection profiles of the 2000 July 14 GLE. The GOES
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The estimate of solar release times in Eq. (1) to determine the
SEP injection profiles is justified only when the SEP mean free
path
AU. However, a range of
AU for SEPs of all energies was found by Palmer (1982)
from SEP intensity-time and anisotropy-time measurements, so it is
necessary to consider the effect of interplanetary scattering on
the injection profiles of Fig. 4. Using the transport equation
(Kallenrode et al. 1992) and a Reid-Axford
injection profile (Reid 1964), we estimate the
displacements in the plot of Fig. 4 that is delayed from the true
injection profiles. The Reid-Axford injection profile is shown to be:
Then, the peaks of SCR,
,
and
injection
profiles should be respectively displaced by
20,
145, and
78 min. Considering these displacements, we
find that the peaks of the injection profiles of SEPs occurs
before 10:31 UT
5 min when the CME height reaches
,
which is very close to the Sun.
This estimation is consistent with the result of Bieber et al.
(2002), who obtained the best fit to the relativistic
protons observed on Bastille Day and found that the injection
function of particles released near the Sun has a peak at 10:26:50 UT with an FWHM (full width half maximum) of 5 min. Please
note that this injection function has a good correlation with the
hard X-ray,
-ray emission and the inferred reconnection
electric field during 10:22-10:33 UT as Fig. 3 shows.
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Figure 5:
Temporal profiles of the soft X-ray and the energetic
proton flux of the 2000 July 14 event. The upper panel shows the 1-8 |
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To fully comprehend the SEP event, proton intensity-time profiles during two days are plotted in Fig. 5, which shows that the injection profiles have two components or phases, which can be named "impulsive component'' and "gradual component''. The impulsive component lasts from 10:26 UT to 15:00 UT on 14 July 2000 only a few hours, followed by the gradual one lasting until the interplanetary shock reached 1 AU at 14:16 UT on 15 July 2000, far beyond the flare duration. It is clearly shown that the gradual component of relative lower energetic protons (P4 and P5) appears to result from interplanetary shock acceleration, which however plays a minor role in accelerating somewhat higher energetic protons (P7).
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Figure 6:
Sketch of the reconnection current sheet. B0 is the
main (reconnecting) magnetic field component, |
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On the condition described above, protons could be effectively and
rapidly accelerated to a very high energy in the RCS. The inferred
GLE onset time also coincides with the hard X-ray,
-ray
emission and the inferred reconnection electric field. It suggests
that the reconnection electric field perhaps makes a crucial
contribution to the acceleration of SCR particles and the
impulsive component of the large gradual SEP event.
An argument against flare acceleration is that the flare did not occur in the well-connected region. However, Klein et al. (2001) find a clear frequency dispersion of the western radio source during the time around the GLE onset, indicating a coronal magnetic structure that bends westward with decreasing frequencies (Fig. 7, left panel). This can be interpreted as a coronal magnetic channel that links to the well-connected region. The large-scale solar surface disturbance observed between 10:12 UT-10:48 UT is also shown in the right panel Fig. 7. It offers a particle transport path from the poor-connected region (flare site) to the well-connected region and may correspond to a field-opening process.
Another argument against flare acceleration in large gradual
events is that reconnection occurs in closed field lines beneath
CME and that the accelerated particles are trapped so they cannot
escape (Reames 2002). However, according to the time
profiles of hard X-ray and
-ray, as well as energetic
particles (including proton, 3He, and 4He) from the FY-2
satellite, Tang & Dai (2003) found that the 2000 July 14
SEP event should be a mixed one, in which both flare and
CME-driven shock accelerated particles exist. Continuous radio
bursts from a few GHz to <1 MHz were also reported (Cane et al.
2002; Klein et al. 2001). It implies that open
field lines extending from within 0.5 solar radii into
interplanetary space must exist, so flare-accelerated particles
can escape along the open field lines into interplanetary space.
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Figure 7: Left panel (Klein et al. 2001Fig. 5): frequency dispersion of the radio source near their maximum brightness at 410, 327, 237, and 164 MHz. Right panel: the large-scale solar disk disturbance on 14 July 2000. The three images show EIT images at 10:12, 10:36, and 10:48 UT with a pre-event image subtracted from them. Arrow indicates the bright edge of the solar disturbance. |
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Acknowledgements
We are very grateful to J. Qiu and the anonymous referee, whose constructive comments have greatly improved this paper. We thank the SOHO/MDI, SOHO/EIT, SOHO/LASCO CME catalog, Yohkoh/HXT, and TRACE teams for providing the observational data. SOHO is a project of international cooperation between ESA and NASA. Apatity neutron monitor data is kindly provided by the Polar Geophysical Institute of the Russian Academy of Sciences (PGI, Apatity). This work was supported by NKBRSF of China G2000078404 and NSFC key projects Nos. 10333040 and 10221001.