A&A 494, 263-268 (2009)
DOI: 10.1051/0004-6361:200810662
G. Michalek
Astronomical Observatory of Jagiellonian University, Cracow, Poland
Received 23 July 2008 / Accepted 15 October 2008
Abstract
Aims. Here, we study the relationship between flares and CMEs.
Methods. For this purpose a statistical analysis of 578 flare-associated CMEs is presented. We considered two types of flare-associated CMEs: CMEs that follow and precede flare onset.
Results. We shown that both samples have quite different characteristics. The first type of CMEs tends to be decelerated (median acceleration = -5.0 m s-2), faster (median velocity = 519 km s-1), and physically related to flares (a correlation coefficient between the energy of the CME and the peak of the X-ray flare = 0.80). The CMEs preceding associated flares are mostly accelerated (median acceleration = 5.4 m s-2), slightly slower (median velocity = 487 km s-1), and poorly related to flares (a correlation coefficient between the energy of the CME and the peak of the X-ray flare = 0.12).
Conclusions. These two types of flare-associated CMEs demonstrate that magnetic reconnection, which influences the CME acceleration, could be significantly different in the two types of events.
Key words: Sun: coronal mass ejections (CMEs) - Sun: flares
The two most important energetic phenomena on the Sun: a flare,
which is a sudden flash of electromagnetic radiation, and a
coronal mass ejection (CME), which is an eruption of solar plasma
into interplanetary space. CMEs and flares originate in closed
magnetic fields and are different manifestations of the same
process which releases magnetic free energy. The first CME was
detected on December 14, 1971 by the white-light coronagraph on
board NASA's seventh Orbiting Solar Observatory (Tousey 1973).
From the early days of CME observations, it is well known that
CMEs are associated with flares and prominences (Munro et al. 1979). Kahler (1992) showed that
of CMEs are
associated with H-alpha flares. The CME association rate clearly
increases with the peak of X-ray intensity. The CME association
rate increases from
(M-class flares) to
(X-class
flares) (e.g. Yashiro et al. 2006). The spatial and
temporal relationship between flares and CMEs was also considered
in detail (Harrison 1987; Kahler et al. 1989; Harrison 1991; Hundhausen 1999; Moon et al. 2002; Yashiro et al. 2008). These studies demonstrated that CME onset typically
precedes the related X-ray flare onset by several minutes. The
LASCO coronagraphs and other instruments have been used to
understand the initial speed and acceleration profiles of CMEs.
Zhang et al. (2004) found a three-phase acceleration
profile. A slow rise over tens of minutes, followed by a rapid
acceleration of 100-500 m s-2 occurs in the height range 1.4
to 4.5
during the flare rising phase and a propagation
with constant or declining speed. Gosling et al. (1976)
and MacQueen & Fisher (1983) suggested that different mechanisms
could accelerate CMEs associated with prominences and flares. The
rapid acceleration of CMEs is strongly correlated with the rising
phase of the associated soft X-ray bursts (Zhang et al.
2004; Vrsnak et al. 2004). The flare-associated CMEs
are faster and decelerating, while the prominence-associated CMEs
are slower and accelerating in the LASCO FOV (St. Cyr et al. 1999). In a statistical analysis of 545 flare-associated
CMEs and 104 non-flare CMEs, Vrsnak et al.
(2005) found that both data sets have similar characteristics and
form one consistent group of CMEs.
All CMEs have to be accelerated as they lift off from the surface.
During the next phase of propagation a balance between propelling
and retarding forces determines the dynamics of the CMEs. Recent
studies demonstrate that the propelling force ceases at heights
below 4
(Chen & Krall 2003). So, in the LASCO FOV,
drag determines the acceleration of CMEs. This interpretation was
proved
by statistical analyses (Yashiro et al. 2004). Generally it is assumed
that fast CMEs (
km s-1) are decelerated and slow CMEs (
km s-1)
are accelerated by the drag force (Yashiro et al. 2004).
In the present study we consider statistical properties of the
flare-associated CMEs only. To perform a detailed study we separate these
events into
two groups: CMEs following and preceding the associated flares.
The paper is organized as follows: in Sect. 2, the data considered in the study is described. In Sect. 3, we perform a broad statistical analysis of the flare-associated CMEs. Discussion and conclusions are presented in Sect. 4.
We describe a procedure used to compile the list of events employed
in
the study. For our analysis we use two data sets - CMEs and flares.
A full description of CMEs in the range of 2-30 solar radii is
included in the SOHO/LASCO catalog. We considered all CMEs detected
from the beginning of 2000 until the end of 2004.
Next, using data from the geosynchronous operating environmental
satellites (GOES), associated flares observed in soft X-ray range
were determined. For this purpose we used the database from the
National Geophysical Data Center
(www.ngdc.noaa.gov/stp/SOLAR/ftpsolarflares.html). X-ray
observations provide an accurate detection of the start of solar
flares. For the associated flare onset times, durations, source
locations, moments of the peak flux and the peak fluxes were
obtained. The duration of X-ray flares is defined in this database
as when the current flux returns to 0.5 of the peak value. In
addition the data are not background subtracted and the durations
of the X-ray flares could be ambiguous. In order to associate
flares with CMEs we employed temporal and spatial criteria. Using
the height-time plots we determined onset times (,
from
quadratic fit) of CMEs. We assume that a given flare is related to
a given CME if it appears 100 min before or after
associated CMEs (a onset of an associated flare should be in a
time window
100 min with respect to
).
Additionally we required that the location of flares is in the
same quadrant of the Sun as the associated CMEs. Using our
criteria we found the 578 flare-associated CMEs during 2000-2004.
In our work we consider two samples of flare-associated CMEs:
those starting before (BF-CMEs) or after associated flares
(AF-CMEs). As we mentioned, the onset times of CMEs are determined
from back extrapolations of the height-time plots and are subject
to errors of up to several minutes. To accurately separate CMEs
into the two sets of events we excluded these pairs of CMEs and
flares which had almost the same onset times (in a time window
min). In this way we established a sample of the 439
flare-associated CMEs used for further considerations.
![]() |
Figure 1: The acceleration distribution of the all CMEs ( top panel), the AF-CMEs ( middle panel) and the BF-CMEs ( bottom panel). |
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Figure 1 shows the acceleration distributions
for all the considered CMEs (top panel), the AF-CMEs
(middle panel) and the BF-CMEs (bottom panel).
The average acceleration of the all CMEs is slightly negative
(
m s-2). This tendency is due to the CMEs
following the associated flares. These events are clearly
decelerated (
m s-2) and more populated than the
CMEs preceding the flares. On the other hand the CMEs that
precede the flares are obviously accelerated
(
m s-2). Generally it is assumed (Chen & Krall
2003; Yashiro et al. 2004) that in the LASCO FOV, the
dynamics of CMEs is determined by drag which depends on the
difference between velocities of CMEs and the interplanetary
medium. Before we drow any final conclusions about dynamics of the
flare-associated CMEs it is necessary to consider the kinematic
properties of the samples of CMEs.
![]() |
Figure 2: The velocity distributions of the AF-CMEs ( top panel) and the BF-CMEs ( bottom panel). |
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Figure 2 shows the velocity distributions of the
AF-CMEs and BF-CMEs. There are no significant differences
between velocities of the two samples of events.
The AF-CMEs seem to be slightly faster (
km s-1)
than the BF-CMEs (
km s-1). The difference is too
small to explain the acceleration behavior of both categories of
events by drag. On average both categories of flare-associated
CMEs are faster than the whole population of CMEs (Yashiro et al.
2004,
km s-1). According to the results presented
in Yashiro et al.'s paper both categories of CMEs should be
slightly decelerated.
![]() |
Figure 3: The scatter plots of the energy of CMEs versus the peak flux of X-ray flares of the AF-CMEs ( left panel) and BF-CMEs ( right panel). |
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Figure 4 shows the acceleration-velocity
relationships of the AF-CMEs and BF-CMEs.
Continuous lines represent linear fits to the data point. The
AF-CMEs show an anti-correlation of the acceleration and velocity
(the slope coefficient of a linear fit = -0.0172), consistent with that obtained by Yashiro et al.
(2004) and
Vrsnak et al. (2004). The second
sample of CMEs (the BF-CMEs) does not show a similar trend (the slope coefficient of a linear fit =
0.0012).
This behavior is inconsistent with the aerodynamic drag
interpretation.
![]() |
Figure 4: The acceleration-velocity relationships of the AF-CMEs and BF-CMEs. Continuous lines represent linear fits to the data points. In the right top corners there are coefficients describing the slope of the linear functions. |
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![]() |
Figure 5:
The acceleration distributions of the CMEs with the
velocities ranges within V<400 km s-1 (panels a), b)),
400 km s
![]() |
Open with DEXTER |
In our study we assumed that the flares and CMEs are physically
associated if both phenomena appear in the time window 100 min. Figure 6 shows the distribution of the difference time
(
)
between the onsets of CMEs and flares.
In the figure we show 578 events because we did not exclude, as in
the previous considerations, the associated events originating in
a time window
5 min. The distribution of
is almost symmetric and Gaussian. About 80
of the associated
phenomena have
lower than
30 min. We repeated
the same studies (the same plots) as in previous subsections but
choosing lower limits for
(
60 min,
30 min and
including events having almost the same onset times
5 min). We
obtained almost the same results (trends) as were presented in the
previous sections. We only observed that CMEs which were more
temporally related to the associated flares were slightly faster
(on average by about 50 km s-1 for CMEs that appeared in the time
window
30 min with respect to the associated flares). The
results presented in the previous subsections do not depend on
temporal linking between the flares and CMEs. Additionally, in
Fig. 7 the diofstributions X-ray fluxes of flares associated
with the two types of CMEs are presented. Both categories of CMEs
are associated with similar populations of X-ray flares.
![]() |
Figure 6:
The distribution of the difference times between the
onsets of CMEs and flares (
![]() |
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![]() |
Figure 7: The distribution of X-ray flares associated with the AF-CMEs ( top panel) and BF-CMEs ( bottom panel). |
Open with DEXTER |
Figure 8 shows the velocity-width
relationships of the AF-CMEs and BF-CMEs. There is a poor
correlation between these parameters for the AF-CMEs (0.44) and
the BF-CMEs (0.30). In the figures we also presented halo CMEs
(
)
but they were not included in the calculations of
the correlation coefficients and average widths. Both categories
of CMEs have similar average widths (
AF-CMEs width
,
and
BF-CMEs width
)
but in the case of the AF-CMEs we
observed many more halo CMEs.
In the present paper we considered the flare-associated CMEs
observed during 2000-2004. We separately studied the two samples
of CMEs: the CMEs following (AF-CMEs) and preceding (BF-CMEs) the
associated flares. The CMEs after the associated flares tend to be
decelerated (median
m s-2). This trend is independent
of the velocity of the CMEs (Figs. 4 and 5), even the slowest
events (V<400 km s-1) are mostly decelerated (median
m s-2). Such a behavior (except deceleration for the
slowest events) was also observed in previous works (Yashiro
et al. 2004; Vrsnak et al. 2005).
These events seem to be accelerated during the rising phase of
flares and in the LASCO FOV the speed is determined by the drag
force of the interplanetary medium. The AF-CMEs are slightly
faster then the BF-CMEs and they are strongly related to the
flares. The correlation coefficient between the energy of CMEs and
the peak of X-ray fluxes is 0.80. The correlation is so
significant because the AF-CMEs receive the total propelling
energy in the beginning phase of propagation (in the LASCO FOV).
The energy is transported by the upward-directed reconnection jets
which enhance and prolong the flux rope acceleration until the
associated X-ray flares are in the increasing phase of eruption
(Mouschovias & Poland 1978; Chen 1989; Vrsnak 1990; Cheng
et al. 2003). Probably in the case of the slowest events, the
reconnection does not generate such jets but only reduces the
magnetic tension and diminishes the erupting-flux rope
acceleration (e.g. Anzer & Pneuman 1982; Cheng & Krall 2003;
Lin et al. 2004). These events tend to be decelerated even if
they are slow (Fig. 5, top left panel).
![]() |
Figure 8: The velocity-width relationship of the AF-CMEs ( top panel) and BF-CMEs ( bottom panel). |
Open with DEXTER |
The BF-CMEs are significantly different. They tend to be accelerated in the LASCO FOV. This trend is independent of the velocities of the CMEs. Even the fastest (V>800 km s-1) CMEs also have the tendency to be accelerated. The BF-CMEs have a delayed propelling boost (due to the flare reconnection process) when the associated flares start in the later phase of propagation. In the case of these CMEs the flare boosting Lorentz force is delayed with respect to the onset of the CME. These events are slightly slower in comparison to the AF-CMEs (but slightly faster than the total population of CMEs) and they seem to be poorly related to the associated flares. The correlation coefficient between the CME energy and the peak of the X-ray flux is only 0.12. Probably these events have the similar ``flare hoop-force'' as the AF-CMEs but it is delayed (starts when the associated X-ray flares appear). The correlation between these parameters might be more significant if we could observe the CMEs behind the LASCO FOV until the propelling force ceases. The BF-CMEs are a specific type of event triggering X-ray flares (during propagation through the corona) which causes the ``second step'' acceleration of these events.
Considerations of the lower limits of
proved that these
trends (for both categories of CME) do not depend on a temporal
relation between the associated flares and CMEs.
X-ray observations
provide an accurate detection of the start of solar flares. The
situation is different in the case of the onset times of CMEs.
These times are received from back extrapolations of the
height-time plots to the surface of the Sun. The onset times of
CMEs are subject to errors for two reasons. First, the height-time
plots are obtained through subjective manual measurements from
LASCO coronagraphic images. So, the height-time plots strongly
depend on the quality (especially brightness) of a particular
event. Additionally, linear or quadratic fits used for the back
extrapolations give only the approximate onset times of CMEs. The
both kinds of errors are very difficult to estimate. To minimize
errors three precautions were taken. First, we considered a large
sample of events (to increase the statistics). To obtain the more
accurate onset times for the back extrapolations quadratic fits
were used. Additionally, we excluded associated events that
started almost at the same time (in the time window 5 min).
We studied the dynamics of CMEs in the 2-30
range. So, we
cannot exclude that the two categories of flare-associated CMEs
have different initiation mechanisms.
Acknowledgements
Work done by Grzegorz Michalek was supported by MNiSW through the grant N203 023 31/3055. In the paper we used data from the SOHO/LASCO catalog. This CME catalog is generated and maintained at the CDAW Data Center by NASA and The Catholic University of America in cooperation with the Naval Research Laboratory. SOHO is a project of international cooperation between ESA and NASA.