A&A 420, 719-728 (2004)
DOI: 10.1051/0004-6361:20034570
T. Fragos - E. Rantsiou - L. Vlahos
Department of Physics, Aristoteleion University of Thessaloniki, 541 24 Thessaloniki, Greece
Received 24 October 2003 / Accepted 4 February 2004
Abstract
A two-dimensional probabilistic Cellular Automaton is
used to model the appearance of active regions at the solar
surface. We assume that two main competing processes control the
magnetic field evolution at the solar surface (1) the magnetic
field is locally enhanced by the flux emergence and/or the
coalescence of emerged magnetic flux and (2) it is diminished by
flux cancellation or diffusion. The flux emergence follows a basic
percolation rule; it is more probable at the points were magnetic
flux already exists. The magnetic field is also enhanced when
magnetic fields of the same polarity collide. The flux
cancellation is due either to the gradual diffusion of the
magnetic field, when it is isolated, or to the partial release of
energy when opposite magnetic field lines collide. The
percolation model proposed in this article is capable of
reproducing the statistical properties of the evolving active
regions. The evolving simulated magnetograms, derived from our
model, are used to estimate the 3-D magnetic fields above the
photosphere using constant
force-free extrapolation
techniques. Based on the above analysis we are able to estimate a
variety of observed statistical characteristics, e.g. the size and
flux distribution of the magnetic fields at the solar surface, the
fractal dimension of the magnetic structures formed at the
photosphere, the energy release frequency distribution, the
waiting time distribution of the sporadic energy releases and the
statistical properties of the steep horizontal magnetic field
gradients in the extrapolated coronal magnetic field. Our main
conclusion is that the photospheric driver plays a crucial role in
the observed flare statistics, and the solar magnetograms, when
interpreted properly, carry important statistical information for
the solar coronal activity (coronal heating, flares, CME etc.).
Key words: Sun: activity - Sun: magnetic fields - Sun: flares - Sun: photosphere - plasmas
The most active phenomena above the solar surface are related to active regions. It is for these reasons that their study has attracted the attention of many observers and theorists in recent years. The main focus of current theoretical studies is on the question: How is the subphotospheric activity mapped onto the formation and subsequent evolution of active regions. Two interrelated questions are usually posed: (1) where are the magnetic fields formed; and (2) how are they manipulated by the convection zone?
The formation and evolution of large-scale magnetic flux tubes inside the convection zone is an important theoretical problem, which still remains open. It is believed today that flux tubes are formed at the base of the convection zone and rise to the surface through buoyant forces. During their buoyant rise, flux tubes are influenced by several physical effects, such as the Coriolis force, magnetic tension, drag and large-scale convective motion. The large-scale magnetic flux tubes undergo a dramatic evolution before reaching the solar surface and probably split, due to hydrodynamic forces, to form small-scale fibrils. The lack of understanding of the relative importance of these forces in the formation and evolution of active regions has lead many observers to develop large-scale statistical studies to undrestand the characteristics of active regions (Howard 1996).
Observations support the idea that active regions on the sun are
formed by the emergence of a large number of separate small
intense flux bundles of the order of 500 G and radii
200 km
(
1018 Maxwells) when they first appear, but that soon
are compressed to
G over 100 km in the
photosphere (Brants & Zwaan 1982; Brants 1985; Brants & Steenbeck 1985). The
flux bundles show a strong tendency to cluster together to form
pores and sunspots as long as fresh flux continues to emerge. This
effect vanishes when emergence ceases (Zwaan 1985).
The separate magnetic flux tubes observed in the photosphere expand in the chromosphere to fill the available space. Hence the clustering observed at the photosphere compresses the close-packed field at higher levels and therefore is opposed by the magnetic stresses. It is obvious that the clustering does not appear spontaneous and it must be driven by hydrodynamic forces beneath the photosphere (Parker 1979, 1992).
Many models have been proposed for the formation and evolution of
active regions, such as the rise of a kink-unstable magnetic flux
tube (see Moreno-Insertis 1992) or the statistical description of the
dynamical evolution of large-scale, two-dimensional, fibril
magnetic fields (Bogdan & Lerche 1985). Schrijver et al. (1997a), using the methods
originally invented by Bogdan & Lerche (1985) for the convection zone,
constructed a set of rate equations, that are valid only at
regions of weak gradients (quiet sun). Schrijver et al. (1997a) searched for
a balance between the flux emergence and the competing processes
of diffusion (partial cancellation, coalescence and fragmentation)
Schrijver et al. (1997b) extended the magnetic carpet model to active
regions. In this model, the collision frequency
between the
fibrils is assumed to vary quadratically with the number density
of their concentration (Nt) i.e.
.
Their
fragmentation rate K is assumed to be proportional to the local
magnetic flux
The solutions deduced from the rate
equations are very sensitive to the spectrum of the emerging flux
concentrations that replace the cancelling flux. The solutions are
also controlled by the ratio of the coefficients k and
which are both loosely related to the physical processes at the
photosphere. Longcope & Kankelborg (1999) use the statistical results of
Schrijver et al. (1997a) to study the interaction of randomly moving
photospheric magnetic flux elements of opposite signs and the
appearance of an X-ray bright point.
Independent models have also been developed using the anomalous diffusion of magnetic flux in the solar photosphere to explain the fractal geometry of the active regions (see Lawrence 1991; Lawrence & Schrijver 1993; Milovanov & Zeleny 1993) and a simple percolation model was also developed where clusters were formed by randomly placed fibrils at the photosphere (see Schrijver et al. 1992).
A new percolation model based on well-known observations was developed to simulate the formation and evolution of active regions by Wentzel & Seiden (1992) and Seiden & Wentzel (1996). In this model the flux emergence was based solely on the observational fact that "magnetic flux emerges where there is flux already''. Fibrils follow a random walk at the surface and collide with other fibrils, merging when they have the same polarity or cancelling when they meet fibrils of the opposite polarity (Wang et al. 1989; DeVore et al. 1985). The percolation model proposed by Seiden & Wentzel (1996) incorporated all the diffusion characteristics present in the magnetic carpet model of Schrijver et al. (1997a) but differs in one fundamental aspect: the process with which the magnetic flux emerges at the surface. The magnetic carpet introduces new flux when it is cancelled while the percolation model uses the rule described above. Both reach a steady state at a given activity level. The percolation model explains the observed size distribution of active regions and their fractal characteristics (Meunier 1999). Vlahos et al. (2002) analysed the sporadic energy release through flux cancellation (reconnection) when flux tubes of opposite polarities collide and analyzed the statistical properties of the energy released. They showed that the percolation model can easily interpret the statistical characteristics of the Ellerman bombs, coronal bright points, Ha bright points and transition region impulsive EUV emission.
In this article, we expand the percolation model proposed initially by Seiden & Wentzel (1996) and recently further developed by Vlahos et al. (2002) to estimate the dynamic evolution and the statistical properties of the magnetograms formed by our simulations. Using standard force-free extrapolation techniques, we estimate the evolving 3-D structures above the photospheres and we investigate in detail the statistical properties of the horizontal discontinuities.
We propose in this article that the main physical properties, as derived from the observations of the evolving active regions, can be summarized in simple Cellular Automata (CA) rules:
A 2-D quadratic grid with
cells (grid sites) is
constructed, in which each cell has four nearest neighbors. The
grid is assumed to represents a large fraction of the solar
surface, more precisely, as the the left and right boundaries are
periodical, it represent a zone around the equator of the sun of
72 degrees width. Initially, a small, randomly chosen percentage (
)
of the cells is magnetized (loaded with flux) in the form
of positively (+1) and negatively (-1) magnetized pairs (dipoles);
the rest of the grid points are set to zero. Positive and negative
cells evolve independently after their formation, but their
percentage remains statistically equal.
The dynamical evolution of the model is controlled by the following probabilities:
P: the probability that a magnetized cell is stimulating the appearance of new flux at one of its nearest neighbors. Each magnetized cell can stimulate (add one positive or negative flux unit) its neighbors only the first time step of its life. This procedure simulates the stimulated emergence of flux which occurs due to the observed tendency of magnetic flux to emerge in regions of the solar surface in which magnetic flux had previously emerged. The physical interpretation of this rule of the CA is the following: magnetic twists, or even knots, travel along larger-scale field lines, as shown by Parker (1979) for force-free fields. But usually twists and knots cannot travel freely because they caught up in the field structure due to line tying. Only occasionally, especially when the field is already somewhat simpler than normal, the twists may travel until they encounter other twists. Then both annihilate and the field is further simplified. The release of flux tubes creates sufficient newly vacated space that nearby fields can relax while expanding into this space. The relaxation provides new opportunities for the twists and knots on those field lines to travel. They have a renewed chance to reach sites where dissipation is possible. Clearly there is then some probability that these fields, newly relaxed and simplified, become sufficiently simple to constitute a flux tube that also rises to the surface (see Wentzel & Seiden 1992 for a qualitative discussion of the relation of the probability P with the physical processes expected below the photosphere.).
D
:
the flux of each magnetized cell has a
probability
to move to a random neighboring cell, simulating
motions forced by the turbulent dynamics of the underlying
convection zone (see Simon et al. 1995). If the moving flux meets
oppositely polarized flux in a neighboring cell, the fluxes cancel
(through reconnection), giving rise to a "sporadic energy
release''. If equal polarities meet in a motion event, the fluxes
simply add up.
D: the probability that a magnetized cell is turned into a non-magnetized on one time-step if it is next to a non-magnetized cell. Each magnetized cell has probability 1-(1-D)n to become non-magnetized, where n is the number of its non-magnetized neighbors. This rule simulates two effects, the direct submersion of magnetic flux and the disappearance of flux below observational limits due to dilution caused by diffusion into the empty neighborhood. It gives us also a control over the lifetime of the flux-tubes on the photosphere.
E: the probability that a non-magnetized cell is
turned into a magnetized one spontaneously, independently of its
neighbors, simulating the observed spontaneous emergence of new
flux. Parker (1992) suggested that flux tubes may start to rise in
response to thermal plumes in the convection zone. Plumes not only
punch through the magnetic field but carry some field with them
which then continues to rise to the surface. If plumes were the
only case of rising flux tubes, then the resulting surface
structures would not exhibit any of the correlations that are
apparent in the active regions. Thus in our model the flux
emergence caused by plumes corresponds to the spontaneous
emergence controlled by the probability
.
Magnetic flux appears always in the form of dipoles. Whenever a
new flux tube appears on the grid by stimulation or spontaneous
emergence, an opposite flux tube also appears, to form a dipole.
The distance between the two poles is
,
where l is a
constant; in the results presented here we use l=10 and
takes a random value between 0-5. The emergence of the
oppositely polarized flux takes place in such a way that all
active regions have the same orientation. During each timestep, we
apply the four rules successively scanning the grid four times and
we store the changes of each of the four scans in a dummy array.
At the end of the timestep, we record the sporadic energy release
and update our main array.
Our model can incorporate differential rotation of the grid. We decided not to include it, since after several tests we came to the conclusion that it has no effect on our statistical results. Seiden & Wentzel (1996) also indicated that differential rotation is unimportant for the young active regions studied.
The level of the active cells where the stabilization is reached
depends critically on the parameters
.
The observed
level of activity at the photosphere places a constraint on their
values. In the rest of the article these values will be kept fixed
and will be called "the standard values''. These values are in no
way unique; slight changes in any of the parameters do not
dramatically affect
the behavior of the model as long as we readjust the
other two free parameters. The level of activity will increase
dramatically if the critical percolation coefficient is reached.
In Fig. 1 we present the evolution of our model using
three different values of P.
![]() |
Figure 1: The percentage of magnetized cells as a function of time. After a short spike, lasting 1000 time steps, the system is stabilized. Dashed line: P = 0.181, solid line: P = 0.179, dotted line: P = 0.177. The method used to calibrate the time in our model is presented in Sect. 2.3.1. |
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The active regions for four different time steps are presented in
Fig. 2. (The method used to calibrate our model in space
and time will be explained later in this section.) These pictures
are the magnetograms produced from our model. All the pictures
are taken were the system had reached stabilization (see Fig. 1). The emphasis in these "magnetograms'' is not placed
on the detailed and accurate representation of all the observed
characteristics, but on the overall statistical properties of the
bipolar structures.
![]() |
Figure 2:
A
|
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We can estimate several observed statistical characteristics of
the active regions using a time sequence of magnetograms produced
from our model. We start with the size distribution, the
distribution of rise times to maximum development (Fig. 3) and the fractal dimension.
![]() |
Figure 3: a) Size distribution from the simulated magnetograms. b) Distribution of rise times to maximum development. |
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We define an active region as a cluster of contiguous active
cells. Neighboring but not adjacent clusters are considered as
different active regions. Wherever in this work we needed to use a
cluster counting method to derive our statistics, we used the
algorithm presented by Stauffer & Aharony (1985), modified suitably for each
case. The size distribution function of the clusters of the active
cells using the standard values for the free parameters was
approximated by a least square power law fit of the form
![]() |
(1) |
![]() |
Figure 4:
a) Frequency distribution of |
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Comparing this graph with the data, we can calibrate the x-axis,
since 150 pixels in our scale are equivalent to
in the
data, or 1 pixel corresponds to
.
Seiden & Wentzel (1996)
calibrated the time scales involved in their model by using the
observed time to maximum development of the active regions and
compared this result to the percolation model. We have used the
same method to calibrate our model. The time of raise to maximum
development is defined as "rise time''. The distribution of rise
times (Fig. 3b) to maximum development begins with a
power law up to 21 timesteps and then becomes exponential. The
observations analyzed by Harvey (1993) show the same form with a
power law extending up to 1.1 days. So the time scale corresponds
to 1.26 h/timestep. Therefore, our phenomenological model is
calibrated in space and time through the existing data. We have
used this result in Fig. 2.
The fractal dimension of the set of active cells in the model has
been measured using the method of box counting (Falconer 1990). The
image is covered with coarse-grained boxes of uniform scale L. If N(L) is the number of boxes containing at least one active cell,
then the limit
![]() |
(2) |
A detailed statistical analysis of four more parameters related to
the observed magnetic field at the photosphere, namely the
absolute value of the total flux (
)
of each active region,
the flux density (
), the maximum magnetic field (
), and the ratio of the maximum magnetic field to the
mean magnetic field (
)
have also been
performed. The frequency distributions of the four parameters
exhibit power laws for small values of the parameters with
indices
,
,
and
respectively, and well defined exponential turnovers for
large values at 100, 40, 40 and 50 units respectively (see Fig. 4). These results resemble remarkably well the
observations (Meunier 2003). Comparing the results from the model
with the observations we can calibrate the unit of the magnetic
field for the percolation model. The distribution of the maximum
magnetic field exhibits a power law up to 40 units of magnetic
field and then becomes an exponential. In the data presented by
Meunier (2003), this turnover occurs at 1000 Gauss. So 1 unit of
magnetic field of the percolation model corresponds to 25 Gauss.
A variety of observational results have been confirmed with our
model using a unique set of the free parameters reported initially
(the standard values). We now discuss the 3-D extrapolation of the
simulated magnetograms using the constant
force-free
approximation (see Alissandrakis 1981; Démoulin et al. 1997).
![]() |
Figure 5: a) A time series of the released energy, b) the energy distribution, c) the peak to peak waiting time distribution, d) the characteristic exponent of the waiting time distribution as a function of the threshold used. |
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![]() |
Figure 6:
a) The 3D topology of the magnetic field and b)
regions
in the 3D space with steep gradient in the
horizontal magnetic field component
(
|
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Equation (3) is linear and allows us to obtain solutions with
the use of Fourier Transforms (FT). We take the z-axis to be
perpendicular to the surface of the sun. The magnetogram gives us
the vertical component of the magnetic field on the surface (z=0plane). We assume that the Fourier transform of our solutions is
decreasing exponentially with height:
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(4) |
![]() |
(5) |
![]() |
(6) |
We use the percolation model to estimate the vertical component of the magnetic field at the boundary and obtain the three components of the magnetic field in the 3-D space above the modelled photosphere. We took care that the simulated magnetograms we used for extrapolation were flux-balanced.
For the visualization of our results, we use the magnetogram as the lower boundary of our image and we choose the points on the magnetogram with the most intense magnetic field to be the starting points for the magnetic field lines to be drawn (see Fig. 6a).
The free parameter
is responsible for the curling of the
field lines. As
increases the field lines get more and
more distorted and curled. We use a canonical value for
in this article (since
has the dimension
of inverse length, we measured the length in terms of the radius
of a typical sunspot on the boundary, and we have chosen
to be a fraction 0.3 of this inverse length unit (see
Sakurai 1981)). Problems related to the distortion at the edges
due to aliasing and their solution have been discussed in the
literature (see Alissandrakis 1981; Démoulin et al. 1997). A typical
extrapolation of the magnetogram produced by our percolation model
is given in Fig. 6a. We should emphasize once again
that it is beyond the scope of our study to give an accurate and
detailed representation of the coronal active region magnetic
field topology. The emphasis is placed on the statistical
properties of the structures formed.
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Figure 7: The magnetic field topology at four different heights: the "green carpet'' represents the z-component of the magnetic field while the vectorgrams represent the horizontal components. The yellow contours are the regions were steep horizontal magnetic gradients appear. |
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We next identify the regions were the horizontal magnetic field
forms steep gradients. For each point of
the 3-D space above the magnetogram, we compute the relative
gradient of the horizontal component of the magnetic field:
![]() |
(7) |
A detailed representation of the magnetic field topology and the regions with steep gradients is shown in Fig. 7. In this picture we plot the intensity of the z-component of the magnetic field for four different heights above the 2-D grid, using the force-free extrapolation method. For each of these plots, we overlay the horizontal component of the magnetic field (represented by the vectors) and the regions where the gradient of the horizontal component is steep, represented by the yellow contour plots.
It is obvious that in the proximity of the photosphere the steep
gradients are localized and concentrated in small volumes with a
strong magnetic field. As we move away from the photosphere the
gradients are spread in larger, cigar-shaped volumes. The
statistical properties, in each time step, of these structures
will be examined in the next section.
![]() |
Figure 8: a) Volume distribution of the structures of steep magnetic field gradients and b) distribution of the available energy of the same structures. |
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Using twenty uncorrelated frames from simulated magnetograms we
estimated the 3-D force-free extrapolation of the magnetic field.
We impose an arbitrary threshold on the horizontal magnetic field
gradient (
)
and record the
structures developed in the 3-D simulation box (see Fig. 6b).
Region (
.
The distribution of the volumes of the structures that are created
is plotted in Fig. 8a. The frequency distribution of
the volumes follows a power-law with index -1.65. Additionally we
plot the probability distribution of the "available energy''
Finally, we measure the fractal dimension of the regions with
steep gradients in the 3D space. We used the same method of box
counting, imposing the necessary changes to apply it in three
dimensions. The fractal dimension was estimated to be
(see Fig. 9). We analyzed the fractal nature of
the unstable volumes for two reasons: (1) it was already pointed
out by McIntosh & Charbonneau (2001) and McIntosh et al. (2002) that the geometric
characteristics of the energy-releasing volumes play an important
role in the coronal heating estimates; and (2) we believe that
there is a correlation between the fractal dimension of the
unstable volumes and the fractal characteristics of the active
region (
.
We analyzed also the behavior of the statistical properties of the
steep-gradient regions by varying the parameter
from 0.01
to 0.09. The fractal dimension remains constant when we used
different values for
(from 0.01 to 0.09) in the force
free extrapolation method. We found that the volume distribution
of the structures does not depend on
but rather on the
height from the photosphere.
The distribution of the available energy inside the structures
reported earlier remains also a power-law but the index changes
from 1.53 to 1.66 when
changes between 0.01-0.09. The
height of the box does not effect the distribution because the
energy is mainly concentrated close to the photosphere.
It is not obvious which of the above structures, if any, will
eventually release energy, but it seems that patterns formed at
the photosphere load the 3-D active region with structures which
follow specific statistical laws.
![]() |
Figure 9:
The fractal dimension of the regions with steep
gradients in the 3D space is estimated to be
|
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The results presented in this article suggest that the observed statistical properties of the magnetic fields at the photosphere (size distribution, fractal dimension, etc.), which are reproduced by the percolation model, produce naturally a loading process which is similar to the one used by Georgoulis & Vlahos (1996). We propose that the energy release in solar active regions follows closely the Self Organized Criticality (SOC) model driven by a power law loading. The percolation model provides the action at the photosphere and the subsequent loading of the active region. The avalanches produced through this specific loading follow the rules of the SOC and yields the observed sporadic energy release in flares. The combined model (Percolation as the driver and SOC providing a model for the energy release) can explain the observed flare statistics.
Our main conclusion is that the activity of the corona is strongly coupled to the detailed balance between the magnetic flux emergence and diffusion in the stochastic photospheric flows. The loading of the coronal active regions and the topology of the magnetic structures formed determine the subsequent evolution of the coronal active regions. We propose that the combination of the photospheric active region formation (using our percolation model) as a dynamic boundary that imposes a power law loading with the energy release processes following the Self Organized Criticality rules can describe the global characteristics of the observed coronal activity (coronal heating, flares, CME).
Acknowledgements
We thank Drs. H. Isliker, A. Anastasiadis and M. Georgoulis for their comments on our article. We also thank the anonymous referee for constructive criticism. E.R. would especially like to thank Prof. F. Moreno-Insertis for his help in understanding the force-free extrapolation techniques during her visit (as part of the European mobility program (Erasmus)) to IAC. This work was in part supported by the Research Training Network (RTN) "Theory, Observation and Simulation of Turbulence in Space Plasmas'', funded by the European Commission (contract No. HPRN-eT-2001-00310).