A&A 489, 441-447 (2008)
DOI: 10.1051/0004-6361:20079086
C. Gontikakis - I. Contopoulos - H. C. Dara
Research Center for Astronomy and Applied Mathematics, Academy of Athens, 4 Soranou Efessiou Str., Athens 11527, Greece
Received 16 November 2007/ Accepted 17 June 2008
Abstract
Aims. We investigate the distribution of heating of coronal loops in a non-flaring solar active region, using a simple electrodynamic model: the random displacements of the loop footpoints, caused by photospheric plasma motions, generate electric potential differences between the footpoints and, as a result, electric currents flow along the loops, producing Ohmic heating.
Methods. We implement our model on the closed magnetic field lines in the potential magnetic field extrapolation of an MDI active region magnetogram. For each one of the magnetic field lines, we compute the heating function and obtain the hydrostatic distribution of temperature and pressure. We find that coronal heating is stronger close to the footpoints of the loops and asymmetric along them. We obtain scaling laws that relate both the mean volumetric heating to the loop length, and the heating flux through the loop footpoints to the magnetic field strength at the footpoints. Our results agree with observational data.
Results. According to our model, we attribute the observed small coronal-loop width expansion to both the preferential heating of coronal loops of small cross-section variation, and the cross-section confinement due to the random electric currents flowing along the loops.
Conclusions. We conclude that our model can be used as a simple working tool in the study of solar active regions.
Key words: Sun: corona - Sun: activity - Sun: magnetic fields
Coronal loops are the main structures observed in the solar corona. To understand coronal heating, we must therefore understand how coronal loops are heated. One particular school of thought argues that the heating could originate from the braiding of magnetic field lines due to photospheric plasma motions (Parker 1972). According to this scenario, disturbed magnetic-field lines release the excess of stored magnetic energy by means of small-scale reconnection events that heat the plasma, and appear as bright loops.
A significant part of the energy release could be due to Ohmic heating of DC electric currents. Interestingly, the observed heating rates (Withbroe & Noyes 1977) cannot be reached if we consider Ohmic heating with an electrical resistivity based on Coulomb interactions of a fully ionized plasma (Spitzer 1962). Coronal plasma is a highly conducting medium, and such high heating rates can only be achieved on small spatial scales, such as inside reconnecting current sheets.
Coronal loop heating due to magnetic-field braiding can be simulated using resistive Magneto-Hydro-Dynamic (MHD) codes for a turbulent single loop (Rappazzo et al. 2007; Hendrix & Van Hoven 2001; Dmitruk & Gómez 1997, 1999) or an entire active region (Gudiksen & Nordlund 2002, 2005a,b). Petrie (2006a) modelled an ensemble of loops with current sheets, using analytical solutions of ideal MHD. All such numerical approaches present an inherent difficulty: one should include, in the same simulation, length scales of the order of meters on which energy diffusion occurs, and length scales of thousands of kilometers that represent the size of coronal loops (Klimchuk 2006). We could argue, however, that in situations where a steady-state turbulent energy cascade from larger to smaller scales develops, the dissipation rate is independent of the smallest scales considered in the simulation.
A phenomenological approach to the coronal heating problem is to obtain scaling laws that relate different physical characteristics of loops, such as maximum temperature, pressure and length, with the heating along their length, under the assumption that the loops are steady. Such scaling laws were tested in loops observed by Skylab (Rosner et al. 1978a; Serio et al., 1981) and Yohkoh (Klimchuk & Porter 1995) and in statistical samples of entire active regions (Golub et al. 1980; Fisher et al. 1998; Schrijver et al, 2004; Warren & Winebarger 2006).
In the present work, we develop a simple electrodynamic model that reproduces qualitatively the main morphological features of coronal loop heating without the need to resort to complicated three-dimensional numerical MHD simulations. Our working assumption is that the loops are heated by direct current (DC) Ohmic dissipation, caused by electric currents that flow randomly along the loops. These currents are generated by magnetic field-line braiding, due to photospheric convective motions at the loop footpoints. The complex microphysics involved in the heating mechanism, such as reconnection, current cascades and/or turbulence (see Aschwanden 2005, for a review), are modelled by means of an enhanced effective electric resistivity. Our aim is to investigate the distribution of coronal heating in an observed active region and compute scaling laws that can be compared with observations.
We begin with a description of our model in Sect. 2. In Sect. 3, we apply it to a particular observed active region and obtain various scaling laws. In Sect. 4, we study the hydrostatic atmosphere above the active region. Our conclusions are obtained in Sect. 5.
We base our discussion on the simplest possible average
coronal magnetic-field configuration, that of a current-free
magnetic field, where
At each photospheric point corresponds a value of the
vertical magnetic field
and a random horizontal
photospheric velocity due to granulation
km s-1.
This configuration leads to the development of random horizontal
electric fields
,
varying over the characteristic
velocity turnover scale l of the order of
1000 km. This is equivalent to the
development of a random photospheric electric potential distribution
In a quasi-stationary configuration, the kinetic energy of random
photospheric motions is continuously channelled through these random
electric currents to the heating of the coronal loop.
We may therefore model the
complex microphysics of the heating mechanism by means of an effective
electric resistivity
of the coronal plasma; each
coronal loop of length L and cross section along the loop Sthen develops an effective integrated resistance
The above parametrization allows us to estimate the random
electric currents flowing along each coronal loop above an active
region as
![]() |
(10) |
We have no physical justification for such a high value of the
coronal resistivity. Plasma phenomena, such as particle-wave interactions, inertial
effects or non-gyrotropic particle orbits can enhance the
resistivity by up to only
106 - 107 times the Spitzer
resistivity locally in the solar corona. The importance of these
effects is studied either with analytic estimations (Martens &
Young 1990), numerical computations (B
chner
& Elkina 2006), and laboratory experiments (Takeda &
Inuzuka 2000).
Interestingly, the 3D MHD simulations of Gudiksen &
Nordlund (2002), which reproduce a typical active
region, were produced with an effective (numerical)
resistivity that is higher than ours.
Therefore, our estimate of
remains phenomenological.
Our present paper represents a first step towards a detailed coronal-loop
heating model. Given our lack of understanding of
the physical mechanism producing such an enormous discrepancy
between
and
,
we ignore any dependence of the
electric resistivity on other plasma variables, such as
temperature (see however Rosner et al. 1978b and Buchlin
et al. 2007, who consider mechanisms such as special
turbulent regimes that can occur in the solar corona).
We show that, irrespective of the presence of strong
highly intermittent electric currents along the loops,
the current free approximation remains valid on average.
For the present calculation, 90% of the
values are
in the range
106 - 108 V, and 90% of the mean current
density along the loops are in the range
(A/m2). Along each loop, we computed the
parameter. For the present
computation, 90% of the
values are in the range of
(Mm-1).
Since the electric currents are orientated randomly along each
loop,
switches from positive to negative values in
neighboring positions. Therefore, the mean
measured over a
bunch of loops will be close to zero, which is consistent with the
potential field hypothesis. For example, in the area centred on
(see Fig. 1)
of the magnetogram, the average value of
,
as calculated
over 360 current carrying loops is 0.003 Mm-1 with
a standard deviation of 0.026 Mm-1.
We conclude that the potential approximation could be valid on large scales, but
not on small scales (lower than a few arcseconds), where the magnetic field may
be highly non-potential.
![]() |
Figure 1: Part of the MDI magnetogram of the active region NOAA 9366 that was used for the magnetic field extrapolation. White (Black) stands for positive (negative) line of sight photospheric magnetic fields. The active region is characterized by two dominant polarities. |
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The present model was applied to the active region NOAA 9366,
which was observed by the Michelson Doppler Imager (MDI)
magnetograph (Scherrer et al. 1995) and the Extreme Ultraviolet Imaging Telescope (EIT), (Delaboudinière
et al. 1995) both onboard the SOlar and
Heliospheric Observatory (SOHO) satellite (Domingo et al.
1995), at (S25W11) on the Sun, on March 6, 2001. This
active region was selected because of its low level of activity
(absence of flares), and isolation from neighboring active
regions. The magnetogram shows two spots of opposite polarity,
and no detected parasitic polarities (Fig. 1).
The spatial resolution of the magnetogram is 2
,
which
corresponds to about 1430 km at the surface of the sun. As we
said, a potential magnetic field extrapolation is a first order
approximation of the magnetic field structure above the active
region. Since we focus on a statistical description of the numerical
results computed by our model, we note that this approximation
is sufficient
(see, however, a discussion about the coronal loop cross-section
expansion with height in Sect. 5). We apply the method presented by
Alissandrakis (1981), by taking into account the geometric
corrections of the longitudinal magnetic field due to the position
of the active region on the solar disk. The result of our
extrapolation is plotted in Fig. 2.
![]() |
Figure 2: Field lines of the magnetic field extrapolation that were chosen to represent the active region loops. Most of the loops connect the two dominant polarities. The axes represent the pixel size of the magnetograph. |
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We consider field lines originating in each one of the MDI
measurement points. We select only field lines for which
|Bz|>16 Gauss at both footpoints (Mandrini et al.
2000) with length larger than 2 pixels. This reduces
the MDI noisy measurements of the magnetic field (Liu & Norton
2001). Field lines that cross the upper boundaries of the
computation box are not shown, and given the magnetogram spatial
resolution, this produced 1500 field lines. In our present
analysis, these field lines trace coronal loops with the
cross-section equal to the MDI spatial resolution squared at one
footpoint, i.e.
.
To study the statistical properties of the active region
above the magnetogram shown in Fig. 2, we calculate
the cross section (Eq. (4)), the resistance R(Eq. (3)), the electric current (Eq. (5)), and the
volumetric heating (Eq. (6)), for each one fo the 1500
coronal loops obtained above. Some important statistical
characteristics, and parameters of the heating model are
shown in Fig. 3. Panels a) and b) show the scatter
plot of the mean loop magnetic field
and mean loop
magnetic field energy density
as a function of
the loop length. The parts of the two scatter plots between 50
and 100 Mm can be represented with power laws of the form
![]() |
(11) |
![]() |
Figure 3: Averages of the magnetic field (panel a), the magnetic field energy (panel b), the maximal loop cross section (panel c), the resistance (panel d), and the average volumetric heating (panel e), as a function of the loop lengths. Panel f) shows the scatter plot between the mean volumetric heating and the mean magnetic energy along the loops. In the first two panels, a linear fit, in logarithmic unit was completed for loop lengths in the range 50-100 Mm. |
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An important characteristic of the computed volumetric heating function is its distribution with height. In Fig. 4, we see that the mean volumetric heating decreases with height in the same way as the mean magnetic energy density (dashed line). This is expected because the heating is roughly proportional to the magnetic field energy density (Fig. 3f), and, both quantities drop by almost an order of magnitude in the first 10 Mm above the photosphere. We note that our result disagrees with detailed numerical simulations (e.g. Gudiksen & Nordlund 2002).
![]() |
Figure 4: Mean volumetric heating (solid line) and mean magnetic field square (dashed line) as functions of height above the active region shown in Fig. 1. |
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In Fig. 5 we show the scatter plot of the loop maximum width versus the average heating of the loops. We note that we consider only loops that extend above the chromosphere, i.e. that are higher than about 2.5 Mm. The width enhancement is defined as the square root of the ratio of the maximum cross section at the loop top over the average footpoint cross section at the level of the chromosphere. We separate the loops in two scatter plots according to their length: 14-70 Mm in panel a), and 70-220 Mm in panel b). According to Eq. (7), only loops with heating rates above 10-3 erg cm-3 s-1correspond to observable coronal structures. We can directly see from panel a) that these loops have a maximum expansion on the order of about 2. As seen in panel b), loops with larger expansion factors have a lower heating rate and are therefore not observable.
![]() |
Figure 5: Maximum loop width (cross section square root) versus mean heating along the loops. The loop points are separated into 2 panels according to their length. |
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The heating along the loops is related to the magnetic field
observed at their footpoints. Figure 6 shows the
scatter plot of the heating flux density through the footpoints
F (in erg cm-2 s-1) as a function of the
average of
at both footpoints. This
scatter plot can be fitted by the relation
![]() |
Figure 6: Heating flux as a function of the average loop footpoint normal magnetic field. Each diamond in this plot represents a single loop. |
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A final note about the loop geometry is in order here. Coronal
loops are highly asymmetric and, as we see, this affects the
heating function in a significant way. To quantify this asymmetry,
we divided the loops into two parts of unequal length around their
apex. For the two parts, we compared the heating length scale
(defined as
)
and the heating h at the
footpoints. As before, we considered only the coronal part of the
loop above 2.5 Mm. Our results are shown in Fig. 7.
The geometry of 4 characteristic loops is shown in panel c), and
their corresponding heating functions h(s) in panel d). In
panel a), we plotted the ratios of the two heating length
scales over the loop length. Panel b) shows the footpoint heatings
for each loop. We see that heating length scales and footpoint
heating, can vary over several orders of magnitude from one
footpoint to the other, for the same loop. Fewer than 30 loops are
quasi-symmetric and are represented close to the diagonals of panels
a) and b).
It is known that loops with asymmetric heating functions develop
unidirectional mass flows from the most heated footpoint to the
less heated one (Winebarger et al. 2002; Patsourakos
et al. 2004). One can nevertheless obtain a first
approximation to the scaling relations of the full hydrodynamic
problem by calculating hydrostatic loop atmospheres along only one
half of the loop (Mok et al. 2005). We therefore decided to
solve the energy and pressure balance equations
![]() |
Figure 7: Statistics of the loop heating asymmetry are shown in the panels of the first row. Panel a) shows the ratios of the heating length scales over loop lengths. Panel b) shows the heating rate at each footpoint. Four examples of loops geometry (panel c) and heating (panel d) along their length showing their asymmetry. The thick parts of the curves correspond to the chromosphere. |
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The use of classical thermal conductivity is justified by the analysis of
damped acoustic waves observed along coronal loops
(Ofman & Wang 2002; Klimchuk et al. 2004).
The right hand side takes
into account volumetric heating and radiative cooling.
The latter is proportional to the product of the square of the
electric density and a function of the temperature
Rad(T), which is given by piecewise power laws (Rosner
et al. 1978a). In the pressure balance equation,
Eq. (16),
is the average ion mass for
a coronal composition of a 90% hydrogen and 10% helium plasma
(Aschwanden & Schrijver 2002),
g is the hydrogen mass,
cm s-2 is
the gravitational acceleration on the solar surface, and
is the angle between the gravitational force and its projection
along the given coronal loop.
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Figure 8: Correlations derived from the stable hydrostatic solutions for half loops. Panel a) shows the maximum temperatures as a function of the loop lengths. Panel b) shows the footpoint pressure as a function of the loop lengths. Panel c) shows the maximum temperature as a function of the footpoint pressure and panel d) the maximum temperature as a function of the mean heating. |
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The integration starts at an altitude of 2.5 Mm, above the
chromosphere and ends at the top of the loop. The boundary
conditions at the coronal footpoint consist of temperature
of
K (Aschwanden & Schrijver 2002;
Rosner et al. 1978a) and zero conduction, which implies that
the loops are in equilibrium and do not conduct energy to and from
the chromosphere. For each loop, the base pressure of the solution
is obtained by means of a ``shooting'' method that guarantees
at the top of the half loop.
Figure 8 shows scatter plots derived from the stable
hydrostatic half-loop solutions. Panel a) shows the maximum
temperatures as a function of the loop heights: 90% of the loop
heights are below 35 Mm, and 90% of the hottest loops, above
800 000 K, have a height below 26 Mm. In panel b), the loop base
pressures are in the
10-4 - 1 dyn/cm2 range. The higher
temperatures and base pressures are found for shorter loops. The
maximum loop temperatures and base pressures, as seen in panel c),
are related by a power law
We simulated and compared the active region morphology with two images of the active region recorded with the EIT telescope taken in the 171 Å and 284 Å passbands. We then computed the brightness of the hydrostatic loops in the 171 Å and 284 Å passbands using the response functions of EIT. We took into account the loop width when computing the emission images. In Fig. 9 we compare the two EIT images of the active region with the corresponding simulated images. The two EIT images were taken within 2 h of the magnetogram observation time. The intensities in the four panels are in a logarithmic scale.
By comparing panels a) and c) of Fig. 9 we can see that
the magnetic field extrapolation represents qualitatively a class
of loops connecting the two main magnetic polarities of the active region with their east footpoint at (90
,
-310
)
and their west one at (250
,
-305
)
in solar
coordinates. In the 171 EIT image, there are also loops with one
footpoint anchored at (90
,
-310
)
a second
footpoint in the east part of the active region and loops
anchored at (250
,
-305
)
closing down at the west part
of the active region. In panel c), these ``periphery'' loops are
represented by field lines that cross the boundaries of the
computational box. The west footpoints of these `` east periphery'' field
lines have scattered positions far away from the pixels
corresponding to (90
,
-310
)
in the EIT image.
A possible reason is that we omitted field lines crossing the
high altitude boundary of our computational box (open lines).
In conclusion, we can say that the magnetic field extrapolation
represents qualitatively some
of the main morphological structures of the active region, although it is
not sufficiently accurate for a detailed comparison with observations. Even with
this limitation, we obtained some interesting results on the
computed active region morphology from the two passband images.
By comparing the EIT images a) and b) we can see that the bunches
of loops in the 171 passband which represent cooler (106 K)
plasmas, cover a larger area than the hottest (
K)
loops in the 284 Å image. This is more obvious for the ``periphery'' loop system, which is hardly visible in the case of
the 284 EIT image. Panels c) and d) show a similar morphology. The
``periphery'' computed loops that cross the borders in panel
c) are less visible in panel d), which means that on average they
are far cooler. The reason is that only 41 of the computed loop atmospheres
have a maximum temperature higher than
K. These
loops connect the main polarities in the central core of the active region and
appear mostly in the 284 Å passband EIT image.
In these panels we can also see that the bright
loops appearing in the computed image have a small thickness variation
along their length. In fact, the heating-maximum thickness
relation of Fig. 5 is stronger for the loops with a
hydrostatic solution so that the brighter loops have a smaller
thickness variation.
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Figure 9: Panels a) and b) show AR 9366, observed in the 171 Å and 284 Å EIT passbands respectively. Panels c) and d) show the computed emission in 171 and 284 based on the hydrostatic solution loops. |
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We have presented a simple model for the distribution of coronal heating produced by DC-currents along coronal magnetic-field lines. The electric currents are due to the potential differences at the footpoints of the magnetic field lines induced by photospheric plasma motions. In our picture, heated plasma along magnetic field lines appears as bright coronal loops. We applied our picture to a particular observed active region. Coronal loops were simulated using a potential extrapolation of the magnetic field observed at the level of the photosphere with MDI. We calculated the electric resistance of each loop and applied Ohm's law to obtain the heating function at each point of the active region. Given the heating function and magnetic field geometry, only a small fraction of the coronal loops support a hydrostatic atmosphere.
Our model yields several testable results, expressible as scaling
laws that could be compared with observations. An important result
is the heating-loop length relation represented by a power law
in Eq. (12). This result is compatible with the index
of
deduced from observations (Porter & Klimchuk
1995). Moreover, the heating that we obtain is closely
proportional to the square of the magnetic field along the loop
(Fig. 3f), which implies that the mean heating of the
active region variation with altitude is similar to the variation
in the magnetic energy. Our result differs from that of
Gudiksen & Nordlund (2002), where the heating decreases
more sharply with altitude than B2. Finally, the heating-flux
density versus footpoint magnetic-field relation described by the relation in
Eq. (14), is compatible with the results of Schrijver
& Aschwanden (2002), which were deduced from
observations. The expressions of the loop heating distributions presented in Eqs. (12) and (14) correspond to the particular morphology of the active region, where the hottest loops are the shortest ones that connect the two main magnetic-field polarities of the active region (Fig. 9). These loops dominate in the simulated 284 Å passband of the EIT instrument whereas cooler loops, which do not connect only the two main magnetic-field polarities, are mostly detectable in the 171 passband in good agreement with observations.
Despite its simplicity, we therefore conclude that our model is able to reproduce the observations.
An interesting yet unsolved problem is that coronal loops appear to have a constant width along their length. The largest measured width variation is 1.15 to 1.3 from footpoint to loop top (Klimchuk et al. 1992; Aschwanden et al. 1999; Watko Klimchuk 2000; Lopez Fuentes et al. 2006). In the present simulation, only loops with a small width expansion are heated to an observable heating rate (Fig. 5). The expansion factors obtained for those loops are slightly higher than the aforementioned observed values. A possible resolution of this inconsistency could be to include the random longitudinal (i.e. along the loop) electric currents of our model in a more accurate non-potential reconstruction of the active region magnetic field (see however Lopez Fuentes et al. 2006). We expect that the higher the longitudinal electric current density, the more uniform the loop cross section along its length.
The loops and the associated heating functions have a high degree of asymmetry. Such loops cannot support atmospheres in hydrostatic solutions and will develop mass flows. To a first order approximation, we can derive the temperature and density distribution along the loop by computing hydrostatic solutions for one half of the loop, from one footpoint to the loop's apex.
The hotter of these loops are found at lower altitudes (Fig. 8), which is compatible with observations. Other physical processes such as steady MHD flows (Petrie 2006b), or impulsive heating (see Patsourakos & Klimchuk 2006; Warren & Winebarger 2006), may also be considered in the calculation of the structure of the active region atmosphere.
We conclude by stating once again that our model presents a simple idea that may answer some aspects of the coronal heating without complex numerical simulations. Several possibilities, such as the non-potential nature of the magnetic field extrapolation, variable electric resistivity, more realistic photospheric velocity field, and non hydrostatic loops, may further be explored in future work.
Acknowledgements
We would like to thank our anonymous referee who helped to improve our manuscript, as well as S. Patsourakos and G. J. D. Petrie for useful suggestions. CG dedicates this work to the memory of Stephanos C. Gontikakis.