A&A 386, 1106-1122 (2002)
DOI: 10.1051/0004-6361:20020179
G. Aulanier1 - B. Schmieder1,2
1 - Observatoire de Paris, LESIA, 92195 Meudon Cedex, France
2 - University of Oslo, ITA, PO Box 1029, Blindern, 0315 Oslo, Norway
Received 26 November 2001 / Accepted 23 January 2002
Abstract
Previous works have shown that dark and wide EUV filament channels
observed at
Å are due to absorption of EUV lines
in cool plasma condensations that are not observed in
.
We extend this interpretation and we address the issue of the
possible injection of their mass into CMEs, through the
magneto-hydrostatic modeling in 3D of one filament observed both
in
and in EUV. The model parameters are fixed so as
to match the
observations only. Further comparison of the
model with the EUV observations reveal the magnetic nature of
the absorbing plasma condensations.
They are formed in magnetic dips, as for the filament itself. Opacity
ratios and the hydrostatic condition imply that the dips must be filled
by cool material up to 1700 km, which increases the filament mass by 50%
as compared to
estimations. Far from the filament, the
absorbing condensations are located below 4 Mm in altitude above the
photosphere, on the edge
of weak photospheric parasitic polarities, within the lower parts of
long field lines overlaying the filament. By physical analogy with
filament feet, we redefined these extended regions as EUV
feet. The broadening of the EUV filament channel is dominated by
EUV feet, while the larger filling of dips plays a
non-negligible but minor role.
Further implications from this work are discussed, on the visibility
and the geometry of the condensations, on the existence of EUV
filament channels in the absence of filaments, on the loading of cool
material into filament feet through bald patch reconnection and on the
complex geometry of the upper prominence-corona transition region.
The magnetic topology implies that during the filament eruption, the mass
of its wide EUV feet will not contribute to the CME, whereas
the extra mass provided by the large filling of dips in the filament
flux tube will be loaded into the CME.
Key words: Sun: chromosphere - filaments - magnetic fields - UV radiation - solar-terrestrial relations
Solar filaments/prominences in their quiescent phase are the largest and best observed coronal structures in which dense plasma is confined in highly stressed magnetic fields. These fields contain a large amount of free magnetic energy, which can eruptively be released through several processes (see the reviews of Forbes 2000; Klimchuk 2001; Low 2001). This naturally explains why some CMEs are associated with filament/prominence eruptions (see e.g. van Driel-Gesztelyi et al. 1998; Schmieder et al. 2000; Delannée 2000; Marqué et al. 2002).
The total mass embedded in a CME has been estimated from
coronograph observations in the range of
1015-16 g
(Gosling et al. 1974; Howard et al. 1985; Hundhausen 1988).
Typical prominence masses are difficult to
measure due to uncertainties in the estimation of ionization
degree and the filling factor (see the reviews of Schmieder
1989; Vial 1990). Considering a typical H
prominence
as a thin volume whose thickness, length and height are
respectively 5, 100 and 40 Mm and taking a mean proton
density of the order of
1010-11 cm-3, then typical
prominence masses range in
g. So,
erupting filaments may account for a non negligible fraction
of the total mass of their related CMEs.
Recent findings on wide EUV filament channels (detailed
below) suggest that filaments may contain much more mass than
what is shown by
observations. Moreover, about
40-60% of all CMEs are associated to filament/prominence
eruptions (Delannée et al. 2000; Subramanian & Dere 2001).
So independantly of coronographic measurements, the fraction of
the mass from a wide EUV filament channel that can be loaded
into a CME when its related filament erupts needs to be
estimated. This issue is important for solar-terrestrial relations
because the kinetic energy of a propagating CME is an
important parameter to study its interaction with the
magnetosphere.
In EUV, the typically observed structure of a filament is a wide
region located along the
filament axis, which corresponds to an
intensity depletion. This region is usually referred to as the
"EUV filament channel'' (hereafter EFC). These structures
have often been reported from Skylab and OSO-4 and -6
observations (Orrall & Schmall 1979, 1979), and are now frequently
observed with SoHO instruments such as SUMER, CDS
(Kucera et al. 1999; Chiuderi Drago et al. 1998, 2001;
Heinzel et al. 2001; Schmieder et al. 2002)
and EIT (Wang 2001, see also Fig. 1), as well as
with the TRACE satellite (Chae 2000). The width of an EFC
can vary from 10 to 50 Mm along its axis, which is in average 5
times wider than its related
filament body.
Chiuderi Drago et al. (1998, 2001) have reported that for emission
lines of a given ion, EFCs are not observed for wavelengths
larger than 912 Å, whereas they are clearly visible for shorter
wavelengths. Therefore it has been proposed that EFCs are due to
the absorption of the background EUV radiation by the Lyman continuum
of hydrogen, in suspended cool plasma condensations in which neutral
hydrogen is present. Heinzel et al. (2001) and Schmieder et al. (2002)
have shown that such condensations are visible in EUV on each side
of
filaments. The lack of
absorbing material in
EFCs has been explained by opacity ratios: with NLTE models,
Heinzel et al. (2001) have calculated that for typical prominence
temperatures, the opacity for
is typically 50-100 times
lower than the opacity
at the head of the Lyman continuum of hydrogen.
Therefore EUV observations of filaments and their surroundings
reveal a much larger distribution of mass than for their related
filaments. The aim of the present study is to explain
(i) how cool plasma condensations (which absorb EUV
radiation) can be formed aside of a filament body and away from
its feet (thus being able to form a wide EFC), to identify (ii)
what is the magnetic field in and around these condensations, (iii)
what is their altitude in the solar atmosphere, (iv) what is their
relation with the filament magnetic fields, and to estimate (v) if
they can contribute to the CME mass when the related filament
eventually erupts.
To address these issues, we perform a linear magnetohydrostatic (LMHS) model of one intermediate filament observed on May 5, 2000 at E17 S21, during a coordinated campaign between THEMIS and SoHO, conducted at the MEDOC operation center. We used a line of sight magnetogram as boundary conditions, and we compared the calculated magnetic features with the EUV observations.
The paper is organized as follows: in Sect. 2, we list the multi-wavelength observations of the
studied filament and we describe specific features.
In Sect. 3, we explain the computational method to calculate
linear magnetohydrostatic configurations, and we construct a
grid of 35 models for various values of the free parameters.
In Sect. 4, we select one of the models so as to match the
data independantly of the EUV data, we give
physical interpretations of the
filament and we describe
the resulting magnetic topology of the filament flux tube.
In Sect. 5, we estimate the plasma filling of magnetic dips
and we show that calculated low-lying magnetic dips match the complex
shape of the observed EFC, which provides direct answers to the
issues (i-iv) addressed above.
In Sect. 6, we compare our modeled topology with other
prominence models and with
observations of filaments.
We also discuss further implications derived from the model on the
injection, the distribution and the visibility of mass in EFCs,
on the possible existence of EFCs in the absence of filaments,
and finally on the fragmented nature of the upper prominence corona
transition region.
In Sect. 7 we address the issue (v) and we show that the
model predicts that the wide extensions of EFCs will not
contribute to the mass loading of CMEs so that only the
mass contained in the filament flux tube will be ejected.
A summary of the results is given in Sect. 8.
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Figure 1:
Partial view of full disc data from the Meudon spectroheliograph
in
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Figure 2:
Intensity maps of the filament channel observed on May 5, 2000 at
E17 S21. Top:
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This paper is focused on the analysis of one filament observed on May 5, 2000 at E17 S21, during a MEDOC campaign with the MSDP of the franco-italian telescope THEMIS and with SUMER and CDS onboard the SoHO spacecraft. The full description of the data acquisition and of the dataset is provided in Heinzel et al. (2001) and in Schmieder et al. (2002).
In the present paper, we use two intensity images from this
campaign: one of the MSDP in
,
obtained at 7:52 UT,
and one of CDS in O V at 629.73 Å, obtained at 8:12 UT
for which 51 min were necessary to do the raster.
We choose this wavelength because it displayed mostly the same dark
features than in the 5 other recorded lines (Si XII [520.60
Å], Ca X [557.77 Å], Ne VI [562.80 Å], He I
[584.33 Å] and Mg X [624.94 Å]), but with a better contrast.
For the
modeling work we also consider one SoHO/MDI line of
sight magnetogram, obtained at 8:00 UT (shown in Fig. 1).
For the aim of the present study, a good co-alignment between the data is crucial, especially for the comparison of models with the observations. But since the MSDP and CDS data are not full disc, we co-align the observations in several steps.
First we overlay the dark filament observed with THEMIS with
a full disc Meudon
spectroheliogram observed at 10:18 UT
(a partial view is shown in Fig. 1). Then
we overlay the Meudon full disc image (after translating it to
account for solar rotation) with the MDI data. In order to
minimize the effects of the evolution of the structures between 8:00
and 10:18 UT, we fine-tune this overlay so that the bright
plages match the strong magnetic fields as well as possible.
In a third step, the CDS image is overlaid with these data
by matching the EUV network brightenings with the strongest
magnetic fields, using an iterative tracking of pre-selected features
such as network brightenings.
Note that during all these steps, we do not modify the magnetogram,
which
otherwise could reduce the reliability of the modeling
(described in Sect. 3). The resulting co-alignment of
the THEMIS, CDS and MDI data is shown in Fig. 2. As pointed out by
Heinzel et al. (2001), the
filament in
is thinner than the EUV filament channel
(EFC) by a factor 5 in average.
Figure 1 shows that the studied filament is located between two decaying active regions (AR1 and AR2), between faculae of opposite polarities, which is typical of 75% of filaments (d'Azambuja & d'Azambuja 1948; Tang 1987). Two other intermediate filaments F1 and F2 are present, on the neutral line of AR1 and AR2 respectively. On that day, the filament F2 was not yet well formed, but both the EUV filament channels for F1 and F2 are clearly visible.
Figure 2 (top) shows that the
filament
has an elbow located at the edge of a strong magnetic
concentration of positive polarity.
This leads to a curved "S-shape'' for the filament, which
may be interpreted as a sigmoid. We discuss in Sect. 4.2 the validity of this interpretation. The filament feet
clearly have a left-bearing chirality. Since the filament is in the
southern hemisphere, the feet follow the chirality rules found by
Martin et al. (1994). At first look, the feet can hardly be associated
with strong parasitic polarities, but a careful examination of the
co-aligned data permits us to identify several weak parasitic polarities
(
-10 G) that are well associated with the feet (see
Sect. 4.3), in accordance with Martin (1990), Aulanier
et al. (1999) and Wang (2001). Some dark fibrils are present in the
filament channel, but due to seeing effects they are not sharp.
The EFC as observed by CDS shows a complex pattern of dark
regions which appear nearly continuous around the neutral line, and which
becomes more and more inhomogenuous away from it (see Fig. 2 (bottom)). In particular, our
fine-tuned co-alignment proves that the elongated thick lateral extensions
in EUV do not follow the
feet. Most of these extensions also
have a left-bearing chirality, however we cannot infer a chirality rule for
EFCs based on this single filament. Some isolated bright patches are
present in the outer parts of the EFC, which all correspond with
magnetic field concentrations.
Interestingly, Figs. 1 and 2 show that the
EFC has the same morphology as observed in O V at
629.73 Å, in He II at 304 Å and in Fe XII at 195 Å.
With the continuum absorption model, this similarity suggests that
EFCs observed with EIT (see e.g. Wang 2001) should also
be due to the absorption of EUV lines, but
in this case not only by the Lyman continuum of H (
Å) but also by the continua of He I (
Å) and He II (
Å), as for arch
filament systems observed in EUV (Mein et al. 2001).
Among the 6 wavelengths observed by CDS the O V line is the
only one that shows a thin elongated brightening in the middle of the
EFC. This O V spine is nearly continuous, and its location
varies from the center to the edge of the
filament along its
axis. We conjecture that this spine may be due to the emission from the
upper prominence-corona transition region (PCTR). Its absence in the
other observed wavelengths recorded by CDS is consistent with
Chiuderi Drago et al. (1998, 2001), who reported that the emission of
the PCTR at the top of filaments was negligible.
In Cartesian coordinates (
,
,
),
where z is the altitude, linear magnetohydrostatic (LMHS) fields
can be calculated up to any height z>0 by solving the following equation
derived by Low (1992):
For the purpose of this study, the lower boundary conditions are
fixed by projecting the distribution of the line of sight component
observed with SoHO/MDI onto the photospheric
plane. So
is obtained. As no existing data
could provide the transverse components of the magnetic field, we assume
that
,
where
is the angle between the line-of-sight (l) and the vertical (z)
directions. For the filament located at E17 S21,
.
The projection effects are accounted for by the use of
the procedure described in Démoulin et al. (1997).
In previous filament models done with LMHS method (Aulanier
et al. 1999, 2000) Bz* was modified in order to
ensure the presence of a flux rope for high values of
.
Here we perform direct extrapolations of Bz* without any
modification. On one hand, this choice leads to more difficulties in
finding a good combination for the free parameters of the model, but
on the other hand the obtained results should be more reliable
than if the magnetogram was modified.
Once Bz* is fixed, the remaining free parameters for the
extrapolation are Dx, Dy and
,
a, H.
The orientation of the computational box is chosen so that its y
axis corresponds to the averaged direction of the observed
filament, which makes an
angle with the solar North (see
Figs. 1 and 2 (top)).
The choice for Dx is not easy because it represents the periodicity of the model perpendicularly to the filament axis. We can evaluate its value from the observations: Fig. 1 shows that the studied filament is located between two decaying active regions (AR 1 and 2) which form a succession of [+, -, +, -] magnetic polarities. We approximate this observed property as a local quasi-periodicity in x. So for a distance in y corresponding to the length of the central filament, we choose Dx to be the average distance between the two neutral lines of AR1 and AR2. We then obtain 192 Mm as an approximated value for the quasi-periodicity. So we choose Dx=192 Mm.
Since Dx is chosen from observational constraints, it defines the
maximum length scale of the box as well as the maximum allowed value
for
in (see Eq. (6)). Therefore we have
to choose
.
However the length of the studied filament
as observed in
is
245 Mm, so larger than Dx
by ![]()
.
So in order to calculate a model for a filament
portion as long as possible, we choose Dy=Dx=192 Mm.
The centering of the computational box is done so that the intersection
of the
filament body with the box edges nearly occurs at the
same position along x, so that the periodicity effects along y are
minimized. The positioning of the computational box above the
observations is shown in Fig. 2.
We checked a posteriori the validity for the choice of the size
D=Dy=Dx of the computational box by re-calculating
several LMHS
models with 150 Mm <D< 400 Mm. We qualitatively found similar results
as in the following for 180 Mm
Mm. Also in order
to estimate the periodicty effects, we re-did a posteriori the calculations
of this paper with different shifts
for the positioning of
the box along the filament axis with
.
We noticed
that the calculated magnetic dips (as described in Sects. 4.2, 4.3 and 5.3) are not very
sensitive to shifts
.
This shows that the periodicity
effects along y are not importamt in the LMHS models of this
filament. More generally for weakly curved filaments, this small effect
is not surprising: it can be explained by the strong alignment of the
magnetic field along the y axis for the high value for the force-free
parameter
needed to produce a filament.
Our previous LMHS models of filaments (Aulanier et al. 1999,
2000) have shown that the parameter a has to be chosen as high as possible
so as to obtain significant departures from the force free state. So
considering Eq. (7), we choose a=1. Since our objective
is to produce a LMHS model that can be compared with the EUV
observations, we only use the THEMIS/MSDP image to constrain the
choice of the two remaining parameters
and H, independantly
of the EUV data.
Following Aulanier & Démoulin (1998), the left bearing orientation
of the filament feet (see Sect. 2.3)
implies positive values
for the force free parameter
.
Five values for
(see Eq. (5)), are considered between 0.88
and 0.98. This interval is chosen by considering previous analytical
studies of the parameter space in which the conditions can be satisfied
for a suitable filament model in a bipolar field, in linear force-free
field invariant by translation (see Aulanier & Démoulin 1998 (Fig. 2)). The minimum value is fixed below the threshold for
which dips are present in z>0, and the maximum value is chosen so
the top part of any resulting twisted flux tube does not reach
unrealistically high altitudes in z (typically D/2), which
is an artifact of linear force free field and LMHS models for
high values of
.
Seven values for the scale-height H of the pressure/gravity
induced horizontal currents are chosen between 5 and 35 Mm, which
correspond to half of the typical height of intermediate filaments
as observed above the limb.
We then perform one LMHS extrapolation for each combination
of
and H, with the boundary conditions defined in
Sect. 3.2, with 512
512 mesh points in x, y. The
magnetic field is calculated up to
z = Dx/2 = 96 Mm, which is above
the typical height of intermediate filaments. Note that the LMHS
method permits us to calculate the magnetic field up to any given height,
provided that the solar curvature and solar wind effects can be
neglected.
From each of these extrapolations, we calculate the resulting
distribution of magnetic dips in the same way as described in Aulanier
(2000), with spatial samplings of
Mm and
Mm, and with a vertical filling of 300 km that
corresponds to one pressure scale-height for typical prominence
temperatures. In this way, we construct a grid of 35 models to be
compared with the
data.
We overlay each model from the grid onto the THEMIS/MDSP data. We consider the shape of the body of the
filament
as the feature to be matched by the 3D distribution of calculated dips.
In the parameter space (
,
H), the models which best fit
the filament body are for
and 20 Mm
Mm.
In these intervals, the models with the lowest values of
(
,
H) reproduce the global shape of the filament body,
but with many gaps (i.e. regions devoid of dips) between the filament
feet. This is because there is neither enough field aligned currents
to produce dips, nor enough effects of the plasma at high altitude
to accentuate them. However for the largest values of (
,
H) the gaps
are filled by the distribution of dips, while at high altitude they
form a structure that is much more aligned with the y axis than the
filament body is. This can be explained by the appearance of a
twisted flux rope which reaches high enough altitudes at
which the neutral line becomes almost aligned with y since the high
spatial frequencies present at z=0 have disappeared (Aulanier &
Démoulin 1998).
Thus, we choose the mean values in the interval, i.e.
(in physical units
m-1) and
H = 25 Mm. With the spatial samplings given in Sect. 3.3 for
the discretization in the calculation of dips, 5600 dips are found in
the computational box.
Figure 3 (top) shows the
image of the
filament overlaid with 3500 low altitude (z<4 Mm) dips and 2100 high altitude (z>4 Mm) dips, drawn up to 300 km from the bottom of
the dip. The high altitude dips match most observed properties
of the filament: the curved shape and the degree of continuity of its
body, as well as the locations and orientations its lateral extensions.
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Figure 3:
Same as Fig. 2, overlaid by magnetic dips calculated
from the LMHS model. 5600 dips are plotted with spatial
samplings of
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Figure 4: Top: view in projection of the same 5600 magnetic dips as shown in Fig. 3. The dark lines are portions of dipped field lines drawn up to a height of 300 km. Bottom: view from the side of the filament. Only the locus of the dips are marked with circles. Units are in Mm. The maximum altitude of the dips varies from 5 to 32 Mm along the filament axis. The stripes on the top panel are due to the discrete sampling chosen for the drawing of magnetic dips (see Sect. 3.3) in which the field is nearly horizontal. This discretization, clearly apparent on the bottom panel, permits to emphasize the magnetic field direction and the projection effects on the top panel. A finer sampling only fills the thin elongated gaps between the dips: it replaces the stripes by a curtain-like black feature, which looks like real filaments/prominences viewed in projection. |
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We have noticed in Sect. 2.3 that the filament body had an "S-shape'' with an elbow. The LMHS model shows that this shape is not due to "sigmoid'' type field lines. The observed curvature is simply due to local deformations of the neutral line by strong magnetic concentrations, with the same polarity than the dominant one on their side of the neutral line. These polarities oppose to the tendency of the filament fields to be aligned along the neutral line. Note however that the presence of a larger scale sigmoid of the coronal loops around the filament (as in the models of Antiochos et al. 1994 and Titov & Démoulin 1999) cannot be ruled out from our model, since the chosen size of our periodic computational box (see Sect. 3.2) does not permit to address this issue.
The observed continuity of the filament body along its axis (see Fig. 2 (top)) appears less straightforward to explain
with the LMHS model, since Fig. 4 (bottom) shows
that the distribution of locus of the dips in the filament body is far
from being continuous, which is also confirmed by calculating dips with
finer spatial samplings in x, y, z. In fact this discontinuous
distribution of dips is not inconsistent with the quasi-continuity of
the
filament. The vertical filling of dipped field lines up
to 300 km also provides an horizontal extension for each dip, which can
go up to 10 Mm. Also in most regions along the neutral line, isolated
patches of dips are well aligned with the direction of the magnetic
field. So the dipped field lines can fill most of the regions devoid
of dips, leading to an apparent continuity of the filament body,
as obtained in Fig. 3 (top). Figure 4 (top) which is a view in projection of the same dips
as shown in Fig. 3, confirms this interpretation. Also
we have checked that this calculated distribution of dipped field lines
matched fairly well the intensity iscocontours of the THEMIS/MSDP
image in the filament.
Several lateral extensions to the filament body, knows as feet or
barbs, are visible on the
data (see Figs. 1 and 2). This property is typical of
filaments,
however as noted in Sect. 2.3, the feet of this filament
are not related to any strong parasitic polarity. Nevertheless, the
LMHS model clearly results in lateral dips which locations and
orientations are consistent with the observed feet (see Fig. 3 (top)). Considering this result, we carefully
examine the underlying magnetic field observed with SoHO/MDI.
Figure 5 shows that magnetic parasitic polarities do
exist in the vicinity of feet (compare with Fig. 2),
but they are at the limit of the instrument sensitivity: they have
very weak field amplitudes of
B|| = 3-10 G. It is likely that
these polarities are not due to the noise since many of them are
extended over 1-10 pixels, even though their maximum value (10 G)
is always located on one single pixel (the pixel size of MDI
is 1.977
). This instrumental limitations may be
responsible for the lower quality of the correlation between
computed dips and observed feet as compared to the filament
model of Aulanier et al. (1999).
Assuming that the MDI is reliable enough for such extended weak fields, we fully confirm our previous results on the interpretation of filament feet in terms of magnetic dips located underneath and next to the filament (Aulanier & Démoulin 1998), their association with photospheric parasitic polarities (as observed by Martin 1990) and their location on the edge of these polarities (as observed by Aulanier et al. 1998b; Wang 2001).
We first emphasize that a large value for H was necessary to produce
a suitable filament model. This implies that plasma pressure and gravity
may not be negligible for the structuring of filaments. However within
the limitations of LMHS models, it is difficult to estimate if
spatial variations of
in non-linear force-free models may
replace or not the effects of plasma induced currents.
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Figure 5:
Close-up of the SoHO/MDI magnetogram of 65 |
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In the present work, a direct extrapolation of the observed magnetogram
used as boundary conditions was done. This contrasts with Aulanier
et al. (1999, 2000) were the magnetograms were modified at relatively
large distances from the filament in order to ensure the presence a
twisted flux rope at z>0 for high values of
.
With this method, we find that the calculated topology for the filament
magnetic field is more complex than a coherent flux rope. Figure 6
clearly shows many interruptions in the filament, manifested by some of
the computed thick field lines which regularly reach the photosphere in
non-parasitic strong polarities, i.e. which have the same polarity as
the dominant one on the side of the neutral line where they are located.
Despite the complex connectivity of the filament field lines at low
altitude, at high altitude they show a global twist of
turn in the computational box. Assuming that the twist per unit length
does not vary within the whole
filament (which is about 245
Mm long), the averaged twist of the portion of the flux tube where the
filament material is visible is
.
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Figure 6:
Magnetic field lines computed from the same LMHS model as in Fig. 3. The field lines passing through the
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It is worth mentioning that the total twist of the full filament flux tube may be more than 0.6
for the following reasons. Firstly, the filament ends as observed in
may not correspond to the footpoints of the flux tube. This
effect would increase the number of turns to
,
with an increase which is likely to be
.
Secondly the
EFC as observed by EIT is much longer than the studied
H
filament. Figure 1 (bottom) even shows that
it may follow the switchabck which links EFC1 in the active region AR1.
It is impossible to know if the full EFC corresponds to one single
flux rope or not. If it does, assuming a constant twist per unit length
and taking into account the length of EFC1 as well (which extends the
EFC length to about
), we estimate an upper bound for
the total twist of
.
In summary, we find that the length for one turn is
Mm,
with an average flux tube radius projected onto the (x, y) plane of
Mm (see Fig. 6 (top right)). Assuming
a circular cross-section of radius R for the filament flux tube,
the ratio between the toroidal field
and the axial field
is then
.
Even though LMHS models do not address the mechanism of
formation of plasma condensations in magnetic dips (see e.g. Poland
& Mariska 1986; Antiochos et al. 2000), they calculate higher
densities in dips than in classical arcades, since the LMHS
equation for the density (Low 1992):
However this method is an approximation, therefore it should not be
considered to measure quantitative densities. For this reason, we
need to estimate separately the amount of mass which is likely to be
present in the dips, whose positions only are reliably calculated with
the LMHS model. We have shown in the present and in previous
filament models (Aulanier et al. 1999, 2000) that a vertical filling
of magnetic dips of 300 km was consistent with the visibility
of absorbing plasma as observed in
.
However in order to
simulate observations in other absorbing wavelengths it is necessary
to calculate different filling heights of magnetic dips to account for
their different opacities as compared to
.
In this section we discuss a simplified 2D model which permits, under several approximations, to estimate the vertical filling of magnetic dips as observed when a background EUV radiation is absorbed by the Lyman continuum of hydrogen (P. Heinzel, private communication).
We consider a 2D vertical distribution of identical dips in the
(x, z) plane, where z is the altitude above the photosphere
as well as the line-of-sight. We take Lz for the vertical extension
of this distribution of dips. Then we fill each of these dips
by dense plasma, which can absorb background radiation
emitted from below at the wavelength
.
We further assume
density isocontours in the (x, z) plane of the form x= constant.
In such a configuration, the optical thickness
for
the wavelength
is given by:
Taking two different positions along a given dipped magnetic
field line (or along the x axis) corresponding to two plasma
densities
and
chosen so
as to obtain the same visibility (i.e. optical thickness) in both
wavelengths
and
,
then Eq. (9)
leads to:
But for two different plasma densities (i.e.
and
), the value for the ratio
is difficult to
estimate, because:
With this simplification it is possible to evaluate
for a given
plasma density. Considering two wavelengths
and
and for one given position along x in the vertical distribution of
dips (so at fixed density
), then Eq. (9) leads to:
Since we now have an expression which only depends on the
ratio, we
can use the results from Heinzel et al. (2001), who computed with NLTE
models an opacity ratio of
-100
for T=8000 K and
-1. In order to evaluate the
maximum effect of the opacity for the observable filling of dips, we take
the maximum value for
.
So we estimate
km.
Note that for a EUV line emitted at
Å,
a factor
/912)3 has to be multiplied to
to obtain the opacity ratio between this
line and
(see e.g. Chiuderi Drago et al. 2001; Heinzel
et al. 2001). In the case of the
O V line observed by CDS (see Sect. 2.1),
.
Taking this modification into account, Eq. (14) leads to z(O V)
.
In the present 2D isothermal and hydrostatic model, the effect
of
is small due its logarithmic expression. So in the
following we neglect this effect because the precise estimation
of the value for the vertical filling of dips is likely to be
more sensitive to the other approximations listed above.
It is only at this stage that we overlay the CDS image in
O V (629.73 Å) with the magnetic dips of the LMHS model
of the
filament, as calculated in Sect. 4.1
but now computed up to height of 1700 km as estimated in Sect. 5.2. This overlay is shown in Fig. 3 (bottom). Despite the limitations of the LMHS model and
the strong approximations for the estimation of the filling of dips,
a striking good match is found between the dark EUV regions and
the projected distribution of dips onto the plane of the observations.
Figure 3 (bottom) shows that a nearly one to one
correspondance is obtained.
Apart for the central filament itself, which is nearly undistinguishable from the rest of the EFC, most of the dark regions located aside of the filament correspond to the locus of low lying magnetic dips, located above the photosphere and below 4 Mm in altitude. The horizontal extension of these dips can at some places reach 10-20 Mm, which permits the filling of most of the dark regions, parallely to the local magnetic field direction. Among all the reproduced dark regions, note in particular the long and thick South-Western extension from the filament, the inhomogeneous structure located along the filament on its South-Eastern side only and several "ring-shaped'' regions connected to the Northern part of the filament.
![]() |
Figure 7:
Summary of the LMHS model. It shows the relation between
the topology of the magnetic field and the location of the plasma
condensations in and around the filament, which absorb the
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This suggests that wide EFCs have the same nature as the
filament: they are composed of suspended (
)
magnetic
dips in which plasma condensations are present. If the typical temperatures
in these condensations are those of prominences so that neutral hydrogen
can be present, the good match between the LMHS dips and the EUV
data supports the absorption interpretation (see Sect. 1).
Moreover, the distribution of dips in the EFC far from the filament
are weakly extended in altitude. This is opposite to the filament
body and feet in which more dips are integrated along the
line of sight. Since these low altitude dips are not correlated with
any obvious
feature, the LMHS model is qualitatively
consistent with opacity ratios calculated by Heinzel et al. (2001).
We have discussed in Sect. 3.3 how the periodicity effects along y only weakly affect the calculated magnetic dips. However it is obvious that this periodicity does not permit to calculate the connectivity of long field lines which come out of the computational box. Despite of this limitation, the LMHS model clearly shows that the dips of the EFC are formed within the lower parts of long sheared arcades that overlay the filament flux tube (see Fig. 6). So the dips in the extended EFC are not located in field lines which belong to the filament flux tube: its radius projected onto the (x, y) plane is too small to cover the full width of the EFC.
As for the filament feet observed in
(see Sect. 4.3), every dip in the EFC is associated with
weak photospheric parasitic polarities located between stronger magnetic
polarities of the network. In particular, the South-Western elongated
left-bearing extension of the EFC which is very well matched by
magnetic dips (as described in Sect. 5.3 and shown in
Fig. 3 (bottom)), is clearly associated with
extended and dispersed weak negative polarities (as shown on the
right portion of Fig. 5).
The local topologies of the magnetic field around each of these polarities are all the same: field lines tangential to the photosphere are present on one edge of each polarity, so forming "bald patches'' (as defined by Titov et al. 1993). Direct representation of the computed topology is difficult since it involves a combination of large and small scales, so we refer the reader to Bungey et al. (1996) and to Aulanier et al. (1998b (Figs. 2a and 6a)) where this topology was calculated for theoretical models.
The chirality and the magnetic topology (see Sects. 2.3
and 5.4) of the laterally extended regions in the studied
EFC are exactly the same as what we found for filament feet observed
in
(Aulanier et al. 1999, 2000). Therefore, in order to
homogeneize the terminology of physically similar solar phenomena as
observed in different wavelengths, we suggest to redefine the wide
extended regions of EUV filament channels as the "EUV feet''
of their central filament.
Even if the large filling of each dip plays a non-negligible role
in the broadening of EFCs, the contribution of EUV feet
is obviously dominant. For example, the longest extended foot described
in Sect. 5.4 is about 100 Mm long and its maximum
width near the neutral line is about 50 Mm. Also, the EUV broadening
of the Eastern part of the
filament occurs on its Southern
side only. Both these examples, as well as the observed "ring shaped''
dark regions, are clearly incompatible with the single contribution
from the large filling of dips. The frequently observed degree of
inhomogeneity near the boundaries of EFCs (see Sect. 2.3) becomes readily interpreted by the inhomogeneous
distribution of parasitic polarities in decaying active regions,
which is consistent with the SoHO/MDI magnetogram (see Fig. 5).
It follows that any EFC related to an active region filament should be narrower and more homogeneous than those related to intermediate and quiescent filaments. Also EFCs in any active region should progressively broaden and become inhomogeneous, as the active region emerges and decays during several solar rotations. This is fully consistent with observations of the long term evolution of active regions (van Driel-Gesztelyi 1998 (Figs. 1 and 2)). We would also like to mention that our results on this studied EFC are also fully consistent with the recent He II (at 304 Å) and magnetic observations of Wang (2001) of several filaments, despite Wang's claims (in his Sect. 7) and his cartoon interpretation (in his Fig. 8).
A schematic which summarizes our results of our interpretation of
and EUV observations is shown in Fig. 7.
We emphasize that this schematic is not a cartoon. It displays the results
of the calculated 3D LMHS model in simplified way, so that large and
small scales can be visualized in one single frame and so that each
feature is clearly identifiable.
The topology of the magnetic field as calculated with the 3D
LMHS model was discussed in Sect. 4.4. We have
shown that in spite of several partial interruptions by photospheric
magnetic concentrations that have the same polarity as the dominant
one on the side of the neutral line where they are located, the
filament flux tube is twisted by less than one turn for the length
of the filament as observed in
.
On one hand, the lower portions of the magnetic field lines rooted in
these non parasitic polarities are not associated with any observed
filament feet. On the other hand, no field line from the
filament flux tube reach the z=0 plane inside parasitic polarities.
In great majority, the field
lines rooted in parasitic polarities are connected to the same side of
the neutral line by small arcades, while a few are connected to the other
side of the neutral line by flat arcades underlying the filament
flux tube. So our LMHS model is opposite to the conceptual
interpretations by Martin et al. (1994) and Wang (2001), which propose
that filament bodies and feet are formed in classical undipped arcades.
Assuming that the filament flux tube is not much longer than the
filament (about 245 Mm), its moderate amount of twist
(
-1) makes the LMHS model consistent both
with weakly twisted flux rope models (e.g. van Ballegooijen 1999;
Amari et al. 1999 (Fig. 2); Titov & Démoulin 1999) and with differentially sheared arcade models (Antiochos et al. 1994; DeVore
& Antiochos 2000). But if the flux tube links the studied filament
with F1 in AR1 (see Fig. 1), then its length (about
)
and number of turns (
-4) would make it
more consistent with the flux rope models of filaments in
switchbacks (van Ballegooijen et al. 2000; MacKay et al. 2000).
But whatever is the total length of the flux tube, its ratio
makes the LMHS model inconsistent
with flux ropes in which the poloidal and the axial field magnitudes
are comparable (see e.g. Amari et al. 1999 (Fig. 3); Gibson
& Low 2001).
Finally, we wish to emphasize that views in projection, both of the
dips only (Fig. 4 (top)) and of the full field lines
(Fig. 6 (bottom)) do not permit us to identify the calculated
weak twist, which is consistent with most
observations of
filaments. Also these projections show that the magnetic dips become
more and more shallow as the altitude increases in the filament.
Under the present limitations of observations of flows in filaments,
using Doppler measurements and/or high cadence filtergram observations,
our numerically calculated magnetic field is also consistent with
and EUV observations of dynamic condensations
as observed on the disc or at the limb (see e.g. Malherbe et al. 1983; Schmieder et al. 1991; Zirker et al. 1998; Wang 1999).
Our calculated LMHS model predicts that, apart from the top of the prominence body where the magnetic field is nearly flat, any given dynamic condensation cannot move all along the prominence body and feet due to the total depth of their dips (J. T. Karpen, private communication). To the authors' knowledge, this remains to be tested by observations.
The
filament structure is undistinguishable in the EUV observations. But the consistency found between the hydrostatic
filling of magnetic dips (Sect. 5.2) and the observed
EUV feet (Sect. 5.3) suggests that the calculated
filling of dips may also hold in the filament body. Consequently, plasma
condensations in filaments may also be as long a 10-20 Mm. This is a
challenge for coupled radiative and thermodynamic models of plasma
condensations in magnetic dips (Poland & Mariska 1986; Antiochos
et al. 2000; Heinzel & Anzer 2001). While these elongated condensations are not completely observed in
for filaments on the disc (due to the opacity of
,
see Heinzel et al. 2001), they may be observed in other wavelengths
(not only in EUV) and/or above the limb in prominences.
Under such different observable conditions and following Sect. 4.2, these elongated dips may fill some gaps that
are frequently observed in filament bodies in
.
This may play a role in interpreting observations
of prominences at the limb which show different patterns as
observed in different wavelengths (see e.g. Kucera et al. 1998;
Wang et al. 1998).
Our co-aligned observations (see Fig. 2) reveal that
EUV feet are not always related to
feet. From the
LMHS modeling, this can be explained and generalized to every
EFC. It is obvious that any given
foot should always
be located inside a EUV foot, in particular close to the filament
body. Also, the absence of a EUV foot at some given location
naturally implies the absence of any
foot at the same place.
But far from the filament, long
feet (or dark fibrils) will
only be observable co-spatially with EUV feet if the size and
flux of the related parasitic polarities is strong enough and if the
arcades overlaying the filament are sufficiently inclined toward the
photosphere, so that the vertical distribution of low lying dips
responsible for the EUV absorption will be thick enough (along
the line of sight) to sufficiently absorb
radiation so
that an observable contrast with the chromospheric background can be obtained.
We calculated several linear force free models (a=H=0) in the same
box as defined in Sect. 3.2, and we compared the distribution
of dips with the EUV images (see Fig. 8). We found
that for increasing values of
from 0 (potential field) to
,
the orientation of the calculated dipped field line
progressively tends to align with the neutral line direction, and also
that their vertical extent slightly increases.
![]() |
Figure 8:
Same as Fig. 3 ( bottom) but here the dips are
calculated from ( top) a potential field extrapolation
(
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In the absence of pressure and gravity effects, we find that no dip
can be matched with the
filament for
,
because in this case the magnetic shear is not sufficient to create the
weakly twisted flux tube above the neutral line responsible for high
altitude dips. Even with
,
some portions
of the complex structure of the EUV dark regions can still be
matched. This is natural because
has a weak effect on the
small parasitic polarities responsible for the low lying dips, because
they correspond to high spatial frequencies in x and y (Aulanier
& Démoulin 1998). But the edges of the EFC
are poorly reproduced, and the distribution of low lying dips is
too dispersed to match the observed degree of homogeneity of the
EFC. This dispersion is mainly caused by the unability of
dipped field lines to fill the gaps between separated patches of
dips, because for
the conditions given in
Sect. 4.2 are not satisfied.
So we predict that dark EFCs with wide EUV feet can be observed, even when no filament is present. This holds not only when prominence material is unobservable in some given wavelength, but also when there is no magnetic configuration capable of supporting any prominence condensation at high altitudes.
This is consistent with the existence of
filament channels
without filaments (see e.g. Martin 1990), but for different physical
reasons: around a given neutral line, the presence of an
filament channel simply indicates a large amount of magnetic shear,
whereas the presence of an EFC mostly indicates the presence
of low lying magnetic dips, for which the magnetic shear is not as
important as the distribution of dispersed weak photospheric
parasitic polarities.
Considering low spatial resolution observations at different EUV
wavelengths, the absence of a filament may be difficult to detect in
a given EFC, because of typically high opacities not only in the
Lyman continuum of hydrogen, but also for other wavelengths in which
filaments are typically observed (e.g. Ly
): with high opacities,
no difference can be observed between thin layers of low lying dips or
thick layers such as filaments. However, if isolated fine structures
exist within EFCs, high spatial resolution observations may
permit to deduce the presence of a filament both through the degree
of homogeneity of the EFC and through the orientation of the
related fine structures.
Since the magnetic dips which form the lateral extensions of
filaments are very shallow (about 10-20 Mm long for 1700 km high)
and are formed at low altitude (
Mm for EUV feet,
and about twice as much for
feet), plasma injection into
these dips may be very easily achieved through simple MHD effects
which may not involve complex thermal processes as required for the
formation of prominence condensations at much higher altitudes (see
e.g. Poland & Mariska 1986; Antiochos et al. 2000).
One possibility is shear Alfvèn waves driven by photospheric motions. They can easily lift up chromospheric material along the magnetic field, which will eventually get trapped in the suspended dips. Another possibility arises from the bald patch topology that we computed. Magnetic reconnection in the bald patch separatrix can provide the direct filling of higher and higher dips by chromospheric material as reconnection proceeds. Note that this process differs from the reconnection scenario of Wang (1999, 2001), which aims at producing dynamic condensations in undipped field lines.
It should be mentioned that the possibility of magnetic reconnection in bald patches was debated by Karpen et al. (1991) due to the thickness of the photospheric layer, but counter-arguments were provided by theory (Low 1991; Billinghurst et al. 1993) and by models of observed flares (Aulanier et al. 1998a) and fibrils (Mandrini et al. 1999). Note that in the case of filament channels, the reconnection scenario in bald patches is also supported by Kucera et al. (1999), who reported isolated bright EUV features located on the side of a filament and observed in Si IV, which were correlated with calculated flux tubes rooted in bald patches, and which were interpreted as magnetic loops heated by reconnection and filled by chromospheric evaporation.
Even though a bald patch reconnection model appears consistent with
some observations, it will have to be tested with new observations and
models. In particular the issue of heating of the chromospheric plasma
will have to be addressed, since EUV absorption by the Lyman
continuum of Hydrogen requires cool temperatures (
K).
In the O V line at 629.73 Å only, a peculiar bright elongated continuous spine is observed in the central part of the EFC (see Fig. 2 (bottom)). We conjectured in Sect. 2.3 that this spine could be interpreted as the upper prominence corona transition region (PCTR) of the filament. We examine below this possibility.
Careful examination of the overlay of the
image with the
modeled dips (see Fig. 2 (top)) reveals that
at some places the uppermost dips in the filament body are shifted
from the center of the
filament. We have confirmed that
theses shifts were due to projection effects in the complex thin volume
which forms the filament body. Also, Fig. 2 (bottom)
shows that the same uppermost dips are well co-aligned with
the bright O V spine. So it is very likely that this spine
is the result of EUV emission from the uppermost dips, which
cannot be absorbed at higher altitudes since there are no higher
dips. So the LMHS model is consistent with an upper
PCTR interpretation for this O V spine located on top
of the filament.
The distribution of dips in 3D (see Fig. 4) shows that the altitude of the uppermost dips strongly varies non-monotonically between 5 and 32 Mm along the filament body. This suggests that the observed continuity of the O V spine is an artifact caused by projection effects. With the LMHS model, the spine is consistent with the emission of several discrete upper PCTRs which are associated with different magnetic dips at various altitudes, which belong to different magnetic field lines. This result may have strong implications for multi-dimensional radiative transfer modeling of prominences.
During the filament eruption, the field lines forming its main flux
tube (described in Sect. 4.4 and shown by thick lines in
Fig. 6) will expand dynamically. Regardless of the EUV
feet, the large vertical filling of hydrostatic dips by 1700 km, which
is about 5.6 pressure scale heights, implies that the filament body could
be about 50% more massive than what can be measured in
.
This extra mass, which can be observed in EUV as opposed to
,
will naturally be loaded into the associated coronal
mass ejection (CME). For the specific class of "three-part
CMEs'' that incorporate a leading front followed by a cavity
which surrounds a bright core, this extra mass should be confined
on the edges of the bright core, since the latter corresponds to
the erupting filament (see the review of Low 2001).
The relative number of calculated low/high altitude magnetic dips (see Sect. 4.1) suggests that there can be at least the same amount of mass in EUV feet than in their related central filament, but located at low altitudes, in thin volumes on top of which the filament stands (see Figs. 4 and 7). A fully time-dependant MHD simulation of the eruption of the studied filament (or any other) would be required to study quantitatively the role of its EUV feet in the mass loading of the CME. This is far beyond the scope of this paper, however it is still possible to infer the evolution of the EFC as its filament erupts through simple argumentations.
The filament flux tube expansion described above will push up, or
aside, the overlaying sheared arcades (shown by thin lines in Fig. 6), as typically calculated by 3D MHD simulations of
erupting flux ropes (see e.g. Amari et al. 2000 (Fig. 3)).
The top parts of the arcades that will be pushed up will eventually
be injected into the CME all together with the filament flux tube.
The bottom parts of these expanding arcades, in which the low-lying
dips which form the EFC are located (see Sect. 5.4), whether they are pushed aside or injected into the CME, are likely to be affected by the eruption in the following
way: each cool condensation of the EFC will remain at low heights if
its pre-eruptive dip is maintained, or will fall down to the chromosphere
along the field if its pre-eruptive dip is straightened. These two
possibilities arise from the competition between the tendancy of
field lines to become quasi-vertical due the field opening and the
flux of the parasitic polarities that tends to keep the field lines
locally bent toward the photosphere at low altitude. After the
expanding phase, the open field lines will close back through reconnection,
loosing a fraction of their magnetic shear, i.e. lowering the value of
in the linear force free field approximation.
This likely scenario, which still needs to be confirmed by time-dependant
simulations, predicts that the mass of the wide low-lying EFC,
i.e. of the EUV feet, will not contribute to the CME
when the filament erupts. It also predicts that an EFC can be
partly or nearly fully maintained after its filament eruption, since
even a strong decrease of
does not remove all the low lying
dips that are responsible for the EUV absorption in the EFC
(see Sect. 6.3).
Wide EUV filament channels have been frequently
interpreted by the Hydrogen Lyman continuum absorption of EUV lines
shortward of 912 Å in cool massive condensations (Orrall & Schmahl
1979, 1979; Chiuderi Drago et al. 1998, 2001).
Heinzel et al. (2001) and Schmieder et al. (2002)
have also shown that these EUV channels are much more
extended as compared to their main
filament.
The object of this work was to propose, through a case study,
a general physical model for EUV filament channels, and to address
their role in the mass loading of coronal mass ejections (CMEs),
which is an important issue for estimating their kinetic energies.
We calculated in 3D the magnetic field in and around one observed
filament, with the linear magnetohydrostatic (LMHS) extrapolation
method (Low 1992; Aulanier et al. 1998a).
The model was built from a SoHO/MDI magnetogram so as to match
the
observations from THEMIS/MSDP, independantly of
the EUV data from SoHO/CDS.
We fully confirmed our previous results on the magnetic structure of
filament
feet in terms of magnetic dips (Aulanier & Démoulin 1998; Aulanier et al. 1999, 2000). We also found that the observed
continuity of the filament
body was ensured by the filling
of gaps between isolated patches of dips by their horizontal extension
due to their vertical filling by plasma up to 300 km. We found a
complex topology for the filament flux tube, in which a global twist
of about 0.6 turn could be identified.
Then we compared the LMHS model with the observed EUV filament channel (EFC). A striking one to one correspondance was found between the EFC and the distribution of every calculated magnetic dip. The joint analysis of the model and the data proved the presence of plasma condensations which can potentially absorb the background EUV radiation. Also this analysis revealed their location, magnetic nature and likely evolution when the filament erupts. The results, which have been sketched in Fig. 7, can be summarized and generalized as follows:
The absorbing condensations in EFCs are formed where the magnetic
field is dipped, in the lower
1700 km portions of their field
lines. In the central parts of EFCs, the dips are the same than
those forming the filament body and feet as observed in
.
In the wide lateral extensions of EFCs, the dips are formed above
dispersed photospheric parasitic polarities and are grouped in thin layers
at low altitude (0
4 Mm, where z=0 is the altitude
of the MDI magnetogram). As for
features, the
vertical filling of dips provides the observed degree of continuity
in EFCs. So the physical properties of EUV extensions
are very similar to those of
feet, but both are not necessarily
co-spatial. In order to homogeneize the terminology for solar
phenomena that have the same physical nature, we redefined the wide
extensions of EFCs by "EUV feet''. The 3D distribution of
dips is qualitatively consistent with the respective visibility of these
structures in
and in EUV as derived from the opacity
ratios calculated by Heinzel et al. (2001) from the NLTE radiative
transfer models.
These findings on the magnetic nature of EFCs and the calculated
coronal magnetic field led us to discuss several implications. We proposed
a possible scenario for plasma injection in the low-lying dips of EUV
and
feet through magnetic reconnection in bald patches.
We have shown that EFCs could exist in the absence of the high
altitude magnetic configuration capable of supporting cool material, so
in the absence of filaments. We have also shown that the apparently
continuous O V bright spine, located at the center of the EFC,
could be interpreted as the emission from several isolated upper
prominence-corona transition regions (PCTRs). We have shown that
each upper PCTR was located ontop of the uppermost filament magnetic
dips, at various altitudes and in different magnetic field lines, depending
on their position along the filament axis.
During a filament eruption, some of the mass of the filament body is
known to be injected into the CME. The ratio for the filling of
the dips by cool (
K) hydrostatic material as observed
in
and in EUV suggests that this ejected mass should
be
1.5 times larger than what is estimated from
observations of filaments. Since this mass is located within the
outer regions of each dip of the filament flux tube, its location
in the propagating CME should remain on the edge of the main
erupting prominence. But the topology of the coronal
magnetic field in and around EFCs implies that the large amount
of mass contained in their wide low-lying EUV feet will not be
loaded into their associated CMEs. We calculated that after a
CME, the loss of magnetic shear in the corona will not remove
all the low lying dips, even if the potential state is reached.
So wide EFCs should be partly maintained, even right after
their filament has erupted and before it eventually reforms.
We have shown that the morphology of EFCs is the same
when observed in several transition region and coronal lines whose
wavelengths are shortward of 912 Å as recorded
by SoHO/CDS, but also in lower wavelengths such as 304 Å
(He II) and 195 Å (Fe XII). It naturally follows
that our interpretation of filament channels observed in these wavelengths
should also be valid. In this case, the absorption by the continua of He I (
Å) and He II
(
Å) must be taken into account, as shown by
Mein et al. (2001) for emerging arch filament systems.
Observations in these EUV wavelengths are typically done by
SoHO/EIT and by TRACE. Also they will be provided by
STEREO/SECCHI/EUVI with the unprecedented capability of doing
stereoscopic observations. So in terms of morphology, these instruments
will be well suited to test further our interpretation and our
predictions. However EUV spectroscopy will be needed
to obtain more quantitative estimates of the mass in filaments
and in their channels.
Acknowledgements
We thank P. Heinzel and K. Tziotziou for their critical comments and their help in the writing of Sect. 5.2. We also thank J.-M. Malherbe and P. Mein for their assistance with the THEMIS observations, as well as P. Démoulin, L. van Driel-Gesztelyi, J. T. Karpen, J.-C. Vial and Y.-M. Wang for stimulating discussions. We are grateful to the MEDOC and the THEMIS staff for having conducted the coordinated observing campaign from which the CDS and the MSDP data used in this paper were obtained. We also thank the EIT and MDI consortiums as well as the French solar database BASS 2000 for providing the other data used in this paper. The THEMIS telescope is operated by INSU/CNRS (France) and CNR (Italy) on the island of Tenerife in the Observatorio del Teide of the IAC (Spain). SoHO is a project of international cooperation between ESA and NASA. The work of G.A. was funded by the Centre National d'Etudes Spatiales (CNES).