A&A 383, 697-705 (2002)
DOI: 10.1051/0004-6361:20011734
I. Roussev1,2 - K. Galsgaard3
1 - High Altitude Observatory, NCAR, 3450 Mitchell Lane, Boulder,
CO 80301, USA
2 -
Armagh Observatory, College Hill, Armagh, BT61 9DG, N. Ireland
3 -
University of St. Andrews, School of Mathematics and Statistics,
North Haugh, St. Andrews, Fife, KY16 9SS, Scotland, UK
Received 1 August 2001 / Accepted 4 December 2001
Abstract
We synthesise three resonance transitions of Li-like ions, C IV
1548.2 Å, O VI 1031.9 Å, and Ne VIII 770.4 Å, based on the MHD
experiments presented in Part I of this study. Part I involved 2D MHD modelling
of magnetic reconnection events in stratified magneto-hydrostatic atmospheres
selected to represent a ``quiet'' Sun transition region environment. Here in Part II,
we discuss some observable consequences of these simulations by including effects
of non-equilibrium ionization in a 1D approximation. All spectral line syntheses
are done along a particular ray, oriented vertically along the initial current
structure. Computed time-series, in the three spectral lines, reveal both blue- and
red-shifted Doppler components. It is found to be easier to detect the reconnection
event in the various emission lines as strongly Doppler-shifted components as the
stratification increases. We predict what the observational consequences of these
reconnection events would be, if various spatial resolutions under 1 arcsec become
available in future observations. This work is a continuation of previous numerical
studies related to solar explosive events.
Key words: MHD - Sun: atmosphere - Sun: transition region - Sun: UV radiation - line: profiles
Recent studies have presented 2D MHD simulations relevant to the ''quiet'' Sun explosive events based on magnetic reconnection models (Jin et al. 1996; Innes & Tóth 1999). They suggest the blue- and red-shifted Doppler components observed during explosive events are observational consequences of bi-directional outflow jets produced by an ongoing magnetic reconnection. All of these computations, however, involve equilibrium ionization of the emitting plasma. This is an assumption that is unlikely to represent the actual physical situation.
Parallel progress in computing resonance transition region lines under the consideration of non-equilibrium ionization was made in the 1D HD simulations of Sarro et al. (1999). This study was aimed at examining changes in the C IV 1548.2 Å transition region line, as a dynamical response to small-scale energy depositions placed at different heights in a 1D coronal loop. The results obtained were (ambitiously perhaps) interpreted as explosive events. Since these simulations involved a different physical mechanism to explain the nature of solar explosive events, the final results were also different, when compared with the 2D reconnection experiments of Jin et al. (1996) and Innes & Tóth (1999). Nevertheless, it has become clear that the consideration of non-equilibrium ionization is a necessary issue in any numerical study aimed at modelling solar explosive events.
In a series of related investigations, Roussev et al. (2001a,b,c,d) explored the
dynamical response of various physical conditions, that loosely represent a ``quiet''
Sun transition region environment, to a magnetic reconnection event. These
investigations were intended to model solar explosive events using 2D MHD, and
involved model situations ranging from unstratified physical configurations
(Roussev et al. 2001a,b,c), to such where the effect of solar gravity was taken
into consideration (Galsgaard & Roussev 2002; hereafter referred to as Paper I).
It is important to note we did not try to model a realistic solar transition region.
Instead, we allowed our flux tubes to have small temperature gradients, and in this
way modelling like cool loops. In a recent study based on SUMER observations, Landi
et al. (2000) presented new evidence that the emission from the ``quiet'' Sun
transition region (at
K) is dominated by cool loop
structures. These are clustered across the network boundaries where solar explosive
events tend to occur.
The numerical modelling in our previous studies involved 2D dissipative MHD, including effects of the nonlinear field-aligned thermal conduction, radiative losses, and volumetric heating. Furthermore, time-series in two resonance transition region lines, namely C IV 1548.2 Å and O VI 1031.9 Å, based on the 2D MHD results discussed in Roussev et al. (2001a,b), were computed and presented in Roussev et al. (2001c). These were obtained under the consideration of non-equilibrium ionization (Non-EI) of the emitting plasma. It was found that the observational consequences of reconnection events are strongly dependent on the actual initial physical conditions, though the general dynamics of these events was similar.
The present study is a continuation of Paper I, and is dedicated to examine the observational consequences of the reconnection events discussed there. These studies are more consistent than the ones in Roussev et al. (2001a,b,c), since here the effect of gravity has been taken into account, and thus the models represent a stratified atmosphere. All the computations presented here are based on the MHD experiments discussed in Paper I, and involve the necessary consideration of non-equilibrium ionization (Non-EI). The final results on the line synthesis are presented as time-series in C IV 1548.2 Å, O VI 1031.9 Å, and Ne VIII 770.4 Å, transition region lines, respectively.
As a ``blue-print'', we first present the set of experiments to be analysed here. This is done in Sect. 2. We then discuss the departures from the equilibrium ionization that are found to take place in the experiments examined in Paper I. Results for this part of our study are summarised in Sect. 3. The line synthesis in the above three spectral lines is presented in Sect. 4, and final conclusions are drawn in Sect. 5.
We examine the observational consequences of the reconnection events discussed
in Paper I and concentrate on experiments ``G1'' and ``G5''. These represent two
extreme cases. The most rapid decline of the initial physical quantities with
height is exhibited by the ``G1'' case, while a most gradual decline is present
in the ``G5''. We found significant differences in the dynamics of the magnetic
reconnection in the two cases. The main conclusion was that the degree of
stratification influences the complexity of the reconnection event, with the
strongly stratified physical conditions requiring much longer time to reach a
steady state reconnection.
| Physical quantity | Notation | G1 | G5a | G5b |
| Length, 108 cm | L0 | 1.5 | 1.5 | 1.5 |
| Alfvén Velocity, 107 cms-1 |
|
0.915 | 0.915 | 1.293 |
| Time, s |
|
16.4 | 16.4 | 11.6 |
| Gravity, 104 cms-2 | g0 | 2.7 | 2.7 | 2.7 |
| Density, 10-14 g
|
10.04 | 10.04 | 5.02 | |
| Temperature, 105 K | T0 | 0.5 | 0.5 | 1 |
| End Time, s |
|
119 | 82 | 49 |
Since the C IV 1548.2 Å, O VI 1031.9 Å, and Ne VIII 770.4 Å,
transition region lines, have different temperatures of formation, it proved
necessary to perform two additional experiments similar to ``G1'' and ``G5'', but at a
lower normalised temperature
,
K. This highlights the arbitrary choice of
the initial conditions that can be made in our exploratory experiments, and in
this sense all experiments presented here are ad hoc.
This paper discusses three of the experiments that have been carried out. The first
one refers to experiment ``G1'' presented in Paper I, where
K
is chosen as the reference temperature. The other two are based on experiment
``G5'', where T0 values of
K (experiment ``G5a''),
and 105 K (experiment ``G5b'') are assigned. A listing of the normalisation units
adopted in the three experiments is given in Table 1, including the time in
physical units,
,
at which each experiment ends.
In order to perform the line synthesis, we choose the line-of-sight to be the
jet symmetry axis,
,
along which the maximum flow velocities are reached
during the reconnection events. This is vertically along the initial current
concentration. We then average the 2D MHD solution over three widths symmetrically
across the current sheet. This way, 1D MHD solutions which represent spatial
regions of bin-size of 0.1 arcsec (
), 0.5 arcsec
(
), and 1.0 arcsec (
)
straddling the symmetry axis are obtained. The 1.0 arcsec bin size completely
covers the two reconnection jets in the ``G5'' experiments. The motivation to examine
bins of various spatial extents is to determine the observational response if various
spatial resolutions of a spectrograph under 1 arcsec are available during
observations.
The deriving of the binned data is done using a simple averaging in the horizontal
direction. This approach can naturally be questioned as the final result of the
analysis are the relative line intensities of the three spectral lines. In observations,
the measured intensity represents the emission measure, which is proportional to the
line-of-sight integral of the density square for an optical thin line. One could
therefore suggest to use a density square weighting of the data instead. A problem
with this approach is that we, from a single spectral line, can not deconvolve the
intensity information and obtain reliable spatial and temporal information of the
physical properties of the emitting plasma. Such information may only be obtained
if a full spectrum is simultaneously ``inverted''. A process that is by no means
simple. The approach we have used to derive the spectral information requires knowledge
of the physical properties along the line-of-sight to derive the distribution of ions
in different states. This information is then integrated along the line-of-sight to
produce the actual line profiles, which then includes a density square weighting.
Taking this approach, then the simple averaging of the data in the horizontal direction
gives the simplest and most sensible weighting of the physical quantities. Therefore,
the most appropriate type of averaging one would use to derive various results depends
on the approach used to obtain the final result.
![]() |
Figure 1: Images of the relative ion populations of C IV (left), O VI (middle), and Ne VIII (right), as a function of time (from left to right), and position along the line-of-sight (from bottom to top), respectively. The upper panels refer to the case of equilibrium ionization, while the bottom ones correspond to non-equilibrium ionization. These are shown to assess the departures from equilibrium ionization that take place in experiment ``G1'' using Bin III averaging. The dynamic range of initial temperature (at t = 0 s) along the line-of-sight is shown in the upper left panel. |
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As inferred from our previous studies (see Roussev et al. 2001a,c), the
assumption of equilibrium ionization (EI) does not apply to the physical
conditions involved in the reconnection events examined there. Bulk motions
and gradients in the physical conditions produce dynamic time-scales that are
short compared to the ionization and recombination times of the emitting
plasma
. Thus, it is necessary to compute time-dependent
ion populations.
The number density, Ni, of a given ion, i, can be obtained by solving the
following system of partial differential equations
A numerical code (``Non-EI'' code hereafter) has been developed for the purposes of
solving Eq. (1) in 1D, where
by assumption. The ionization and recombination coefficients adopted in this code
are those given by Arnaud & Rothenflug (1985). At each time-step, t = tj, all
quantities on the right-hand side are known, and Eq. (1) is integrated explicitly to
find the solution at a new time-step,
t = tj+1. The initial populations of oxygen,
carbon, and neon used to run the ``Non-EI'' code are calculated assuming EI. This is
consistent with the equilibrium assumptions made for the initial state.
We examine experiment ``G1'' (with a bin-size of 1.0 arcsec) which has the longest
dynamic time-scales of all our experiments
. The relative ion populations
,
,
and
are shown in
Fig. 1, computed from the 1D version of Eq. (1), and in the ionization
equilibrium approximation (upper panels). For each ion, relevant images in the two
cases are scaled using the same dynamic range. The adjacent grey-scale bar represents
the translation table of value versus degree of grey-scale. From bottom to top on each
image (along y), the initial temperature (at t = 0 s) ranges from 0.87 to
K. At the location of the ad hoc diffusion region (placed at
y/L0
= -0.5), the temperature is
K. Since the temperatures of
formation
of C IV, O VI, and Ne VIII resonance lines
are approximately 1.0, 3.2, and
K, respectively, one would expect
to encounter an initial situation like that shown in Fig. 1. The peak values
of
,
,
and
,
are reached at spatial locations
y/L0 = -4.33, 0.89, and 3.85, respectively.
By comparing the case of EI with that of Non-EI, one can only see significant differences
in C IV and Ne VIII towards the end of the experiment. Departures from EI occur
when the contribution from the advective term,
,
becomes comparable or larger than the terms on the right-hand side of Eq. (1). The
time-dependent increase of
(respectively
)
at a certain y location takes place when the advective term becomes
negative. This happens at the expense of C V (respectively Ne IX) which
becomes depopulated at that location
. In the case of C IV such behaviour is seen after
s; while in Ne VIII it happens after
s.
As seen in Fig. 1, the largest difference between EI and Non-EI is encountered
for the O VI ion. This is expected, since the most rapid changes in the physical
conditions are taking place at roughly the formation temperature of the O VI ion.
Notice the split of
population into three main branches
at
s. Two branches appear as double-peaked in EI, and they move farther
apart as time passes. As
happens to have different
signs at the two peaks of each lane, and since Uy does not change its sign, the result
is an advective contribution with different signs at the two peaks. In Non-EI, one would
therefore expect a time-dependent increase of
at one of the peaks,
while the other peak should decrease. This is precisely what Fig. 1 shows.
Here the peak population observed at the higher absolute value of y continues to grow
in time, while the one at slightly lower y continuously depletes. The increase is found
to occur at the expense of O V ion, while the decrease seen in the other peak
increases the number distribution of the O VII ion. A similar behaviour is seen in
the double-peaked lane of
at negative y positions.
For convenience, let the ``blue'' jet refer to the one propagating in the positive
y-direction, while the ``red'' jet moves in the opposite direction. As seen in
Fig. 1, the largest departures from EI occur in the ``red'' jet, where
also reaches its maximum. Hence, one would expect to see a relatively strong
red-shifted Doppler component in the spectra, and a less strong blue-shifted Doppler
component. Even some emission at the rest wavelength is expected to be present in the
spectra. The ``red'' jet will be visible in the C IV line, while the ``blue'' one will
be recognised in the Ne VIII line as a blue-shifted Doppler component in the spectra.
It is clear from the discussion so far, that departures from EI indeed take place in the reconnection events presented in Paper I. These affect the various ions differently, with the magnitude of the effect depending on the actual physical conditions encountered. Since we have only analysed experiment ``G1'' so far, where the dynamical time-scales is longer than in experiments ``G5'', we infer that deviations from equilibrium values of the three ions will be even larger in the ``G5'' cases. It has to be mentioned that the analysis made so far applies when the line-of-sight coincides with the jets symmetry axis, along which the maximum flow velocities are reached. We expect to observe smaller departures from EI if there is a slanted angle between the two axes.
![]() |
Figure 2:
Line synthesis of experiment ``G1'' is shown as time-series in
C IV
|
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In experiment ``G1'', it is possible to see the reconnection event in all the three lines.
The initial plasma temperature varies along y, as follows:
T= 1.01-4.11,
0.89-5.66,
and
K, in Bins I, II and III respectively. At the location of
the ad hoc diffusion region the initial temperatures are 1.75, 1.99, and
K, respectively. In experiment ``G1'', the initial temperature gradient along
the symmetry axis,
,
is smaller than outside the current concentration (Paper I).
Thus, the wider the region is that we average the temperature over (Bin I-III), the larger
the effective variation with height becomes. This has a clear impact on the observable
consequences of the reconnection event in the three lines of interest, as seen in
Fig. 2.
Since the initial peak population of the C IV ion is obtained far below the reconnection site (see Fig. 1), one does not expect to see any significant changes to the profile of the C IV 1548.2 Å line. In Bin I, this peak population is found very close to the bottom boundary of computational domain. This is why the corresponding time-series (top left in Fig. 2) show no ``velocity'' events, and reveal only a gradual decrease of the intensity of C IV line with time. In contrast, a slightly red-shifted Doppler component becomes visible in the spectra of Bins II and III towards the end of the experiment (after t=90 s). This is an effect of the temperature in these bins being above the temperature of line formation at the lower boundary of the domain. The plasma parameters in this region are therefore, only being effected as the ``red'' jet approaches this region of the domain. In the same way, the decrease in the intensity of the central line reflects the change in physical conditions the reconnection jet imposes on this region.
A different physical situation is encountered for the Ne VIII 770.4 Å resonance
line. Assuming the initial condition is extended above the numerical domain, then for
Bins I and II, the peak population of Ne VIII ion is reached above the top boundary
of computational domain, while in Bin III this occurs just inside the top boundary.
Although the absolute intensity of the Ne VIII line in Bin I is much lower than
in Bin III, the reconnection event is seen in the time-series of Bin I as both red- and
blue-shifted Doppler components. The blue component appears at a lower relative intensity,
and at a slightly larger velocity than the red component.
The presence of the red Doppler component is at first quite surprising. The ``red'' jet is
propagating towards colder and denser plasma and should therefore have much less of a
chance to produce a signal in the line profile than the ``blue'' jet that propagates towards
region where the Ne VIII line is formed. By re-scaling the right hand side panels of
Fig. 1, it is possible to see a weak presence of the Ne VIII ion at the
locations of the ``red'' jet. Because the density decreases significantly with height, then
the density squared effects the line intensity, providing a large signal from the
red-shifted Doppler component. In the Bin II time-series, however, the blue-shifted Doppler
component is brighter than the red one, and the central line intensity is larger than in
Bin I, although the intensity is gradually declining with time. With regard to Bin III, one
would expect the ``blue'' jet to be present as a strong Doppler-shifted component towards the
end of the time series. This is confirmed by Fig. 2 (bottom right); the line
spectra after
s is dominated by this component
. The central
line intensity rapidly decreases after
s, though some finite emission is
still present at the end of the time-series. This could be predicted from Fig. 1,
where it is seen that the initial region of Ne VIII ions is ``pushed'' out through the
top boundary as the ``blue'' jet propagates in this direction.
![]() |
Figure 3:
The line profile of O VI
|
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In O VI 1031.9 Å both red- and blue-shifted Doppler components are present in the
spectra. This is expected, since the EI peak population in O VI ion is reached inside
the computational domain for all three bins. The population peak of Bin III appears closest
to the ad hoc diffusion region in the initial physical condition, with the distance to
the diffusion region increasing as the spatial resolution of the Bin is increased. Thus, one
would observe both the red- and blue-shifted Doppler components as being brighter in the
Bin III spectra than in the Bin I profiles. All of this is confirmed by the images in the
middle column of Fig. 2. The red-shifted component appears at relatively
higher intensity than the blue-shifted in all bins. Toward the end of the time-series, the
red- and blue-shifted components both reach approximately the same absolute value of
Doppler-shift of about 70 kms-1. The maximum Doppler-shift found in the spectra at this time
is nearly
80 kms-1. The line-core intensity centred at rest wavelength is again found
to continuously decrease in time, but never reaches a zero intensity. For Bin I, all three
emission components have comparable strength, while the Doppler-shifted components dominate
in Bin III
.
Following the discussion made in the previous section, Fig. 3 demonstrates how the
departures from EI affect the O VI line profile. This is shown for the case of EI
(dashed line) and Non-EI at the final time of the simulation, i.e. t=119 s. It is found
that the departures from EI mostly affect the two Doppler-shifted components, with the red
one being about 10% brighter in Non-EI than in EI. Here the peak population of O VI
in Non-EI nearly coincides with the maximum flow velocity of the ``red'' jet. In contrast, the
blue-shifted component appears at a 5% higher spectral line intensity in EI compared to that
in Non-EI. This is because the peak population of O VI in Non-EI is located ahead of
the position of maximum flow velocity in the ``blue'' jet. Furthermore, the line-core intensity
is a few % higher in Non-EI than in EI.
| Emission Line | C IV 1548.2 Å | O VI 1031.9 Å | Ne VIII 770.4 Å |
| 0.1 arcsec |
|
|
1.0a |
|
|
|
|
1.10 | 1.00 | 5.46 |
| 0.5 arcsec |
|
|
|
|
|
|
|
1.04 | 1.46 | 1.00 |
| 1.0 arcsec |
|
|
|
|
|
|
|
1.04 | 2.41 | 1.00 |
The observable consequences of the ``G1'' reconnection event are different for the various
emission lines, as well as the three spatial bins. The corresponding time-series reveal
signatures that are similar to those of solar explosive events. The ``visibility'' of the
reconnection jets in the above three lines is well present in the spectra, where they are
observed as strongly Doppler-shifted components. A similar picture is revealed during
observations of solar explosive events, except for the time-dependent evolution of the
line-core intensity (see Teriaca et al. 2001). This could be an indication that most of
the intensity in the observations arises from plasma along the line-of-sight that is not
involved in the explosive event. This could be investigated by taking different orientations
of the line-of-sight, sampling more of the plasma at rest. A summary of the line synthesis
made for experiment ``G1'' is given in Table 2. In this table,
is the spectral
line intensity at the rest wavelength,
,
at time zero, where the unit of
is
.
The other
quantity,
,
measures the maximum line intensity reached during
the whole time-series in units of
.
From this table, it can be seen that the
dominant line, in terms of absolute intensities, is C IV
Å. Less
intense is the resonance line of O VI
Å, and the least emission
originates from Ne VIII
Å. In passing from Bin I to III,
in C IV and O VI decreases, while it increases Ne VIII.
This is a result of the initial temperature variation between the cold current sheet and
the hot exterior, the width of this temperature variations relative the bin size and the
formation temperature of the spectral lines.
| |
Figure 4:
A set of time-series in C IV
|
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| Emission Line | C IV 1548.2 Å | O VI 1031.9 Å | Ne VIII 770.4 Å |
| Experiment ``G5a'' |
| 0.1 arcsec |
|
|
|
1.0a |
|
|
|
10.22 | 1.21 | 1.06 |
| 0.5 arcsec |
|
|
|
|
- |
|
|
1.00 | 75.76 | - |
| 1.0 arcsec |
|
|
|
|
- |
|
|
1.05 | 46343 | - |
| Experiment ``G5b'' |
| 0.1 arcsec |
|
|
|
|
1.0b |
|
|
2.31 | 6.41 | 1.01 |
In experiment ``G5a'', the binned initial plasma temperature varies along y, as follows:
T= 2.85-2.91,
1.45-1.51, and
K, in Bins I, II, and III
respectively. At the location of the ad hoc diffusion region, this temperature is
2.88, 1.48, and
K, respectively. Because of the small temperature
gradient along the line-of-sight, the observational aspects of the magnetic reconnection
are mainly limited to a single resonance transition region line. This event is therefore
very weak or absent in lines formed at spectral lines with peak intensity at temperatures
far away from the plasma temperature of the diffusion region. Table 3 summarises the
results for the ``G5'' experiments in the same format as Table 2. The unit of
is
for experiment ``G5a'', and
for experiment ``G5b'', respectively. The Ne VIII
Å
is very faint for Bin I in experiment ``G5a'' and has been omitted for the other bins as
the relative populations are too low to provide sensible results.
In experiment ``G5a'' the reconnection event is well observed in C IV
Å. The detailed results are shown in Fig. 4. From left to right in
this figure are shown the time-series obtained for Bins I, II, and III, respectively.
All plots shown here are prepared in similar manner to those of Fig. 2. In
this case, the initial temperature at the ad hoc diffusion region for Bin I, is
approximately 3 times higher than the temperature of formation for the C IV
line, while the temperature of diffusion region in Bin III is comparable to the
formation temperature. The intensity of the initial line will therefore obtain its
maximum in Bin III. The resulting time-series in the three Bins reveal the appearance
of two almost symmetric Doppler-shifted components at
s. The symmetry
in this case is caused by the nearly uniform initial temperature along the line-of-sight.
The effect of the two jets on the plasma is therefore almost symmetric with regard to
the rest wavelength of the spectral line. The line Doppler-shifts reach a maximum value
of
kms-1 at the end of computed time-series. The central line intensity
is found to decrease with time, and at the end of the time-series, the line intensity of
the two Doppler components dominate the spectra.
| |
Figure 5:
A set of time-series in C IV
|
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The O VI
Å line is formed at a temperature that corresponds
closely to the temperature of the ad hoc diffusion region in Bin I. From Table 3,
it is seen that this line is the strongest among all three for this experiment, and
therefore the easiest to observe. Line profiles derived for the three bins correspond
to those shown in Fig. 4 for the C IV spectral line.
Figure 5 shows the appearance of the three spectral lines derived for the ``G5b'' experiment using the narrow Bin I. This again clearly shows the symmetric appearance of the reconnection jets in the Doppler profiles and the general decay of the line intensity at the rest wavelength. One can also see that the ratio of the rest wavelength to the Doppler components becomes very large for the lines that only have marginal intensity at the rest wavelength.
In this case, the initial plasma temperature varies along y from 6.17 to
K, with a temperature at the ad hoc diffusion region of
K. One therefore expects that the reconnection event provides the strongest signal
in the Ne VIII line that has a formation temperature close to that of the ad hoc diffusion region. This is confirmed by the information provided in Table 3.
At the end of the computed time-series, the two Doppler-shifted components in the three lines have an absolute value of about 110 kms-1. A more general discussion of experiments with this characteristic setup can be found in Roussev et al. (2001c).
We have examined the observational consequences of the reconnection events discussed in Paper I, in three resonance transition region lines, namely C IV 1548.2 Å, O VI 1031.9 Å, and Ne VIII 770.4 Å. All computations involved time-dependent ion populations, since departures from the equilibrium ionization were found to take place in the events. This implies that it is necessary to consider non-equilibrium ionization in studies of magnetic reconnection events in the solar transition region, when future detailed comparisons between models and observations are to be made.
The line synthesis was based on the data from 2D MHD simulations of magnetic reconnection in a stratified plasma discussed in Paper I. Here experiments with varying degree of stratification were made. By changing the scale-height of the stratification, different characteristics in terms of the structure of the magnetic field and the plasma temperature was achieved. The ``G1'' experiment represents the case with a short scale-height, which gives a more significant change in the plasma temperature with height than across the current sheet. In the case with a long scale-height, ``G5'', the dependence on the temperature gradient is reversed and the initial condition becomes increasingly independent of height as the scale-height goes to infinity.
These differences in the initial physical conditions were found to affect the observational consequences of the reconnection events examined in Paper I quite substantially. When the scale-height in the initial physical condition is short, the temperature increase with height makes it possible to observe the reconnection jets in several spectral lines formed at different temperatures. This gives rise to asymmetric line profiles with either the ``blue'' or the ``red'' jet dominating the Doppler components in the line spectra. In turn, a large scale-height results in a rather small temperature gradient along the initial current structure, which limits the Doppler signatures to spectral lines with a temperature of formation close to that in the reconnection region. It also changes the appearance of the jets, in that they, will produce nearly identical blue and red Doppler components in the spectral lines in this situation. These changes in the spectral line profiles correspond to those observed during solar explosive events.
We examined the observational consequences of reconnection events subject to various spatial resolutions of a spectrograph (under 1 arcsec). For this purpose, we performed line synthesis in the three lines of interest, in regions of various bin-sizes across the line-of-sight, such as 0.1, 0.5, and 1.0 arcsec, respectively. The steeper the gradients in the physical conditions are across the reconnection jets (experiments ``G5''), the more substantial are the differences in corresponding spectra of the lines, with the narrow bin showing by far the highest line intensity of the Doppler-shifted components relative to the line-core intensity. The higher the observational resolution, the less of the background plasma at rest is included in the observations, so that the response from the reconnection jets becomes more dominant. Also, when large gradients are present in the plasma across the observational resolution, this will naturally influence the actual observational output away from the physical conditions of the actual jet, i.e., monitoring the intensity at the rest wavelength much better.
The numerical modelling presented here could not reproduce the increase of
line-core intensity associated with transient events (see Teriaca et al. 2001).
One possible reason for this result is the fact that all computations of
time-dependent ion populations used a 1D approximation. In the evolutionary
equation, Eq. (1), the advective term associated with the
coordinate across the initial current structure, i.e.,
,
was neglected. A rough estimate
of the importance of this term for the O VI ion population in experiment
``G1'' (see Sect. 3) shows that
All spectral line syntheses was done along a particular ray, oriented vertically along the initial current structure. This implies that at different slanted angles between the jet symmetry axis and the line-of-sight, the results from the line synthesis will also be different. The results on this aspect of our investigations further confirmed that the observational consequences of these reconnection events are very subtle, clearly dependent on the assumed initial physical conditions and view angle.
Lastly, we emphasize the qualitative means of the numerical results presented in this study. These are required to achieve a better physical interpretation of solar explosive events. Our numerical calculations did not attempt to match any particular set of observations. The physical situations examined here are far too simplistic to do that.
Acknowledgements
The National Center for Atmospheric Research (NCAR) is sponsored by the National Science Foundation. Research at Armagh Observatory is grant-aided by the N. Ireland Dept. of Culture, Arts and Leisure, while partial support for software and hardware is provided by the STARLINK Project which is funded by the UK PPARC. I. Roussev dedicates his studies to Ana and Elena. He is also thankful to the Department of Applied Mathematics, University of St. Andrews, and the NSO in Tucson, Arizona, for the support provided during his visits there. K. Galsgaard was supported by PPARC in a form of Advanced Fellowship, and is thankful for the visitor grant supported by HAO used to initiate this work. The MHD experiments were carried out on the PPARC funded Compaq MHD Cluster in St. Andrews. I. Roussev is grateful to Luca Teriaca for the atomic data provided. We are all very thankful to Tom Bogdan, Phil Judge, Gerry Doyle, B. C. Low, Tom Holzer, and an unknown referee for the useful comments and suggestions made while this manuscript was prepared.