Astron. Astrophys. 363, 289-294 (2000)
4. Comparison with line parameter correlations
Theoretical correlations ,
, and
can be compared with results of
spectral observations made with high spatial resolution, namely with
correlations ,
, and
, if we suppose that a) we know
exactly the region of the atmosphere where the spectral line is formed
and b) if the region which contributes mainly to the line formation
process is narrow. Both assumptions are supported by results of
Kucera et al. (1998). Here
denote spatial variations of
residual intensity in the line core and
correspond to spatial variations of
Doppler shifts.
To test whether spectral lines reproduce the main real correlative
relationships of the model photosphere we simulated a set of 13
Fe I and 6 Fe II lines using
our time-dependent 2-D models. The line parameters are given in
Table 1. Together with line wavelength
( ) and low excitation potential
(EPL), Table 1 represents an estimation of line formation
heights. denotes the effective
height of line formation for the line equivalent width (weighted over
the whole profile); is the effective
height of line formation for central line depth;
is the geometrical height at line
center optical depth = 1.0. Here
denote the integral optical depth in
the line and in the continuum at the wavelength of the line center.
and
were calculated with depression
contribution and Unsöld-Pecker weighting functions. All these
weighting quantities we computed for a 1-D model which was obtained by
spatially and temporally averaging our sequence of 2-D models.
![[TABLE]](img60.gif)
Table 1. Spectral lines used for simulation.
Fig. 5 displays correlations, derived from these simulations.
They are shown in dependence on
(Fig. 5a-c) and
(Fig. 5d-f). If we compare between
and
(Fig. 2 - Fig. 5a and d),
and
(Fig. 4 - Fig. 5b and e),
and and
(Fig. 2 - Fig. 5c and f)
it is easy to conclude that a) spectral line correlations correctly
reproduce real correlative relationships of the model atmosphere if b)
we use the scale of geometrical
heights for our sample of spectral lines. Therefore, this scale is
more suitable for diagnostic purpose in the context of our 2-D
models.
![[FIGURE]](img61.gif) |
Fig. 5a-i. Correlations found from simulated a -f and observed g -i variations. Error bars are estimates of the standard deviations - they reflect a scatter of the correlation coefficients measured from the set of spectrograms. The open circles and dashed lines represent Fe II lines, filled circles with solid lines are correlations obtained with Fe I lines. The squares stem from Fe I observations of Hanslmeier et al. (1990); triangles from Fe I observations of Kucera et al. (1995) and those presented here; and diamonds from Fe I lines investigated by Balthasar et al. (1990).
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To test these simulated correlations we present in Figs. 5g-i
correlation coefficients calculated for five Fe I
lines from spectral observations described in Sect. 2. The
numerical values of correlations are given in Table 2 where means
and differences have been derived from two subsequent exposures taken
in the same slit position. The height
, determined in the same way as in
Table 1, is given in Table 2 too. Moreover in
Figs. 5g-i some previously published data are plotted from papers
of Hanslmeier et al. (1990), Balthasar et al. (1990), and
Kucera et al. (1995).
![[TABLE]](img63.gif)
Table 2. Correlations of the spectral line characteristics derived from the observations.
Although these observations do not describe possible relationships
in detail, they are not in disagreement with the theoretical
prediction. It is very important that
show a tendency to decrease their
negative correlative relationship in the upper photosphere in
agreement with model predictions.
© European Southern Observatory (ESO) 2000
Online publication: December 5, 2000
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