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Astron. Astrophys. 317, 942-948 (1997)
3. Data reduction
We first selected the spectrograms exhibiting the best spatial
resolution. These were first reduced in the usual fashion: The average
dark signal was subtracted and a gain correction was derived from the
flat field spectrograms and was applied. The latter eliminates
possible effects from vignetting, varying width of the spectrograph
slit along the spatial direction, and dust on the optical surfaces and
on the chip. Next, since the two oppositely polarized light beams pass
through the spectrograph along slightly different paths, correction
for different optical aberrations had to be applied. For this the
and subframes had to be
adjusted to have the same orientation of the spatial and the
wavelength axes and to have the same spatial and wavelength scale.
This is necessary to avoid spurious V signals upon subtraction
of the spectrograms. Noise reduction was achieved by low-pass Fourier
filtering in wavelength direction and by taking running means in
spatial direction over 3 CCD pixels, limiting the spatial resolution
to 0 5.
The addition and subtraction of subframes yielded spectrograms of
the Stokes I and V components, respectively, which were
normalized to the continuum intensity . The
polarimetric accuracy is of 0.5% of ,
essentially due to photon noise and to inaccuracies of the gain
corrections. Fig. 1 depicts profiles from regions with strong V
signals, i.e. from magnetic regions. The data for the 615.1 and 617.3
lines were taken simultaneously. Those of the 614.9 line stem from a
different observing date, thus from a different scenery on the Sun.
For comparison, the average I profiles obtained from the flat
field spectrograms from disc centre are shown as well. Typical
observed profiles of these lines are also shown in Kneer et
al. (1996).
![[FIGURE]](img17.gif) |
Fig. 1. Stokes I and V profiles observed with high spatial resolution in plages near disc centre, normalized to the local continuum intensity. The V zero crossings have been chosen as reference wavelengths. The data of the Fe I lines are from simultaneous observations. The dotted profiles are from disc centre of the quiet Sun.
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From the I profiles we determined the following line
parameters: continuum intensity ; line centre
residual intensity ; velocity
from the position of the line centre; and the
full width at half line depression FWHD. The values of
will be given relative to the running mean
velocity taken over derived from the position
of the minimum intensity . In this way
small-scale, mainly granular velocities are averaged out and
is measured relative to the background of the 5
min oscillations. The V profiles yield: the maximum amplitude
= max( ) with
and the unsigned blue
and red extrema of the V profile, respectively; the amplitude
asymmetry ; the wavelength separation
of and
; and the velocity
deduced from the position of the zero crossing of the V
profile. Again, is measured relative to the
average line centre position, i.e. its running mean over
. ,
, ,
, and are obtained from
parabolic fits about the extrema of the profiles,
from a third order polynomial fit about the
zero crossing of V. The Stokes V data are determined
only at spatial positions where the V signal is sufficiently
strong. We chose as a lower limit = 0.02
, which is well above noise and possible
spurious, instrumental V signals.
© European Southern Observatory (ESO) 1997
Online publication: July 8, 1998
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