![]() |
Figure 2:
The mean flat-field frame
![]() |
The reduction was performed with programs written in the Interactive Data
Language (IDL) using also the IDL KIS package at the Kiepenheuer-Institut
für Sonnenphysik, Freiburg.
![]() |
Figure 3:
Average background
![]() |
To keep the S/N ratio as high as possible it is useful to average several background G frames (see Newberry 1991, for a more detailed description of signal-to noise considerations).
Thus, the Eq. (4) takes the
following form:
As we stated in Sect. 2, the flat-field is used to correct both the non-uniform
response across the surface of the chip and non-uniform illumination of the chip.
Therefore, it is not enough to illuminate the chip with uniform light and use the
resultant exposure for correction.
The uniform light must pass through the complete optical system with an identical
focus, exposure time and other conditions as those valid for every particular spectrum P.
Moreover, the spectral range of the flat-field source frame F should match that of
the object being imaged.
Therefore, for solar CCD spectroscopy, the ideal source for flat-fielding
should be at infinity, should be a source similar to sunlight and the light must
pass through the telescope and spectrograph.
From these last requirements it is clear that it is impossible to get ideal artificial
uniform light from infinity for flat-fielding in this case and the Sun itself is the only
source intensive enough to mimic observational conditions.
Thus, the flat-field source frames F must be derived from images that are almost
identical to the particular raw spectrum P.
There are several ways to create the flat-field source frames Fin this case:
a) the simplest way is to sandwich all particular raw P images we made and
get an average "soft'' spectrum with smoothed spectral line(s);
b) the second possibility is to de-focus the telescope and to make
enough un-sharp images.
Then we construct the average of them to obtain a similar
result to the previous case;
c) The third method of creation of the flat-field source frame F is to
move the image of the Sun across the slit in the focal plane of the telescope
and take a lot of images.
The average of such images will give a similar result to the previous two cases, because the
spectral lines will be smeared due to the fast movement
of the solar image across the spectrograph slit.
It is also possible to use a combination of the second and third methods
(e.g. Johannesson et al. 1992).
It is useful to take the flat-field source frames F very often, to minimize the influence of the temporal changes of the flat-field conditions. Many cases of observations do not allow us to make flat-field source frames F very often. For example, the simultaneous observations with VTT and space instruments or investigation of temporal changes in the solar atmosphere require uninterrupted long series of observations. Then, one can take the flat-field source frames F only at the beginning and at the end of the observing run. So the temporal changes of the flat-field conditions introduce rather serious problems for the reduction of these spectra.
It is clearly seen, from the methods mentioned above, that all non-uniform illuminations
of the chip in the case of large solar spectra are grouped together into one mean
flat-field frame
.
Namely, the
for the first (sandwiching) method will be defined
as:
However, all three methods for the construction of
have some limitations.
Usually, one tries to observe the long series during the best seeing conditions,
keeping the spectrograph slit in the same position of the solar disk or scanning
within small areas.
Thus, the average of many raw spectra P still exhibits shifted patterns which remain
from the real Doppler velocity shifts of a particular part of every particular
raw spectrum P.
This results in non-uniform
in the case of the first method.
The second method with the de-focused telescope tends to optically disturb the spectrum
giving rise to lateral displacement of the location of the spectral line(s) in the
image plane in the camera and changes the fixed pattern, particularly the variations
due to fringing and illumination.
A similar displacement of the spectral lines could appear when one moves the telescope,
if the scanned area at the solar disc is very large.
This smears the spectral line due to averaging of shifted lines caused by real
differential rotation of the Sun.
We used the third method for construction of the mean flat-field frame
.
The quick movement of the telescope was kept very near to the disc centre in a quiet
region to minimize the mentioned above displacement effects in every particular
flat-field source frame F.
The final
was an average of 40 particular flat-field source frames Ffrom which
had previously been subtracted.
The mean flat-field frame
is given in Fig. 2 with a description
of the most important features in the spectrum. Identical features also appear in
the raw spectrum P shown in Fig. 1.
The
contains all six flat-fields Mi mentioned in Sect. 2,
and also the spectral lines as a consequence of the facts discussed in the beginning
of this section.
In the following sections we show how to retrieve the particular Mi from
the mean flat-field frame
.
Because the flat-field M6 is uniform within every sub-segment, it is enough to
estimate the ratios of sensitivities between them and simply construct the
segment-flat matrix M6 as a matrix of four subsegments with appropriate ratios
of sensitivities between them.
We experimentally determined the sensitivities of the segments which are equal to 1.004, 1.029, 0.930 and 1.037 for segment I, II, III and IV, respectively, comparing
to the mean intensity of the whole chip, normalized to unity.
The designation of the segments is identical as in Fig. 3.
We have found the stability of the sensitivity of the individual segments to be within
the range of 0.1% for the intensity range of 400-3200 ADU.
Obtaining the segment-flat M6, it was possible to correct the mean flat-field
frame
by dividing it by M6.
Logically, the spectrum S was also corrected in the same way at this stage of the
reduction process.
We will name this improved spectrum S1.
It will be used in the simple reduction approach.
It was possible to extract the segment-flat M6 from the mean flat-field
frame
even when the spectral lines were presented.
This is not the case in the other flat-field matrices.
The spectral lines constrain the flat-field matrices and we must erase them from
the
.
The smoothing processes used for retrieving the flat-field matrix M are applied to
spectra in both the X and Y directions in the image.
To run them correctly it is necessary to have the mean flat-field frame
(as well as the spectrum S1) parallel to both edges of the CCD camera.
The correction of spectral line stretching and inclination is essential for the next
steps of flat-fielding.
To erase the spectral line from the
the smoothing also runs in the Y direction in the image.
If the spectral line in the
is not strictly vertical, i.e. parallel with
the Y edge of the image, the process will not work correctly, as we will see later.
The best procedure to estimate line "stretching'' is to utilize a terrestrial
line if it is available in the spectrum. Such a line has a well defined and stable
centre.
The positions of the centres determined for every scan directly reflect the curvatures
and inclination of the spectral lines in the particular spectral region.
But often there are no terrestrial lines available in the spectrum or the terrestrial
lines are very weak, e.g. as in our case.
Here we used the smoothed observed line itself derived from the mean flat-field frame
as the source of the required information.
Again, the vector of the positions of the centres of the particular line profile
(row) gave us information about the curvature and inclination of the spectral lines
along the slit.
Such a vector is given in Fig. 4b.
The vector of the positions of the centres was approximated by a polynomial approximation
of the second order in this case (thick line in Fig. 4b). The resulting polynomial approximation was finally used for shifts of every particular scan
(row) in the X direction to make the spectral lines parallel to the Y edges of the image.
An identical polynomial approximation for shift was applied to both the mean flat-field
frame
and the spectrum S1.
This again, similar to the previous step, required several incomplete columns on the left
and right of the image to be cut away.
The prepared spectrum S2 and the mean flat-field frame
after
all steps of the reduction mentioned above are shown in Fig. 5.
The spectrum S2 will be used in the extended and precise reduction.
Equation (10) is calculated in two steps:
Dividing the mean-flat field frame
by the "soft'' part of the flat-field
matrix M we derived the "hard'' part of the flat-field matrix M.
This is shown in Fig. 6a.
Then the spectral lines are eliminated from the "soft'' part of the
flat-field matrix M dividing this part by "mean scan''.
It is constructed as an average of all rows of the image.
From this last step it is clear why the spectral lines must be parallel to the Y edge of the image.
If it is not the case, some residual intensities in every row of the image will remain.
This incorrect resulting "soft'' flat-field matrix M2,3 is shown in
Fig. 4a.
The correct "soft'' M2,3 is shown in Fig. 6b.
For the VTT no published data about the drift of its spectrograph exist.
Within the investigation performed in 1988 one of the authors (H.W.) determined
drifts using terrestrial oxygen lines 6302.005 Å and 6302.771 Å.
He found drifts that ranged from 0.015 pm within a minute up to 0.3 pm within an
hour in August 1988.
![]() |
Figure 7: The "slit-vector'' which represents the average of all columns of the flat-field matrix M1,4,5 shown in Fig. 6a. |
We also found the drift of the spectrum in the focal plane of the spectrograph of VTT in both directions in a data set observed in 1996 using different CCD cameras. Again the terrestrial lines of the oxygen molecule 6302.005 Å and 6302.771 Å were used for determination of the drift in wavelength direction. The wires (WL) in the images were used as tracers for determination of the drift in spatial direction. Values of 1.06 pm (1.3 pixel) per hour and 0.26 arcsec (1.5 pixel) per hour were found for the X and Y directions, respectively. In addition we have found that the drift was not linear. It was steepest in the morning and gradually decreased in the middle of the day.
The analysis of the drift made with the data used in this work shows that the drift in the spatial direction (the WL wires were used for tracking) was 1.7 pixel per hour that corresponds to 0.21 arcsec. It is in agreement with the previous results.
Time dependent parts of the flat-field matrix M
As we have documented above the spectrograph drift moves the image (spectrum) in the focal plane of the spectrograph in both the X and Y directions. This will affect only two components of the whole flat-field matrix M, namely the illumination-flat M2 and the slit-flat M5, because the other three M1,3,4, i.e. the pixel-flat, the shutter-flat and the camera-flat are closely connected to the CCD camera body.
The intensity errors caused by the movement of the illumination-flat M2 are negligible because its gradient is very small across the camera field (see Fig. 6b). Thus a shift of even several pixels does not match any measurable effect in intensity changes. We separated the M2 (together with the shutter-flat M3) directly in the flat-fielding procedure as the "soft'' part of the flat-field matrix M.
The movement of the slit-flat M5 is much more important. This flat-field is caused by dust and defects of the spectrograph slit. These show rapid changes of the intensity across the camera field in the Y direction and they are seen as the horizontal white and black lines and stripes described in Fig. 2 and mentioned above many times. The movement of the slit-flat M5 acts in both the X and Y direction in the spectrum.
The movement of the slit-flat M5 in the X direction is not important. The horizontal lines do not significantly change their intensities in the X direction because the inclination of the image was corrected in the previous step of the reduction (cf. Sect. 4.4.1).
But movement of the slit-flat M5 in the Y direction by even a fraction of a
pixel changes dramatically the whole "hard'' flat-field matrix M1,4,5 which
then does not match the conditions valid for the observed spectrum S2.
To solve this problem, one has to separate the slit-flat M5 from the
"hard'' part of the flat-field matrix M1,4,5 (Fig. 6a),
to be able to shift only the slit-flat M5 in the Y direction, to fit the
particular spectrum S2 well.
Separation of the slit-flat M5
We benefited from the fact that only the slit-flat M5 is uniform in the
X direction.
This is a direct consequence of the imaging of the slit on the focal plane of the
spectrograph.
Thus, the vector made as an average of all columns of the "hard'' flat-field M1,4,5 will mainly represent the fluctuations of the slit-flat M5in the Y direction because the other two components, the pixel-flat M1 and
the camera-flat M4, are randomly distributed across the CCD image and they
will not contribute systematically to the averaged vector.
We denoted this vector the "slit-vector'' (see Fig. 7).
We created a new array of the same dimensions as the spectrum S2 and the
"slit-vector'' was replicated in all columns of the created array.
Thus, this new array represents the pure slit-flat M5 (see Fig. 6c).
Obtaining the pure slit-flat M5 makes it possible to extract the pixel-flat
and the camera-flat M1,4 dividing the "hard'' flat-field matrix M1,4,5
by the pure slit-flat M5. The resulting M1,4 is shown in Fig. 6d.
![]() |
Figure 8: a) The spectrum R2 as the resultant of the extended reduction made according to Eq. (12). The symbols V and H denote the sharp intensity spikes resulting from incorrect fitting of the strips and lines caused by dust and defects on the spectrograph slit and by the artificial wires seen in the prepared spectrum S2; b) The spectrum R3 as the resultant of the precise reduction made according to the Eq. (13). The grey-scale bars give relative intensities expressed in ADU. |
P |
![]() |
R1 | R2 | R3 | |
Fig. 1 | Fig. 8a | Fig. 8b | |||
![]() |
2192 | 2149 | 2308 | 2291 | 2282 |
STD [![]() |
5.61 | 5.72 | 5.67 | 6.09 | 4.72 |
We need to keep the positions of the artificial wires WL for adjustment between the two CCD images taken with different CCD cameras in different spectral regions. Therefore, just before dividing the prepared spectrum S2 by the flat-field matrices, the central rows of the artificial wires WL in the flat-field matrices were replaced by rows of mean intensity. After dividing the spectrum by the flat-field matrices the two horizontal central WL wires appeared back in identical positions in the reduced spectrum R3 because they had not been removed from the prepared spectrum S2.
G |
![]() |
F | F-G |
![]() |
![]() |
![]() |
M1,4,5 | M2,3 | M5 | M1,4 | |
Fig. 3 | Fig. 2 | Fig. 5b | Fig. 6a | Fig. 6b | Fig. 6c | Fig. 6d | |||||
![]() |
44 | 44 | 1248 | 1204 | 1204 | 1205 | 1303 | 1 | 1 | 1 | 1 |
STD [![]() |
2.87 | 0.80 | 4.96 | 5.06 | 5.04 | 5.09 | 4.84 | 2.59 | 1.44 | 2.27 | 1.23 |
Copyright ESO 2002