Computing synthetic spectra is one step, distilling useful information from it is a second - and far more difficult - one. Fundamental stellar parameters for this sample of bright stars are a first direct result which can be deduced from this comparison between ISO-SWS data and synthetic spectra. In Papers III and IV of this series, these parameters will be discussed and confronted with other published stellar parameters.
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Figure 3:
Comparison between the ISO-SWS data of
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Figure 4:
Comparison between band 1 and band 2 of
the ISO-SWS data of ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
A typical example of both a warm and cool star is given in
Figs. 3 and 4 respectively. Different types of
discrepancies do emerge. The size of the discrepancies between
ISO-SWS observations and theoretical predictions varies a lot.
Both for the warm and for the cool stars we see a general
good agreement in shape between the ISO-SWS and theoretical data in
band 1, with however (local) error peaks up to 8%. An exception
is
Peg for which the shape is wrong by
6% and local
error peaks may go up to
15%. The agreement between
observational and synthetic data is worse in band 2: a general
mismatch by up to
15% may occur.
By scrutinising carefully the various discrepancies between the ISO-SWS data and the synthetic spectra of the standard stars in our sample, the origin of the different discrepancies was elucidated. First of all, a description on the general trends in discrepancies for the warm stars will be made, after which the cool stars will be discussed.
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Figure 5:
In panel a) the high-resolution FTS-ATMOS
spectrum of the Sun is compared with its synthetic spectrum based
on the Holweger-Müller model (1974) and computed by using the
atomic line list of Hirata & Horaguchi (1995). Panel b) shows the same
comparison as panel a), but now at a resolving power of 1000 for
the wavelength range going from 3.52-4.08 ![]() ![]() |
For Fig. 5, the atomic line list of Hirata & Horaguchi (1995) was used to generate the synthetic spectrum. This line list has as starting files the compilation by Kurucz & Peytremann (1975) and Kurucz (1989) who lists the semi-empirical gf-values for many ions. Energy levels were adopted from recent compilations (Sugar & Corliss 1985) or individual works. The line list of Kelly (1983) was merged into the file. The gf-values are taken from several compilations (e.g. Fuhr et al. 1988a, 1988b; Reader et al. 1980; Wiese et al. 1966, 1969; Morton 1991, 1992). Published results of the Opacity Project (Seaton 1995) were also included. Comparing the atomic line list of Hirata & Horaguchi (1995) with the identifications as given by Geller (1992) made clear that quite some lines are misidentified or not included in the IR atomic line list of Hirata & Horaguchi (1995).
The usage of VALD (Vienna Atomic Line
Database: Piskunov et al. 1995;
Ryabchikova et al. 1997;
Kupka et al. 1999) and the line list of van Hoof (1998)
did not solve the problem.
Obviously, the oscillator strengths of the atomic lines in the
infrared are not known sufficiently well.
In order to test this hypothesis, Sauval (2002, priv. comm.) has constructed a new atomic line list by deducing new oscillator strengths from the high-resolution ATMOS spectra of the Sun (625-4800 cm-1). A preliminary comparison using this new linelist is given in Fig. 6 (which should be compared with Fig. 5). The contents, nature, limitations, uncertainties, ... of this new line list will be discussed in a forthcoming paper. But it is already obvious from a confrontation between Figs. 5 and 6 that these new oscillator strengths from Sauval are more accurate.
It is plausible that the same reason, i.e. wrong and missing oscillator strengths of atomic lines in the infrared, together with noise, is the origin of the observed discrepancies between the ISO-SWS and synthetic spectra for the other warm stars in the sample, because
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Figure 7:
FTS-ATMOS intensity spectrum of the Sun
(black) at a resolving power
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Figure 10:
Band 2 for Sirius (A1 V) and ![]() |
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Figure 11:
Comparison between the ISO-SWS observation and the
synthetic spectrum of ![]() |
In these oxygen-rich stars, the CO lines are a direct measure of the C abundance. From the present spectra, this carbon abundance can be estimated in two ways:
A first step towards solving this problem was the use of the
high-resolution FTS-KP spectrum of Boo (see Sect. 5). As was explained in Sect. 5 a
high-resolution synthetic spectrum was generated for
Boo
and rebinned to a resolution of 60 000. The agreement between the
observed FTS-KP and synthetic spectrum is extremely good! One
example was already shown in Fig. 16, another one is
depicted in Fig. 17 on page
. In this
latter figure, the problematic subtraction of the atmospheric
contribution causes the spurious features around 2.46700
m for the summer FTS-KP spectrum and around 2.46735
m for the
winter FTS-KP spectrum
. When scrutinising carefully the
first-overtone CO lines in the FTS-KP spectrum, it is obvious that
all the 12CO 2-0 lines, and almost all the 12CO 3-1
lines, are predicted as too weak (by 1-2%) and not as
too strong as was suggested in previous paragraph from the
comparison between ISO-SWS and synthetic spectra! Also the
fundamental CO lines are predicted as being a few percent too
weak. For a better judgement of the KP-SWS-synthetic
correspondence, the FTS-KP spectrum was rebinned to the ISO
resolving power. This was not so straightforward due to the
presence of the spurious features originating from the problematic
subtraction of the atmospheric contribution. In order to conserve
the flux, these spurious features were replaced by the flux value
of the synthetic spectrum. This adaptation is acceptable for the
following reasons:
Figure 18 on page shows the
comparison between the ISO-SWS,
the FTS-KP and the synthetic spectrum for
Boo at a resolving
power of 1500. It is clear that the differences between the
strength of the CO features in the ISO-SWS and FTS-KP spectrum are
significant. This is a strong indication for problems in the
calibration process. The question now arises where this
calibration problem originates from.
Firstly, it has to be noted that the flux values are unreliable in the
wavelength region from 2.38 to 2.40 m due to problems with the
RSRF of band 1A; main features here include the CO 2-0 P18 and
the CO 2-0 P21 lines.
Secondly, no correlation is found with the local minima and maxima in the RSRF of band 1A.
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Figure 12:
Comparison between the AOT06 observation
(revolution 538, black) and the AOT01 speed-4 observation (grey) of
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Defining the spectral resolution and instrumental profile for the ISO-SWS
grating spectrometers, is not straightforward (Lorente 1998;
Lutz et al. 1999). Only for an AOT02 observation has the instrumental profile now been
derived quite accurately (Lutz et al. 1999). The AOT01 mode introduces an
additional smoothing which, due to the intricacies of SWS-data acquisition, is
different from a simple boxcar smooth. The simulation of SWS-AOT01 scans gives
non-gaussian profiles, as can be seen in Fig. 6 by Lorente (1998).
Nevertheless, the theoretical profile of a speed-4 observation
approximates a gaussian profile very closely. Therefore, since the instrumental
profile of an AOT01 is still not exactly known, the synthetic data were
convolved with a gaussian with
/resolution. This incorrect
gaussian instrumental profile introduces an error which will be most visible on
the strongest lines.
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Figure 13:
Top: Comparison between the
AOT01 speed-4 observation of ![]() |
Only for
Dra an AOT06 observation, scanning this
wavelength range, was available in the ISO data-archive. The
comparison between the AOT01 speed-4 and AOT06 observation, both
rebinned to a resolving power of 1500, is an indication that the
resolving power of an AOT01 speed-4 observation in band 1A is lower
than 1500 (Fig. 12). The theoretical resolving power for an
AOT01 speed-4 observation in band 1A is
1500. Figure 5 in
Lorente (1998) shows, however, a large deviation from this value,
attributed to the fainter continuum of the source used for
measuring the instrumental profile and the less accurate fitting in
this band. The use of a resolving power of 1300 - instead of the
theoretical resolving power of 1500 - for band 1A yields a) almost
no difference from the AOT01 SWS data at a resolving power of 1500 and b) a
better match between the SWS and synthetic data for the
strongest CO features (Fig. 13). This observational resolving power of 1300 is also
in good agreement with the observational value given by Lorente (1998) in
her Fig. 5.
The incorrect use of a Gaussian instrumental profile, together with too high a - theoretical - resolving power of 1500 form the origin of the discrepancy seen for the strongest CO features. Therefore, the resolving power of band 1A was taken to be 1300 instead of 1500. Part of the other discrepancies seen in band 1A may be explained by problems with 1. the accuracy of the oscillator strengths of atomic transitions in the near-IR (see point 1. in this section) or 2. the RSRF in the beginning of band 1A (see point 5. in previous section).
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Figure 14:
Summer and winter FTS-KP
spectra of ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() ![]() |
Copyright ESO 2003