For the purpose of analysing our observations, synthetic spectra have been generated (Ryde et al. 1998) using model photospheres from the new grid of spherically-symmetric model photospheres of M giants, which is currently being calculated with the latest version of the MARCS code. This version is the final major update (of the code and its input data) in the suite of MARCS model-photosphere programs first developed by Gustafsson et al. (1975) and further improved in several steps, e.g. by Plez et al. (1992), Jørgensen et al. (1992), and Edvardsson et al. (1993).
These hydrostatic, spherical model photospheres are computed on
the assumptions of Local Thermodynamic Equilibrium (LTE),
homogeneity and the conservation of the total flux (radiative plus
convective; the convective flux being computed using the mixing
length formulation). The radiative field used in the model
generation, is calculated with absorption from atoms and molecules
by opacity sampling in approximately 84 000 wavelength points over the entire, relevant wavelength range considered for the star (
-
).
Data on the absorption by atomic species are collected from the
VALD database (Piskunov et al. 1995) and Kurucz (1995, private
communication). The opacity of CO, CN, CH, OH, NH, TiO, VO, ZrO,
H2O, FeH, CaH, C2, MgH, SiH, and SiO are included and
up-to-date dissociation energies and partition functions are used.
The continuous absorption as well as the new models will be fully
described in a series of forth-coming papers in A&A (Gustafsson et al.; Jørgensen et al.; Plez et al., all in preparation).
The new models were used by, among others, Decin et al. (2000) in their
modeling of the K5III-giant
Tau.
Using the computed model photospheres we calculated synthetic
spectra by solving the radiative transfer at a high wavelength
resolution in a spherical geometry through the model photospheres.
Using extensive line lists (consisting of wavelengths, excitation
energies of the lower state of the transition, and line strengths
in the form of oscillator strengths), we produce synthetic spectra
of wavelength regions around the water vapour bands ( and
)
at 2.60-3.66
m.
The line lists included in the generation of the synthetic spectra
are H2O (Partridge & Schwenke 1997) (including all lines stronger than given by
the condition
,
where
and
is the excitation energy in eV,
leading to more than 2 million lines), CO (Goorvitch 1994), SiO
(Langhoff & Bauschlicher 1993), CH (Jørgensen et al. 1996), CN (Jørgensen & Larsson 1990; Plez 1998, private communications), OH
(Goldman et al. 1998), and C2 (Querci et al. 1971; Jørgensen 2001,
private communications). The accuracy and the
completeness of these line lists are discussed in
Decin (2000). We have also included CO2 with data from the
Hitran database (Rothman et al. 1987, 1992) and the Hitemp database
(Rothman et al. in preparation).
In the generation of synthetic spectra, we calculate the radiative
transfer for points in the spectrum separated by
(corresponding to a resolution of
)
even though the final
resolution is much less. With a microturbulence of
in the model photosphere, this means that
we are sure of sampling all lines in our database in the
generation of the synthetic spectrum. This is an important point
since a statistical approach, by only taking fewer,
opacity-sampled points, will give an uncertainty in the
synthesised spectrum. There will be noticeable differences in the
synthesised spectra calculated with different sets of points,
unless one chooses the spacing between the points
smaller than the physical width
of the line broadening. This is especially important when dealing
with molecular bands, since the separation between lines differs
greatly with wavelength depending on whether the lines are close
to a band head or not. For example, by choosing random points in
the spectrum, at which the radiative transfer is calculated for
the synthetic spectrum, with a larger separation than we have
chosen, one will tend to overestimate the absorption at band heads
(or in regions with a high line density) and underestimate it far
from band heads (or in regions with a low line density).
The emergent model spectra are subsequently convolved with a Gaussian in the same manner and with the same resolution as the observed bands. This will allow a comparison with ISO observations.
Copyright ESO 2002