It is important to assess the relevance of the effects of spherical geometry and radiative transfer on the synthetic spectra. For hot stars, have shown that a combination of geometric effects and line blanketing can resolve a long standing problem of discrepancies between synthetic and observed spectra. The effects of spherical symmetry on cool giant atmospheres has been investigated previously by for giant M and C stars, by for M giants, and by for Carbon stars. Our model grid extends this work toward warmer stars and reduces the gap to the stars considered in . In addition, improved molecular line lists are now available and since found a close connection between line blanketing and sphericity for hot stars, the improved molecular line data could affect the results.
In Fig. we compare normalized
(to the same area) low-resolution (
) spectra for 3 sets of models. Each
panel displays a NG-giant synthetic spectrum (full lines) and a synthetic
spectrum calculated with the same parameters and input physics, but assuming
plane parallel geometry. In this figure, only the model with
shows visible differences between the plane parallel and spherical
cases. However, plotting the relative differences of the spectra in
Fig. 4 reveals systematic differences even for low resolution
spectra. For
(top panel), we find that the spherical model
emits more flux than the plane parallel model in the short wavelength regime.
There are also some changes in the slopes of the spectra between 0.45 and
m, which are hardly noticeable in the low resolution spectra. The
middle panel shows the results for
. This model displays a
different systematic change in the blue spectral region, the long wavelength
part of the displayed wavelength interval does not reveal large systematic
effects. The highest effective temperature shown,
, shows the
smallest systematic changes.
Figure 5 is similar to the previous plot but it shows the changes
for a resolution of (10 times better). From this figure it becomes
clear that the changes are due to the effect of line blanketing: line overlap
and individual line strengths change between spherical and plane parallel
models. In low resolution spectra this produces a change in the
pseudo-continuum that is formed by the overlapping spectral lines. In the
model the TiO lines are significantly affected. This shows that
spectral analyses based on high-resolution spectra need to account for spherical
effects.
For longer wavelengths we find that the differences between spherical and plane
parallel models are smaller. Figures 6 and
7 demonstrate this for low resolution and medium resolution
spectra, respectively. The changes are mostly due to the sensitivity of the CO
lines to changes in the structure of the atmosphere, therefore, they are larger
at lower effective temperatures. The figure with the higher resolution shows
that there are significant changes in individual water lines for low
. At higher effective temperatures, individual atomic lines are up to
15% stronger in the plane parallel models (less emitted flux, since these are
absorption lines). The conclusion is that high-resolution spectral
analysis requires spherical models, whereas low resolution spectra or colors
can be interpreted using simple plane parallel models.
In order to demonstrate the reason for these differences, we display in
Fig. 8 the electron temperatures as functions of our standard
optical depth , which is simply the optical depth in the continuum (b-f
and f-f processes) at a reference wavelength of
m. The temperature
structures for the 2 models with
are nearly identical, the
differences are less than about
everywhere. In the model with the lowest
effective temperature (
) the differences are larger, close to
at
. This amounts to nearly 10% change in the absolute
temperature, which is quite significant for the formation of the spectrum. Note
that the line optical depth in the blue spectral region can be orders of
magnitude larger than
and many ``blue lines'' actually form around
. The model with
lies in between the two
extremes and is not shown in the figure. The temperature structure is only a
part of the full structure of the atmosphere, gas pressures and partial
pressures change accordingly. For larger gravities, the differences between
plane parallel and spherical models become smaller and for gravities
log(g)>3.0 the differences are small enough to be negligible for most
applications.