A&A 391, 195-212 (2002)
DOI: 10.1051/0004-6361:20020612
L. Girardi1,2 - G. Bertelli3,4 - A. Bressan4 - C. Chiosi1 - M. A. T. Groenewegen5,6 - P. Marigo1 - B. Salasnich1 - A. Weiss7
1 - Dipartimento di Astronomia, Università di Padova,
Vicolo dell'Osservatorio 2, 35122 Padova, Italy
2 -
Osservatorio Astronomico di Trieste,
via Tiepolo 11, 34131 Trieste, Italy
3 -
Istituto di Astrofisica Spaziale, CNR, via del Fosso del Cavaliere,
00133 Roma, Italy
4 -
Osservatorio Astronomico di Padova,
Vicolo dell'Osservatorio 5, 35122 Padova, Italy
5 -
PACS ICC-team, Instituut voor Sterrenkunde,
Celestijnenlaan 200B, 3001 Heverlee, Belgium
6 -
European Southern Observatory, Karl-Schwarzschild-Str.
2, 85740 Garching bei München, Germany
7 -
Max-Planck-Institut für Astrophysik, Karl-Schwarzschild-Str.
1, 85740 Garching bei München, Germany
Received 5 November 2001 / Accepted 19 April 2002
Abstract
We provide tables of theoretical isochrones in several
photometric systems. To this aim, the following steps
are followed:
(1) first, we re-write the formalism for converting
synthetic stellar spectra into tables of bolometric
corrections. The resulting formulas can be
applied to any photometric system, provided that
the zero-points are specified by means of either ABmag, STmag,
VEGAmag, or a standard star system that includes well-known
spectrophotometric standards. Interstellar absorption can be
considered in a self-consistent way.
(2) We assemble an extended and
updated library of stellar intrinsic spectra. It is mostly
based on "non-overshooting'' ATLAS9 models, suitably extended
to both low and high effective temperatures. This offers an
excellent coverage of the parameter space of
,
,
and [M/H]. We briefly discuss the main uncertainties and points
still deserving more improvement.
(3) From the spectral library, we derive tables of bolometric
corrections for Johnson-Cousins-Glass, HST/WFPC2, HST/NICMOS,
Washington, and ESO Imaging Survey systems (this latter
consisting on the WFI, EMMI, and SOFI filter sets).
(4) These tables are used to convert several sets of Padova
isochrones into the corresponding absolute magnitudes and
colours, thus providing a useful database for several astrophysical
applications. All data files are made available in electronic
form.
Key words: stars: fundamental parameters - Hertzprung-Russell (HR) and C-M diagrams
One of the primary aims of stellar evolution theory is that of
explaining the photometric data - e.g. colour-magnitude diagrams
(CMDs), luminosity functions, colour histograms - of resolved
stellar populations. To allow whatever comparison between theory and
data, the basic output of stellar models - the surface
luminosity L and effective temperature
- must be first
converted into the observable quantities, i.e. magnitudes and
colours. This conversion is performed by means of
bolometric corrections (BC) and
-colour relations, and
later by considering the proper distance, absorption and
reddening of the observed population, and the photometric errors.
Determining BCs and
-colour relations
is indeed one of the most basic tasks in stellar astrophysics.
Empirical determinations (see e.g. the compilations by
Schmidt-Kaler 1982; Flower 1996; Alonso et al.
1999a,b) involve a great observational effort, and
are obviously the most reliable if compared to purely
theoretical determinations. However, since the empirical calibrations
are mostly based on
nearby stars, only a limited region in the space of stellar
parameters (
,
,
and metallicity [M/H]) can be covered by
observations. This contrasts with our
present-day capabilities of getting resolved photometry of populations
that are certainly very different from the local one, like those in dwarf
galaxies and in the Bulge. For instance, present empirical relations
do not include young-metal poor populations, or super-metal rich stars,
which are likely present in the resolved galaxies of the Local Group.
Another important limitation of empirical relations is that they are usually available just for a small set of filters or photometric systems, like the popular Johnson-Cousins-Glass one. Again, this is in contrast with the rapid diffusion in the use of specific filter sets, for which no empirical relation is yet available, though large databases are already being collected. Just to mention a few relevant examples, new filter sets have been adopted in the Hubble Space Telescope (HST) Wide Field Planetary Camera 2 (WFPC2), in the European Southern Observatory (ESO) Wide Field Imager (WFI), and in the Hipparcos mission. Moreover, brand-new photometric systems have been designed for the Sloan Digital Sky Survey (SDSS), and will be adopted in the future GAIA mission. An impressive amount of data will be provided by these instruments in the coming years, and much of it will soon become of public access. Then, it would be highly desirable to have the capability of converting stellar models to these many new photometric systems, bypassing for a moment the time-consuming procedure of empirical calibration.
With this target in mind, we have undertaken a project aiming at providing
theoretical BCs and colour transformations for any broad-band
photometric system, and many intermediate-band systems as well.
Actually, the project starts with the work by
Bertelli et al. (1994), who presented a large database of theoretical
isochrones and converted them to the Johnson-Cousins-Glass UBVRIJHK
system. The transformations were primarily based on Kurucz (1993)
synthetic atmosphere models, suitably extended in the intervals
of lower and higher effective temperatures. In Chiosi et al. (1997),
the same theoretical isochrones are converted to the WFPC2 photometric
system, and the attention is paid to the features that
isochrones and single stellar populations present in ultraviolet (UV)
colours. In particular, they address the question whether the
variation of UV colours of elliptical galaxies as a function of
red-shift presents signatures from which one can infer the age and type
of the source emitting the UV flux. Later on, Salasnich et al. (2000)
present new isochrones for
-enhanced chemical mixtures,
for both UBVRIJHK and WFPC2 photometric systems.
The present work is a natural follow-up of this project, in which, besides extending the number of available photometric systems, we aim at updating and improving the database of stellar spectra which is at the basis of the complete procedure.
The plan of this paper is as follows: Sect. 2 details the adopted formalism. In Sect. 3, we describe the stellar spectral library in use. Section 4 gives the basic information about the several photometric systems under consideration. The resulting tables of bolometric corrections are then applied to a large database of stellar isochrones, which are already described in published papers and briefly recalled in Sect. 5. Section 6 illustrates some main properties of the derived isochrones, and describes the retrieval of data in electronic form.
By synthetic photometry we mean the derivation of photometric quantities based on stellar intrinsic (and mostly theoretical) spectra, rather than on actual observations. The first works in this field (e.g. Buser & Kurucz 1978; Edvardsson & Bell 1989) were based on sets of synthetic spectra covering very modest - by present standards - intervals of effective temperature, gravity, and metallicity. The situation dramatically improved with the release of a large database of ATLAS9 synthetic spectra by Kurucz (1993). The first systematic use of Kurucz spectra on theoretical isochrones has been from Bertelli et al. (1994) and Chiosi et al. (1997).
In order to apply synthetic photometry to sets of theoretical isochrones, the basic step consists in the derivation of bolometric corrections and temperature-colour relations from the available spectra. Several papers deal with the problem (e.g. Bertelli et al. 1994; Chiosi et al. 1997; Lejeune et al. 1997; Bessell et al. 1998), presenting mathematical formalisms that, although looking somewhat different, should be equivalent and produce the same results when applied to the same sets of spectra, filters, and zero-points. In the following, we re-write this formalism in a very simple way. Our aim is to have generic formulas that, by just minimally changing their input quantities, can be applied to a wide variety of photometric systems.
For a star, the spectral flux
as it arrives at the Earth,
,
is simply related
to the flux at the stellar surface,
,
by
In Eq. (2), the integrands
are proportional to the photon flux
(i.e. number of photons by unit time, surface,
and wavelength interval) at the telescope detector.
This kind of integration applies well to
the case of modern photometric systems that have been
defined and calibrated using photon-counting devices such as
CCDs and IR arrays. However, more traditional systems
like the Johnson-Cousins-Glass
UBVRIJHKLMN one, have been
defined using energy-amplifier devices. In this latter case,
energy integration, i.e.
The starting point of our work are extended libraries of stellar
intrinsic spectra
,
as derived from atmosphere calculations
for a grid of effective temperatures
,
surface gravities g,
and metallicities
.
The particular library we adopt will be
described in Sect. 3.
From this library, we aim to derive the absolute magnitudes
for each star of known
-
and hence known
.
This can be obtained by means of
Eq. (2) (or (3)), once a distance
of d=10 pc is assumed, i.e.
Substituting Eqs. (3) and (6)
into Eq. (5), we get
To keep consistency with our previous works (e.g. Salasnich et al. 2000), we adopt
,
and
(Bahcall et al. 1995).
By means of Eq. (7), we tabulate
for all
spectra in our input library, and for several different photometric
systems. The
can be then derived for any
intermediate
value, by interpolation
in the existing grid. We adopt simple
linear interpolations, with
,
,
and [M/H] as the
independent variables.
Next, to attribute absolute magnitudes to stars of given
along an isochrone, we simply compute
with Eq. (6), and hence
Finally, it is worth mentioning that the newly-defined SDSS photometric system makes use of an unusual definition for magnitudes (see Lupton et al. 1999). This specific case, for which some of the above equations do not apply, will also be discussed in a subsequent paper of this series.
By photometric zero-points, one usually means the constant quantities
that one should add to instrumental magnitudes in order to
transform them to standard magnitudes, for each filter
.
In the formalism here adopted, however, we do not
make use of the concept of instrumental magnitude, and hence
such constants do not need to be defined. Throughout this work,
instead, by "zero-points'' we refer to the quantities in
Eqs. (2) and (3) that depend only
on the choice of
and
.
They are constant for each filter, and are responsible for
the conversion of the synthetic magnitude scale into a standard
system.
As for these quantities, there are four different cases of interest.
Calibrated empirical spectra of Vega are available (e.g. Hayes & Latham
1975; Hayes 1985), covering the wavelength range from 3300 to
10 500 Å, an interval that can be extended up to 1150 Å when
complemented with IUE spectra (Bohlin et al. 1990).
They can be used to define VEGAmag systems in the optical
and ultraviolet. However, as the wavelength range accessible
to present instrumentation is much wider, a Vega spectrum covering
the complete spectral range has become necessary. Synthetic spectra
as those computed by Kurucz (1993) and Castelli & Kurucz (1994),
fulfill this aim. In this case, the predicted fluxes at Vega's
surface,
,
are scaled by the geometric dilution factor
More recently, composite spectra of Vega have been constructed by
assembling empirical and synthetic spectra together
(e.g. Colina et al. 1996), so that some small deficiencies
characteristic of synthetic spectra
are corrected.
This has the precise scope of providing a reference spectrum for
conversions between apparent magnitudes of real (observed)
stars, and physical fluxes.
However, it is not clear whether such composite Vega
spectrum should be preferable when synthetic photometry
is performed on theoretical spectra, as in the present work.
For instance, if the ATLAS9 spectrum for Vega has the core of
Balmer lines differing by as much as
10 percent from the observed ones (cf. Colina et al. 1996),
it is probable that the same deviations will be present in all Kurucz
spectra of comparable temperatures/gravities. If this is the case,
the synthetic Vega spectrum would probably give better zero-points
for these stars than the composite Colina et al. (1996) one.
For this reason, we simply adopt the synthetic ATLAS9
model for Vega, with
K,
,
,
and microturbulent velocity
,
the spectrum being provided by Kurucz (1993).
Castelli & Kurucz (1994) have computed a higher-resolution spectrum
for the same model, using the more refined ATLAS12 code. As
discussed by these authors, ATLAS9 and ATLAS12 spectra for
Vega are almost identical.
Once the synthetic model
is chosen,
we just need to adopt a fixed value for the dilution factor
(R/d)2, in order to have
at the
Earth's surface (outside the atmosphere).
Two choices are possible then: we
either (i) adopt an observed value of
as input to Eq. (9),
or (ii) adopt the observed Vega flux as measured at the
stellar surface, at a given wavelength, as an input to
Eq. (1).
Since direct measures of
are relatively more
uncertain than direct measures of
,
we prefer to adopt the second alternative: Taking the flux values
at 5556 Å from Hayes (1985;
), and at 5550 Å from
Kurucz (1993) Vega model
(
erg s-1 cm-2 Å-1),
we obtain
.
This
value implies an angular diameter of
mas
(Eq. (9)) for Vega,
that compares very well with the observed values of
mas (Code et al. 1976) and
mas (Ciardi et al. 2000).
It is worth remarking that, since the zero-points in
VEGAmag systems are attached
to the observed Vega fluxes, their synthetic absolute magnitudes
may have systematic errors of a few hundredths of
magnitude (say up to 0.03 mag), which is the typical magnitude of
errors in measuring fluxes at the Earth's surface. Somewhat smaller
errors, however, are expected in the colours.
These uncertainties will probably not be eliminated unless
definitive
and
measurements become available.
This means that a reference spectrum of
constant flux density per unit frequency
This definition can be extended to any filter system, provided that
we replace the monochromatic flux
with the
photon counts over each pass-band
obtained from the star,
compared to the photon counts that one would get by observing
:
It is worth mentioning that different practical implementations of
the ABmag system have been defined over the years (e.g. Oke & Gunn
1979; and Fukugita et al. 1996).
They differ only in the definition of the reference
stars (or reference stellar spectra) used as spectrophotometric
standards during the conversion from observed
instrumental magnitudes into fluxes
(that are used
in Eq. (10)). Since we are dealing
with synthetic spectra only, such a conversion is not necessary in our
case. It follows that these different definitions are not a
point of concern to us.
In this case, we are forced to use empirical spectra of standard
stars in order to define
and
.
A good set is provided by the four metal-poor subdwarfs
BD +17
4708, BD+26
2606, HD 19445 and HD 84937, which
are widely-used spectrophometric secondary standards
(Oke & Gunn 1983), as well as standards for several photometric
systems.
Actually, the present work does not deal with any "standard stars''
system, and this case is here included just for the sake of
completeness.
Details about a few specific systems - including the possible
choices for
- will be given in forthcoming papers.
In the following, we will present the stellar spectral library
put together for this work. For the sake of reference,
Fig. 1 presents the distribution of all spectra
in the
plane.
![]() |
Figure 1:
Distribution of the
|
| Open with DEXTER | |
Earlier Padova isochrones were based on the Kurucz (1993)
libraries of ATLAS9 synthetic atmospheres.
As discussed in a series
of papers by Castelli et al. (1997), Bessell et al. (1998),
and Castelli (1999), these models are superseded by now.
Firstly, small discontinuities associated to the scheme of
"approximate overshooting'' initially adopted by Kurucz have
been corrected (cf. Bessell et al. 1998).
Secondly, no-overshooting
models have been demonstrated to produce
-colour relations
in better agreement with empirical ones, at least for stars hotter
than the Sun (Castelli et al. 1997).
In the present work, we adopt the ATLAS9
no-overshoot models that have been calculated by
Castelli et al. (1997). They correspond to the "NOVER''
files available at http://cfaku5.harvard.edu/grids.html.
The metallicities cover the values
,
-2.0, -1.5,
-1.0, -0.5, 0.0, and +0.5, with solar-scaled abundance ratios.
A microturbulent velocity
,
and a mixing length
parameter
,
are adopted.
Notice that these models are now being extended so as to include
also
-enhanced chemical mixtures, which represents a potentially
important improvement for our future works.
Kurucz models cover quite well the region of the
vs.
plane actually occupied by stars,
at least in the
,
intervals (see Fig. 1).
However, it has to be extended to
both lower and higher
s, as will be detailed below.
It is important to recall that Kurucz (ATLAS9) spectra are widely used in the field of synthetic photometry, mainly because of their wide coverage of stellar parameters and easy availability. Moreover, there are also good indications in the literature that these spectra do a good job in synthetic photometry, provided that we are dealing with broad-band systems. Compelling examples of this can be found in Bessell et al. (1998), who compares the UBVRIJHKL results obtained from the recent ATLAS9 spectra to empirical relations derived with the infrared flux method, lunar occultations, interferometry, and eclipsing binaries. Their results indicate that the 1998 ATLAS9 models are well suited to synthetic photometry, but for small errors, generally lower than 0.1 mag in colours, that we do not consider as critical. In fact, we are more interested in the overall dependencies of colours and magnitudes with stellar parameters - probably well represented by present synthetic spectra - than on details of this order of magnitude.
Additionally, Worthey (1994) presented extensive comparisons between Kurucz (1993) spectra and stars in the low-resolution spectral library by Gunn & Stryker (1983), obtaining generally a good match for wavelengths redder than the B pass-band. Worthey's Fig. 9 also presents a comparison between Kurucz (1993) solar spectra and Neckel & Labs (1984) data, with excellent results (errors lower than 0.1 mag) all the way from the UV up to the near-IR. Since the ATLAS9 1998 spectra differ just little from the Kurucz (1993) version (a few percent in extreme cases), these results are to be considered still valid.
The previously mentioned works point to a reasonably good agreement between ATLAS9 spectra and those of real stars of near-solar metallicity, especially in the visual and near-infrared pass-bands. However, there are many known inadequacies in these spectra, which should be kept in mind as well. Here, we give just a brief list of the potential problems, concentrating on those which may be more affecting our synthetic colours.
ATLAS9 spectra are based on 1D static and plan-parallel LTE model atmospheres, which use a huge database of atomic line data (Kurucz 1995). The line list is known not to be accurate: In fact, Bell et al. (1994) show that the solar spectra calculated using Kurucz list of atomic data present many unobserved lines; moreover, the number of lines which are too strong exceeds those which are too weak. The problem can be appreciated by looking at the high-resolution spectral plots presented by Bell et al. (1994), but could hardly be noticeable in low-resolution plots (such as in the comparisons presented in Worthey's 1994 Fig. 9, and in Castelli et al. 1997 Fig. 2).
Also, Bell et al. (2001) show that a motivated increase in
the Fe I bound-free opacity cause a significant
improvement in the fitting of the solar spectrum in the
3000-4000 Å wavelength region, affecting the entire
UV region as well. Such increased sources of continuous
opacity are still missing in ATLAS9 atmospheres
.
These results indicate that
ATLAS9 spectra will produce worse results when applied to
(i) narrow-band photometric systems, in which individual metallic
lines can more significantly affect the colours, and (ii) in the UV
region, especially shortward of 2720 Å (see Bell et al. 2001).
In both cases, the errors caused by wrong atomica data are such that
we can expect not only systematic and
-dependent
offsets in synthetic colours,
but also a somewhat wrong dependence on metallicity.
Clearly, these points are worth being properly investigated by
means of detailed spectral comparisons.
Regarding the present work, the above-mentioned problems (i) critically determine the inadequacy of synthetic colours computed for the Strömgren system (Girardi et al., in preparation), and (ii) may possibly cause significant errors in our synthetic HST/WFPC2 UV colours.
Other potential problems worth of mention are:
Finally, we remark that some authors (Lejeune et al. 1997, 1998)
propose the application of a posteriori transformations
to Kurucz (1993) spectra, as a function of wavelength and
,
such as to reduce the errors of the derived synthetic UBVRIJHKL
photometry. In our opinion,
such transformations are questionable because they do
not correct the cause of the discrepancies - majorly
identifiable in the imperfect modelling of absorption lines -
and the case for applying them to stars of all surface
metallicities and gravities is far from compelling.
For
K, we simply assume black-body spectra.
This is probably a good approximation for wavelengths
Å. In fact, we find always a reasonably smooth
transition in the computed
s as we cross the
K temperature boundary.
Synthetic spectra for M giants have still many problems - mainly in their ultraviolet-blue region - that partially derive from incomplete opacity lists of molecules such as TiO, VO and H2O (see e.g. Plez 1999; Alvarez & Plez 1998; Alvarez et al. 2000; and Houdashelt et al. 2000a,b to appreciate the state of the art in the field).
Therefore, we prefer to use the empirical M giant spectra from Fluks et al. (1994; or "intrinsic'' spectra as referred in their paper). They cover the wavelength interval from 3800 Å to 9000 Å. Outside this interval, the empirical spectra have been extendend with the "best fit'' synthetic spectra computed by the same authors.
However, the whole procedure reveals a problem:
if we simply merge empirical and synthetic spectra from
Fluks et al. (1994), the resulting synthetic
and
colours
just badly correlate with the measured colours for the
same stars (which were also obtained by Fluks et al. 1994).
This problem probably derives from a
bad flux calibration at the blue extremity
of the observed spectra and/or from the imperfect match between
synthetic and observed spectra at 3800 Å. In order
to circumvent (at least partially) the problem, we simply
multiply each M-giant spectrum blueward of 4000 Å (with a smooth
transition in the range from 4000 Å to 4800 Å) by a constant,
typically between 0.8 and 1.2, so that the synthetic colours recover
the observed behaviour of the
vs.
data.
The first two panels of Fig. 2 show the results.
![]() |
Figure 2:
Colour vs. |
| Open with DEXTER | |
Actually, Fig. 2 presents six different
colour vs.
diagrams that are useful to understand the
situation for giants. Care has been taken in expressing data and models
in the same photometric system, the "Bessell''
UBVRIJHK one, that we will detail later in Sect. 4.1.
For M giants, the empirical photometric data from Fluks et al.
(1994; small dots) can be compared with the results of our
synthetic photometry
. Noteworthy, there is a
reasonably good match between the synthetic and observed relations
for most colours. This has been imposed for
and
,
whereas is
a natural result for all colours involving wavelengths longer
than
4800 Å. The only clear exception is the
colour,
for which differences of
0.4 mag are found for all giants
of spectral type later than M4 (
). The reason for this
discrepancy is not clear, but may lie in the use of R filters
with different transmission curves. Also the predictions for
do not fit well all the photometric data, somewhat failing
for the spectral types later than M7 (
). However, since
these latters are quite rare, such mismatch does not pose a
serious problem.
For the sake of comparison, Fig. 2
also presents the relations obtained by means of
the M-giant models from Houdashelt et al. (2000a), in the
case of solar metallicity. Together with other recent examples
(e.g. Plez 1999; Alvarez et al. 2000), they represent
state-of-the-art computations of cool oxygen-rich stellar
atmospheres. As can be appreciated in the figure,
Houdashelt et al. models reproduce well the empirical data as
far as
(spectral types earlier than M5), but start
departing from these for cooler stars. A similar situation
holds if we look at different
-colour relations, as
can be seen in Figs. 13 and 14 of Houdashelt et al. (2000a),
where they compare their
-colour relations with those
obtained with Fluks et al. (1994) spectra and data for field
giants. Also in this case, it seems that Fluks et al. (1994)
spectra do better reproduce the empirical relations for the
spectral types later than M4.
Once we have defined the library of M-giant spectra,
we associate effective temperatures to them by using the scale
favoured by Fluks et al. (1994). In this scale, M giants cover
the temperature interval from 3 850 K
(MK type M0) to 2500 K (MK type M10).
We recall that Fluks et al. (1994)
values
are derived from a careful fitting of the observed spectra with
synthetic model atmospheres of solar metallicity. Their scale is also
in excellent agreement with the empirical one from Ridgway et al.
(1980), which covers spectral types earlier than M6.
After the proper
is attributed, each one of our modified
spectra is completely re-scaled by a constant, so that the
total flux vs.
relation - i.e.
- is recovered.
Finally, we face the problem of defining the transition between the M-giant spectra, and the ATLAS9 ones which are available for temperatures higher than 3500 K. To this aim, it is helpful to examine Fig. 2, where we also include:
From inspecting this and other similar plots, we can conclude that
the mismatch between Kurucz ATLAS9 and
Fluks et al. (1994) spectra starts at about
and
increases slowly as the temperature decreases down to 3500 K
(i.e. from
to
).
Hence, we adopt a smooth transition between these two spectral
sources over this temperature interval. The same
M giant spectra are assumed for all metallicities.
The complete procedure ensures reasonable colour vs.
relations
for all giants of near-solar
metallicity (Fig. 2). Nevertheless, this kind
of approach cannot be completely satisfactory, first because the
original Fluks et al. (1994) spectra have been artificially
corrected at wavelengths shorter than 4800 Å in order to produce
reasonable
and
,
and second because we do not dispose of similar M-giant spectra for
metallicities very different from solar. Better empirical and
theoretical spectra for M giants seem to be urgently needed.
Anyway, in the context of the present work the problem is not
dramatic because M giants cooler than
K are only
found in the RGB-tip and TP-AGB phases of high metallicity stellar
populations, and constitute just a tiny fraction of the number of
red giants. The problem could be critical, instead, when we consider
integrated properties of stellar populations, because M giants,
despite their small numbers, have high luminosities and
contribute a sizeable fraction of the integrated light.
Although the modelling of cool dwarfs atmospheres presents challenges comparable to those found in late-M giants (e.g. the inadequacy of TiO and H2O line lists, and dust formation; see Tsuji et al. 1996, 1999; Leggett et al. 2000), present results compare reasonably well with observational spectral data (see e.g. Fig. 9 in both Leggett et al. 2000 and 2001). A review on the subject can be found in Allard et al. (1997).
An extended library of synthetic spectra for cool dwarfs (of types M and later) is provided by Allard et al. (2000a; see ftp://ftp.ens-Lyon.fr/pub/users/CRAL/fallard). We use their set of "BDdusty1999'' atmospheres (see also Chabrier et al. 2000; Allard et al. 2000b, 2001), that should supersede the "NextGen'' models from the same group (Hauschildt et al. 1999) due to the consideration of better opacity lists and dust formation. Dust can significantly affect the coolest atmospheres, corresponding to dwarfs of spectral types L and T.
The selected spectra cover the
intervals:
We find that there is a good agreement between
ATLAS9 and BDdusty1999 spectra in the
range between
3800 K and 4000 K. Then, we set the transition between
ATLAS9 and BDdusty1999 spectra at
3900 K. This choice
guarantees smooth
vs. colour relations for dwarfs.
In this section we present the basic information regarding the filter transmission curves and zero-points for each photometric system. As a reference to the discussion, Fig. 3 presents the filter sets under consideration, as compared to the spectra of a hot (Vega), an intermediate (the Sun), and a cool star (an M5 giant).
![]() |
Figure 3:
The filter sets used in the
present work. From top to bottom, we show the
filter+detector transmission curves |
| Open with DEXTER | |
Aiming to reproduce the Johnson-Cousins-Glass system, we adopt the filter pass-bands indicated by Bessell (1990; for Johnson-Cousins UBVRI) and Bessell & Brett (1988; for JHK). We also apply their prescription for computing the U-B colour by means of a slightly modified pass-band BX90, instead of the normal B one. Moreover, in order to better recover the original system, we adopt energy instead of photon count integrations (see Sect. 2.1).
It is worth recalling that these pass-bands represent just one specific version of the "standard'' Johnson-Cousins-Glass system, that may differ from filter systems in usage at several observatories. The Bessell & Brett (1988) JHKLM pass-bands, for instance, represent an effort in the direction of homogenizing several different near-infrared systems (SAAO, ESO, CIT/CTIO, MSO, AAO, and Arizona). In Bessell (1990) and Bessell & Brett (1988), the reader can find a set of useful fitting relations between colours in the several original systems.
As previously mentioned, Johnson-Cousins-Glass is essentially a VEGAmag system. We fix the zero-points by assuming that Vega has apparent magnitudes equal to 0.03 in all UBVRIJHK bands, i.e. we impose all colours to be null. Notice that our definition is very similar to the Bessell et al. (1998) one, who adopt Vega colours differing from zero by just some thousandths of a magnitude (see their Table A1).
In the context of the present work, the distinctive feature of HST photometry is the use of ABmag and STmag systems, which greatly simplifies the definition of zero-points. WFPC2 and NICMOS observations can also be expressed in VEGAmag magnitudes.
As for the WFPC2, we produce bolometric corrections and magnitudes in the F170W, F218W, F255W, F300W, F336W, F439W, F450W, F555W, F606W, F702W, F814W, and F850LP filters. Similar tables have been produced in previous papers (Chiosi et al. 1997; Salasnich et al. 2000); the present ones differ just in minor details.
The transformations have been computed in STmag, ABmag, and VEGAmag systems. Whereas the STmag and ABmag systems can be straightforwardly simulated, the VEGAmag one deserves some comments.
According to the SYNPHOT package distributed with the STSDAS software, in a VEGAmag system Vega should have apparent magnitudes equal to zero in all pass-bands. However, the most widely used calibration of WFPC2 photometry comes from Holtzman et al. (1995), who adopt a set of zero-points in which Vega has apparent magnitudes U=0.02, B=0.02, V=0.03, R=0.039, I=0.035. Accordingly, we choose this latter definition, and impose that for the WFPC2 filters that correspond to UBVRI in wavelength, the synthetic magnitudes of Vega have these same values. For filters of intermediate wavelength, we adopt a linear interpolation between these values, whereas for bluer and redder filters a Vega magnitude equal to zero is assumed.
As for the
functions, we use the
pre-launch pass-bands kindly provided by Jon Holtzman
(see Holtzman et al. 1995). We recall that,
owing to the presence of contaminants inside the WFPC2
(see Baggett & Gonzaga 1998; Holtzman et al. 1995),
changes slowly with time, especially for UV filters.
To cope with this, observers usually apply small corrections
to the definition of the instrumental magnitudes,
in order to bring the magnitudes back to the original conditions
(see Holtzman et al. 1995). This justifies our use of
pre-launch pass-bands instead of the present-day ones
provided by SYNPHOT.
For NICMOS filters, we compute bolometric corrections and absolute magnitudes in the ABmag, STmag, and VEGAmag systems. For the moment, calculations are limited to the three most frequently used filters, i.e. F110W, F160W, and F205W. The pass-bands come from SYNPHOT, and have been kindly provided by Don Figer.
NICMOS observations are also frequently expressed in units
of milli-Jansky (mJy). The conversion between AB magnitudes and
mJy is straightforward:
| (16) |
The EIS survey (Renzini & da Costa 1997; da Costa 2000) aims at providing a large database of deep photometric data, among which the astronomical community could select interesting targets for VLT spectroscopy. The survey is conducted at several different instruments at ESO.
The Wide Field Imager (WFI) at the
MPG/ESO 2.2 m La Silla telescope provides imaging of excellent
quality over a
field of view.
It contains a peculiar set of broad-band filters,
very different from the "standard'' Johnson-Cousins ones.
This can be appreciated in Fig. 3; notice in
particular the particular shapes of the WFI B and I
filters. Moreover, EIS makes use of the WFI Z filter which
does not have a correspondency in the Johnson-Cousins system.
Given the very unusual set of filters, the importance of computing isochrones specific for WFI is evident. This has benn done so for the broad WFI filters U (ESO#841), B (ESO#842), V (ESO#843), R (ESO#844), I (ESO#845), and Z (ESO#846), that - here and in Fig. 3 - are referred to as UBVRIZ for short.
Bolometric corrections have been computed in the VEGAmag system assuming all Vega apparent magnitudes to be 0.03, and in the ABmag system, which is adopted by the EIS group. The photometric calibration of EIS data is discussed in Arnouts et al. (2001).
It is very important to notice that any
photometric observation performed with WFI that makes use
of standard stars (e.g. Landolt 1992) to convert WFI instrumental
magnitudes to the standard Johnson-Cousins UBVRI system,
will not be in the WFI VEGAmag system we are dealing
with here. Instead, in that case, we should better
compare the observations with the isochrones in the
standard Johnson-Cousins system, or, alternatively, apply
colour transformations to our WFI isochrones so that they
reproduce the
-colour sequences of dwarfs and giants
in the Johnson-Cousins system. This aspect will be better
illustrated Sect. 6.
SOFI is a near-infrared imager and grism spectrograph at
the ESO NTT 3.6 m telescope. It is used to complement WFI observations in
near-infrared pass-bands. More specifically, it disposes of
J, H and
filters
that have some similarity to Glass JHK (see Fig. 3).
VEGAmag magnitudes are computed assuming the same as before, i.e.
that Vega apparent magnitudes are 0.03.
EMMI is a visual imager and grism spectrograph also at
the NTT. The EIS project uses a set of its
wide filters, i.e.
,
,
,
and
,
together with the
R filter. The pass-bands have been kindly provided by S. Arnouts.
As before, VEGAmag magnitudes are computed assuming that Vega
has 0.03 mag in all filters.
The Washington system, originally defined by G. Wallerstein and developed by Canterna (1976), has been more and more used since Geisler (1996) defined a set of CCD standard fields. In the present paper, we reproduce the Washington CCD system (filters C, M, T1 and T2) by adopting the transmission curves as revised by Bessell (2001).
Following Geisler (1996), the Washington T1 filter has been frequently replaced by the Kron-Cousins filter R, which presents a similar transmission curve and is available in almost all observatories. Additionally, Holtzman et al. (in preparation) suggest the use of BVI colours together with Washington ones for breaking the age-metallicity degeneracy of stellar populations in colour-colour diagrams. For these reasons, in all tables that deal with the Washington C M T1 T2 system, we also insert the information for the Johnson-Cousins BVRI filters.
Finally, following Geisler (private communication), the zero-points should be well represented by a VEGAmag system. We assume Vega has magnitude 0.03 in all filters.
Forthcoming papers of this series will be dedicated to
The tables of bolometric corrections here described have been
primarily constructed to be applied to the Padova database of
stellar evolutionary tracks and isochrones
. These latter have been described in several
previous papers, and a complete description of them is
beyond the scope of this work.
In the following, our intention is just to briefly mention the sets of isochrones which are the most useful for comparisons with observed photometric data, and to first mention some data that has not been published in precedence. A summary table of the available material is presented in Table 1.
| Initial chemical comp.: | Evolutionary tracks: | Isochrones: | ||||||||
| Mass ranges (in |
TP-AGB | convec- | age range | filename in | basic | |||||
| Z | Y | kind1 | 0.15-0.55 | 0.6-7.0 | >7.0 | evolution3 | tion4 |
|
database | reference2 |
| 0.0 | 0.230 | S | - | Ma01 | Ma01 | - | O | 6.30 - 10.25 | isoc_z0.dat | Ma01 |
| 0.0001 | 0.230 | S | Gi01 | Gi01 | Gi96 | G | O | 6.60 - 10.25 | isoc_z0001.dat | Gi01+Gi96 |
| 0.0004 | 0.230 | S | Gi00 | Gi00 | Fa94a | G | O | 6.60 - 10.25 | isoc_z0004.dat | Gi00+Be94 |
| 0.001 | 0.230 | S | Gi00 | Gi00 | - | G | O | 7.80 - 10.25 | isoc_z001.dat | Gi00 |
| 0.004 | 0.240 | S | Gi00 | Gi00 | Fa94b | G | O | 6.60 - 10.25 | isoc_z004.dat | Gi00+Be94 |
| 0.008 | 0.250 | S | Gi00 | Gi00 | Fa94b | G | O | 6.60 - 10.25 | isoc_z008.dat | Gi00+Be94 |
| 0.019 | 0.273 | S | Gi00 | Gi00 | Br93 | G | O | 6.60 - 10.25 | isoc_z019.dat | Gi00+Be94 |
| 0.030 | 0.300 | S | Gi00 | Gi00 | - | G | O | 7.80 - 10.25 | isoc_z030.dat | Gi00 |
| 0.019 | 0.273 | S | Gi00 | Gi00 | - | G | C | 7.80 - 10.25 | isoc_z019nov.dat | Gi00 |
| 0.008 | 0.250 | S | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z008s.dat | Sa00 |
| 0.019 | 0.273 | S | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z019s.dat | Sa00 |
| 0.040 | 0.320 | S | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z040s.dat | Sa00 |
| 0.070 | 0.390 | S | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z070s.dat | Sa00 |
| 0.008 | 0.250 | A | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z008a.dat | Sa00 |
| 0.019 | 0.273 | A | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z019a.dat | Sa00 |
| 0.040 | 0.320 | A | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z040a.dat | Sa00 |
| 0.070 | 0.390 | A | Sa00 | Sa00 | Sa00 | G | O | 7.00 - 10.25 | isoc_z070a.dat | Sa00 |
| 0.004 | 0.240 | S | Gi00 | Gi00 | - | M | O | 7.80 - 10.25 | isoc_z004m.dat | MG01 |
| 0.008 | 0.250 | S | Gi00 | Gi00 | - | M | O | 7.80 - 10.25 | isoc_z008m.dat | MG01 |
| 0.019 | 0.273 | S | Gi00 | Gi00 | - | M | O | 7.80 - 10.25 | isoc_z019m.dat | MG01 |
|
1 S indicates a solar-scaled distribution
of metals, A indicates an 2 References for tracks and isochrones: Be94 = Bertelli et al. (1994, A&AS, 106, 275); Br93 = Bressan et al. (1993, A&AS, 100, 647); Fa94a = Fagotto et al. (1994a, A&AS, 104, 365); Fa94b = Fagotto et al. (1994b, A&AS, 105, 29); Gi96 = Girardi et al. (1996, A&AS, 117, 113); Gi00 = Girardi et al. (2000, A&AS, 141, 371); Gi01 = Girardi (2001, unpublished); Ma01 = Marigo et al. (2001, A&A, 371, 152); MG01 = Marigo & Girardi (2001, A&A, 377, 132); Sa00 = Salasnich et al. (2000, A&A, 361, 1023). 3 G means a simple synthetic evolution as in Girardi & Bertelli (1998), whereas M stands for more detailed calculations as in Marigo (2001; and references therein). 4 O means a model with overshooting (see Gi00 for all references), whereas C corresponds to classical semi-convective models. |
Girardi et al. (2000) computed a set of low- and
intermediate-mass stellar tracks which supersedes
those previously used in Bertelli et al. (1994) isochrones.
Additional models (unpublished)
have been recently computed for initial chemical
composition
[Z=0.0001, Y=0.23].
Thus, we have created a new set of isochrones combining
the latest low- and intermediate mass tracks (in the range
0.15 - 7.0
)
with the formerly
available massive ones. The full references are given in
Table 1.
In all cases in which "2000'' and "1994'' tracks have been combined,
we find excellent agreement between the relevant quantities (lifetimes,
tracks in the HR diagram) at the transition mass of 7-8
.
This is explained considering
that the intermediate- and high-mass models share the
same prescription for convection, and have interior opacities dominated
by electron scattering (which has not been changed in the meanwhile).
For the solar metallicity, we have combined tracks presenting
slightly different initial metallicities -
[Z=0.019, Y=0.273] in Girardi et al. (2000),
and
[Z=0.020, Y=0.280] in Bressan et al. (1993) -
without finding any significant discontinuity.
Finally, to this extended set we have included the Marigo et al. (2001) isochrones for zero-metallicity stars.
For solar metallicity and in the mass range
0.15 - 7.0
,
Girardi et al. (2000) presents an additional set of tracks and
isochrones computed with the
classical semi-convective prescription for convective borders.
Then, the two
[Z=0.019, Y=0.273] sets are useful if one
chooses to compare classical with overshooting models.
The same kind of work is being extended to metallicities
[Z=0.004, Y=0.240] and
[Z=0.008, Y=0.250] (Barmina et al. 2002),
and will be included in the database when completed.
Salasnich et al. (2000) presents new
models for 4 different metallicities
(
[Y=0.250, Z=0.008],
[Y=0.273, Z=0.019],
[Y=0.320, Z=0.040]
and
[Y=0.390, Z=0.070]), computed both with scaled-solar and
alpha-enhanced distributions of metals. The tracks cover the
mass range from 0.15 to 20
.
They represent a valid
alternative to the isochrones referred to in Sect. 5.1,
but do not cover the low-metallicity interval.
Anyway, it has been demonstrated by Salaris et al. (1993; see
also Salaris & Weiss 1998; and VandenBerg 2000),
that for low metallicities one may safely use scaled-solar
stellar models instead of
-enhanced ones of same Z.
All the tracks and isochrone sets above mentioned, include the complete TP-AGB phase as computed with a simple synthetic algorithm (Girardi & Bertelli 1998). In parallel, Marigo (2001, and references therein) has developed a much more sophisticated code for synthetic TP-AGB evolution, which includes crucial processes such as the third dredge-up and hot-bottom burning. Sets of complete TP-AGB tracks have been so far presented for metallicities [Y=0.240, Z=0.004], [Y=0.250, Z=0.008], and [Y=0.273, Z=0.019] (Marigo 2001). A set of isochrones has been generated by combining these detailed TP-AGB tracks with the previous evolution from Girardi et al. (2000); they are presented in the appendix of Marigo & Girardi (2001).
These isochrones represent a useful alternative to the isochrones referred to in Sect. 5.1, any time the TP-AGB population is under scrutiny - for instance, when we have near-infrared photometry of objects above the RGB-tip. Marigo TP-AGB models are being extended to cover a larger metallicity interval.
This work is dedicated to the presentation of theoretical isochrones in several photometric systems. It represents the continuation of a wide project of the Padova group, started with Bertelli et al. (1994) and then carried on by Chiosi et al. (1997), and more recently by Salasnich et al. (2000). It starts describing the formalism for converting synthetic stellar spectra into tables of bolometric corrections (Sect. 2), in such a way that it can be easily applied to different photometric systems, and with the possibility of including extinction in a self-consistent way.
![]() |
Figure 4: Comparison of Girardi et al. (2000) isochrones transformed to Johnson-Cousins-Glass magnitudes and colours by using either present relations (continuous lines) or Bertelli et al. (1994) ones (dashed lines), in several CMDs. The isochrones have solar metallicity (Z=0.019) and ages 108, 109, and 1010 yr (from top to bottom). |
| Open with DEXTER | |
![]() |
Figure 5: Comparison of Girardi et al. (2000) isochrones as transformed to the WFPC2 VEGAmag system using either present relations (continuous lines) or Salasnich et al. (2000) ones (dashed lines). The isochrone ages and metallicities are the same as in Fig. 4. |
| Open with DEXTER | |
Then, we describe the assemblage of an updated library of stellar
spectra (Sect. 3). The library is quite
extended in
and
,
and includes the crucial dependence
of spectral features on metallicity. Of course, it suffers from some
limitations:
very hot stars and M-giants are not included among synthetic spectra,
a situation which can be remediated by using blackbody and empirical
spectra, respectively. The strinkingly different spectra of
carbon stars will also have to be
considered in the future (Marigo et al., in preparation).
These are probably the points where the models can be most improved.
Moreover, several problems may be affecting the ATLAS9
synthetic spectra we are using to simulate the broad-band
colours of most stars
(see Sect. 3.1). Although such spectra
have been demonstrated to be suitable for
synthetic photometry (mainly for the Johnson-Cousins-Glass
system; e.g. Bessell et al. 1998), their accuracy
has still to be sistematically evaluated for stars of all
metallicities, temperatures and gravities.
Anyway, we assume that they
are good enough for simulating broad-band photometric systems
in the visual-infrared wavelength region, whereas
expect that the results in narrow-band systems, and in the
ultraviolet pass-bands, will be affected by more significant
errors.
Another important aspect of synthetic spectra is that they
are usually computed for scaled-solar chemical compositions,
whereas the extension to peculiar and
-enhanced mixtures
would be of high interest. This latter problem will probably be
alleviated in a near future, with the release of extensions
to ATLAS9 spectra.
From the spectral library, we derive bolometric corrections for each pass-band mentioned in Sect. 4, and apply them to the Padova isochrones. In practice, only in few cases we present newly-constructed isochrones: the bulk of isochrone data is already described in previous papers by our group, and it is only the transformation from theoretical quantities to absolute magnitudes that changes compared to past releases. Section 5 summarizes the basic characteristics of the different sets of isochrones, indicating the full references.
It is important to illustrate the differences between the present and previous transformations. The previous ones for UBVRIJHK are fully described in Bertelli et al. (1994), and were adopted by Girardi et al. (2000), Salasnich et al. (2000) and Marigo et al. (2001); for HST/WFPC2 photometry, they are the ones described in Salasnich et al. (2000).
The situation for Johnson-Cousins-Glass is tentatively illustrated in Fig. 4, which compares a set of Girardi et al. (2000) isochrones, transformed according to both present (continuous lines) and Bertelli et al. (1994; dashed lines) transformations. We point out that:
From the plots at the top row of Fig. 5, one can
also appreciate the unusual appearance of isochrones in CMDs
that involve ultraviolet WFPC2 pass-bands: Notice for instance that
in F170W, F218W, F255W and F330W magnitudes, giants may be fainter
than turn-off stars. Isochrones in the F218W vs. F170W-F218W and
F255W vs. F218W-F255W diagrams are even "twisted'', because the
vs. colour relations are not monotonic for
these filters. These effects are related to the presence of a
red leak in the ultraviolet HST filters (for both the present WFPC2
and the former FOC camera), and are extensively
discussed by Yi et al. (1995) and Chiosi et al. (1997).
As a consequence of the great similarity between present and
previous UBVRIJHK and HST/WFPC2 transformations,
for most colours and over a large portion of the HR diagram,
most results derived from previous Padova isochrones
are not expected to change.
Exceptions may show up for works that are concerned with
the photometry of the reddest giants, with
K
(
), or that deal with low-mass main-sequence stars
in the
and ultraviolet colours.
![]() |
Figure 6: Isochrones in the CMDs of NICMOS ABmag photometry. Ages and metallicities are the same as in Fig. 4. |
| Open with DEXTER | |
![]() |
Figure 7: Isochrones in the T1 vs. C-T1 plane of Washington photometry. Left panel: from top to bottom, a sequence of Z=0.008 isochrones with ages 107, 108, 109, and 1010 yr. Right panel: from left to right, a sequence of 14 Gyr old isochrones with metallicities Z=0.0001, 0.0004, 0.001, 0.004, 0.008, 0.019, and 0.030. |
| Open with DEXTER | |
The greatest improvement of the present database is in the presentation of Padova isochrones in several photometric systems for which they were not available so far - including the case of brand-new systems. Three examples of theis kind are given in Figs. 6-8.
First, Fig. 6 presents the isochrones in NICMOS ABmag system. In a VEGAmag system, NICMOS isochrones would look similar to their equivalent Johnson-Cousins-Glass ones, shown in Fig. 4. In the ABmag system, however, they appear shifted to quite different colour and magnitude intervals.
Figure 7 illustrates how Padova isochrones look like in the T1 vs. C-T1 CMD of Washington photometry, both for varying age at constant metallicity (left panel), and for varying metallicity at constant age (right one). The striking feature in these plots is the excellent separation in metallicity offered by the C-T1 colour, from the main sequence up to red giant phases. This feature, combined to the excellent throughput in the C filter (Fig. 3), is among the advantages that make the Washington system a very competitive one if compared to Johnson-Cousins (see also Paltoglou & Bell 1994; Geisler & Sarajedini 1999).
Preliminary comparisons point to a good agreement
between our Washington isochrones and real data for LMC
fields from Bica et al. (1998). Just to mention an
example, we notice that C-T1 for giants
"saturates'' at
3.4, both in the models and in
the LMC data.
![]() |
Figure 8: Comparison between the same set of Z=0.019 isochrones as seen in the UBVI CMDs using either Johnson-Cousins (dashed lines) or WFI filters (continuous lines). VEGAmag systems are used in both cases. Ages are the same as in Fig. 4. |
| Open with DEXTER | |
An example of "new'' photometric system is provided
by the WFI, which has broad-band filters very different
from Johnson-Cousins ones. To illustrate the effect in
colours, Fig. 8 shows exactly the same
isochrones as seen in BVI CMDs
using either Johnson-Cousins or WFI filters, and applying
in both cases the VEGAmag definition of zero-points.
The differences are striking. In particular, since the BV
WFI filters represent a wavelength baseline shorter than the
Johnson ones, they provide a more modest separation of stars
in
colour. It is evident from this plot that the normal
Johnson-Cousins isochrones cannot be used to interpret WFI data that
has been converted to VEGAmag or ABmag systems, as for most of
EIS data (e.g. Arnouts et al. 2001; Groenewegen et al.
2002)
.
All the data here mentioned are available at the WWW site
http://pleiadi.pd.astro.it. The database already includes a
very large number of files, and is expected to increase further
as we publish data for other photometric systems. Thus, it is
hard to describe here both the structure of the database,
and the content of each file. Moreover, this kind of information
is probably useful just to whom actually accesses the database.
Thus, we opt to provide all the relevant information
in readme.txt files inserted in the database.
To the general reader, suffice it to briefly mention the kind of data which is available:
Acknowledgements
L.G. thanks the many people who helped by providing filter transmission curves and zero-points information (in particular E. Bica, D. Geisler, J. Holtzman, D. Figer, E. Grebel, M. Gregg, M. Rich, S. Arnouts, and L. da Costa). Particularly appreciated are the availability (R. Kurucz, F. Allard) and help with (I. Baraffe) on-line spectral data, the useful comments by B. Plez regarding cool giants, and the many useful remarks by R. Bell and M.S. Bessell, which greatly helped to improve this paper. Also acknowledged are those who kindly pointed out some mistakes in our preliminar releases of data. L.G. acknowledges a stay at MPA funded by the European TMR grant ERBFMRXCT 960086. This work was partially funded by the Italian MURST.