The main aim of this work is to derive empirical fitting functions for
the D4000 in terms of the stellar atmospheric parameters:
effective temperature, metallicity and surface gravity. After some
experimentation, we decided to use as
the temperature indicator, being [Fe/H] and
the parameters
for the metallicity and gravity. Following the previous works of
G93 and W94, the fitting functions are expressed as
polynomials in the atmospheric parameters, using two different
functional forms:
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(11) |
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(12) |
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(13) |
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Figure 6:
Details of the fitting functions in the mid-temperature range for
a) giant (![]() ![]() |
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Figure 7: Residuals of the derived fitting functions (observed minus predicted) against the three input stellar parameters. Symbol types are the same as in Fig. 3. The length of the error bar is twice the unbiased residual standard deviation |
The polynomial coefficients were determined from a least squares fit where all the stars were weighted according to the D4000 observational errors listed in Table 1. Note that this is an improvement over the procedure employed by G93 and W94 for the Lick indices.
Obviously, not all possible terms are necessary. The strategy followed to
determine the final fitting function is the successive inclusion of
terms, starting with the lower powers. At each step, the term which yielded a
lower new residual variance was tested. The significance of this
new term, as well as those of all the previously included coefficients, was
computed using a t-test (i.e. from the error in the coefficient, we tested
whether it was significantly different from zero). Note that this is
equivalent to performing a F-test to check whether the unbiased residual
variance is significantly reduced with the inclusion of the additional term.
Following this procedure, and using typically a
significant level of , only statistically significant terms were
retained. The problem is well constrained and, usually, after the inclusion of
a few terms, a final residual variance is asymptotically reached
and the higher order terms are not statistically significant. Throughout
this fitting procedure we also kept an eye on the residuals to assure that no
systematic behaviour for any group of stars (specially stars from any given
cluster or metallicity range) was apparent.
After a set of trial fits, it was clear that temperature is the main parameter
governing the break. Unfortunately, the behaviour of the D4000 could not
be reproduced by a unique polynomial function in the whole temperature range
spanned by the library, forcing us to divide the temperature
interval into several regimes. The derived composite fitting function is shown
in Fig. 5. In Table 3 we list the corresponding
coefficients and errors, together with the typical error of the N stars used
in each interval (), the
unbiased residual variance around the fit (
) and the
determination coefficient (r2).
In the high temperature regime (,
K) a
dichotomic behaviour for dwarfs and giants on one side, and supergiants on the
other, is clearly apparent. Therefore we derived different fitting functions
for each gravity range. For the first group the amplitude of the break is
quite constant and only the linear term in
is statistically
significant (note that we subdivide this range in two intervals to achieve a
better fit). The independence on metallicity is naturally expected (see
Sect. 2) but note that an important fraction of the stars in this range
either lack of a [Fe/H] estimation or are restricted to the solar value.
The behaviour of the cool stars (,
K) is more complex and [Fe/H] terms are
clearly needed. On the other hand, no gravity term is
significant. However, whilst for the giant stars D4000 increases
with
all the way up to
, for higher
gravities it reaches a maximum at
and then levels
off. Furthermore, separate fits for dwarfs and giants in this
range (with a gravity cutoff around 3-3.5) yield residual
variances that are significantly smaller than the variance from a
single fit. Hence, we have derived different fitting functions for
dwarfs and giants. This dichotomic behaviour of the break is not
surprising since its strength is quite dependent on the depth of the
CN bands (Fig. 1) which also shows a similar behaviour (G93)
due to the onset of the dredge-up processes at the bottom of the giant
branch. In Fig. 6 we show in detail the fitting functions
derived for each gravity group in this temperature range.
Concerning the cold stars (,
K), the
difference between giants and dwarfs is quite evident and two fitting
functions have been derived (see also Sect. 2). Again, the metallicity terms
are not significant, although this may be, at least in part, due to the
paucity of input metallicities in this range. It must be noted that the
different fitting functions have been constructed with the constrain of
allowing for a smooth transition in the predicted D4000 indices among the
different
and gravity ranges.
In Fig. 7 we plot the residuals from the fits as a
function of effective temperature, metallicity and gravity. Note that
no trends are apparent with any of these parameters. We have also
checked for systematic residuals within any of the star
clusters. Except for an unexplained negative offset for the Coma stars
(, not due to an error in the adopted
metallicity), no systematic offsets have been found. For the 420 stars
used in the fit, we derive an unbiased residual standard deviation
. This must be compared with the typical error
in the D4000,
. Therefore, the residuals
are, in the mean, a 2.5 factor larger than what should be expected
solely from measurement errors. Since we are quite confident that these
latter errors are realistic (see Sect. 5), and although
some scatter may arise from the fact than the fitting functions are
not able to reproduce completely the complex behaviour of the
D4000, most of the extra scatter must arise form uncertainties in
the input atmospheric parameters. For example, the residual D4000
scatter of 0.248 for the cool giants (at
and
) can be fully explained by the combined effect of a 166
K uncertainty in
and a 0.29 dex error in [Fe/H], both
consistent with the typical errors found by [53, Soubiran et al.
(1998)] when comparing atmospheric parameters from the
literature. Another quantitative measurement of the quality of the
present fitting functions is the determination coefficient for the
whole sample r2=0.96. This indicates that a 96% of the original
variation of the break in the sample is explained by the derived
fitting functions.
Since the goal of this work is to predict reliable D4000 indices for any given combination of input atmospheric parameters, we have investigated, using the covariance matrices of the fits, the random errors in such predictions. These errors are given in Table 4 for some representative sets of input parameters. Note that, as it should be expected, the uncertainties are smaller for near-solar metallicities. Interestingly, although the library does not include a high number of 0-B stars, the predicted indices at the hot end of the star sample are rather reliable.
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