The synthetic grids of VJHK colours used in this paper are based on
the ATLAS9 Kurucz
models computed by Castelli with the overshooting option for the
convection switched off (NOVER grids, Castelli et al. 1997).
When (V-K) colours in the Johnson (J) system are considered,
the NOVER RIJKL grids available at http://kurucz.harvard.edu were used,
while when (V-J), (V-H), and (V-K) colours in the Bessell-Brett (BB) homogenized
system
are considered, the BCP NOVER grid of colours were
used. We recall that for (V-K), the conversion from the J system to the
BB system is (Bessell & Brett 1988):
![]() |
(1) |
![]() |
(2) |
Table 3 gives
for
,
,
and
in the interval 6500 to 10 500 K for metallicities
,
-1.0, -1.5 and -2.0. This table is in two parts; the first for
= 4.0
and the second for
= 4.5.
In both Tables 2 and 3 the step in
is 10 K.
Figures 1 and 2 show the effect of gravity and the
effect of the metallicity respectively on the relations
vs.
,
vs.
,
and
vs.
.
Table 1 shows the effect of gravity on the
vs.
relation
indicating that it is at a maximum at 8000 K with
= 123 K
for
= 1.0.
Figure 1 shows that this effect is of the same order as for the
vs.
and
vs.
relations. The effect of errors in the metallicity on
the
vs. colour relations are not larger than those caused by gravity.
Table 1 shows that, for (V-K), the largest difference in
produced by
a [M/H] change of 1.0
is about 100 K. Figure 2 shows that this behaviour is similar for all the
three colour indices.
Houdashelt et al. (2000) have used updated MARC-SSG models to obtain
colours on the Johnson-Glass system for
stars with 4000 K
6500 K.
Their hottest model (6500 K) is somewhat
cooler than the temperatures with which we are concerned in this paper.
Nevertheless, it may be interesting to note that at this temperature, for
= 4.0,
,
their relation gives a V-K = 1.047 compared with
1.079 for the BCP colors. Thus, at 6500 K, their model gives a
which is
56 K cooler than that given by BCP.
Such systematic differences do not seem
unreasonable considering the use of different atmospheric models and the
different calibrations for the colours.
Copyright ESO 2002