8.3 Fluid stars: collapse 301
It is clear that very few modifications are needed to transform the Misner–Sharp equa-
tions to observer time coordinates. Hence a code using Misner–Sharp equations can be
rewritten in observer time coordinates simply by adding a few terms and using ψ instead
of φ. The advantage is that the revised code can handle black holes without breaking down.
There are two very attractive properties of observer time coordinates. One is that the
coordinate u immediately corresponds to the time at which a distant observer would see
a certain event, as for example a gamma-ray burst (GRB) in a supernovae explosion.
The other one is that the global structure of spacetime is conveniently “hard-wired” into
the integration scheme. This means that there is no need to search for apparent horizons
(actually, apparent horizons never appear in observer time coordinates because they are
always inside event horizons) or to track null rays in order to locate event horizons. In
this case the event horizon can be found simply by looking for events at the which the
lapse function e
ψ
becomes exceedingly small. The lapse function plummets for every fluid
element approaching the event horizon and essentially causes its further evolution to cease.
For a typical application involving collapse to a black hole, one can terminate the evolution
if and when e
ψ
drops below, say 10
−3
at the outermost shell. By then, the lapse in the
center can be considerably smaller and can reach machine underflow.
The only subtlety that arises in using observer time coordinates has to do with the
implementation of initial data. It is usually convenient to specify initial data on a spatial
t = constant hypersurface instead of a null hypersurface. Consequently, for typical appli-
cations, the implementation of initial data occurs in two stages. First, initial data are given
on a t = constant surface. These are then evolved using a Misner–Sharp scheme. During
this evolution, a null geodesic is sent out from the center of the configuration, and the
data on its path are stored. When the null ray arrives at the surface, this stage of the
evolution can be stopped and the data on the ray’s path can now be used as initial data on
a u = constant = 0 surface, at which point the Hernandez–Misner scheme takes over for
the rest of the evolution.
As an example of the Hernandez–Misner scheme at work, we show in Figure 8.21 “test-
bed” results for the collapse of a homogeneous, dust ball initially at rest, i.e., Oppenheimer–
Snyder (OS) collapse. As we noted earlier, OS collapse provides one of the few highly
nonlinear, dynamical examples in general relativity for which the solution is known ana-
lytically (see Chapter 1.4). However, as we noted in previous cases, before this analytic
solution can be compared with the numerical results, the solution must be transformed to
the coordinate system adopted in the numerical approach. This transformation has been
carried out
46
for null coordinates and the comparison with a numerical simulation in these
coordinates is shown in the figure.
A more interesting result is shown in Figure 8.22 for the collapse of a 1.4M
, n = 3
polytrope with adiabatic index γ = 4/3 and initial central density ρ
0c
= 10
12
gcm
−3
.
Plotted in the figure is a spacetime diagram for the late time evolution of a configuration in
46
Baumgarte et al. (1995).