368 Chapter 10 Collapse of collisionless clusters in axisymmetry
fairly small separations, the energies and waveforms agreed well with the results of full
2 + 1 numerical simulations, like the ones discussed in the previous section.
33
The remarkable success of the “close limit” approach can be explained, at least in part,
by the presence of the black hole horizon and its use as an inner boundary at which all
matter and radiation are purely ingoing. Once the horizon forms and the spacetime settles
down to a perturbed Schwarzschild black hole, data obtained by further evolution with a
2 + 1 numerical routine are no longer required to obtain the final gravitational waveform.
The 2 + 1 simulation can be terminated at a relatively early epoch; instead of continuing
the simulation in order to propagate the exterior radiation pulse out to the weak-field
extraction regime, a simpler set of black hole perturbation equations can be solved for the
waveform, using the fields on the last numerical time slice for initial data. However, this
“close limit” approach does require the formation of a black hole during the numerical
simulation: its horizon is essential for preventing all further evolution inside the black hole
from influencing the spacetime outside. The same approach does not work for, say, an
oscillating neutron star, where there is no horizon.
In the perturbation approach we treat the spacetime metric as a static Schwarzschild black
hole plus a perturbation (see Chapter 9.4.1). Since for our applications all perturbations
have even (i.e., polar) parity, we can restrict the analysis to the even-parity modes and
identify, from the perturbations, the gauge-invariant Moncrief functions R
lm
,aswellas
their time derivatives, on a spatial slice (see equation 9.87). In axisymmetry, the only
nonvanishing modes are those with m = 0, R
l0
. These functions now provide initial data
for the Zerilli equation (9.90)
∂
2
t
R
l0
− ∂
2
r
∗
R
l0
+ V
(e)
l
R
l0
= 0, (10.16)
where r
∗
= r
s
+ 2M ln(r
s
/M − 1) is the tortoise coordinate, r
s
= r(1 + M/2r)
2
is the
Schwarzschild radius corresponding to (isotropic) radius r , and the Zerilli potential V
(e)
l
is
given by equation (9.91). Given that this equation depends on only one spatial coordinate,
it can be integrated on a fine mesh from a small radius very close to the event horizon,
say r
∗
/M =−500, to a very large radius, say r
∗
/M = 1000, until the perturbation has
propagated out to a large distance, well beyond the peak of the potential just outside the
horizon. At large radius, the even-parity gravitational wave amplitude h
+
can be computed
from the R
l0
as in equation (9.109). This perturbation waveform can be compared with
the waveform calculated by standard spacelike extraction of the 2 + 1 radiation data at
large distance.
34
In contrast to the perturbation result, the amplitude found from standard
extraction is cut short once the 2 + 1 integrations break down due to, e.g., grid stretching.
We can now mention another advantage of the perturbation method over wave extraction
at a finite radius. Integrating the Zerilli equation (10.16) to large radii automatically takes
into account the effects of gravitational wave backscatter off the black hole curvature.
33
See also Abrahams and Cook (1994), who extended this technique to initial data representing boosted black holes with
a common apparent horizon.
34
Chapter 9.2.2. The extraction algorithm of Abrahams and Evans (1990) was actually employed for the disk scenario
described here.