
C
The surface element on the
apparent horizon
In this appendix we outline a method for computing the surface element on a closed 2-surface
S embedded in some 3-dimensional spatial hypersurface . The approach is useful for diverse
numerical applications that require areas of closed 2-surfaces on spatial slices, but our prime
motivation here is to compute the proper area of an apparent horizon of a black hole or a system
of black holes. Recall that for stationary spacetimes, the apparent horizon coincides with the
event horizon and its area then determines the irreducible mass (7.2) of a black hole.
One approach to computing this surface element is to construct the induced metric m
ij
on the
surface S (see Chapter 7). Typically. however, the resulting line element will not be expressed
in terms of coordinates that are convenient for setting up the surface element. One way of
constructing such a coordinate system is the following:
1
We start with the line element for the
spatial hypersurface ,
dl
2
= γ
ij
dx
i
dx
j
, (C.1)
where the x
i
denote the spatial coordinates that have been used to label points on in the
numerical calculation. We can now transform to spherical polar coordinates, centered on some
fiducial point C
i
. The coordinate separation between nearby points as expressed in the two
coordinate systems will then be related by the usual transformation,
dx
i
=
∂x
i
∂r
C
dr
C
+
∂x
i
∂θ
dθ +
∂x
i
∂φ
dφ. (C.2)
Using the notation of Chapter 7, we define the closed 2-surface S around C
i
as the level surface
τ (x
i
) = r
C
(x
i
) − h(θ,φ) = 0, (C.3)
where r
C
is the coordinate separation between the point x
i
and the point C
i
. For example, in
Cartesian coordinates, we have r
2
C
= x
2
+ y
2
+ z
2
, provided the centers of the polar and Cartesian
coordinate systems coincide. The function h(θ,φ) then measures the coordinate distance from
C
i
to the 2-surface S in the (θ,φ) direction.
2
In the following we assume that we have already
determined h(θ,φ) by means, for example, of the techniques described in Chapter 7 in the case
where S is an apparent horizon.
On S, where r
C
= h(θ,φ), we must have
dr
C
=
∂h
∂θ
dθ +
∂h
∂φ
dφ. (C.4)
1
See Appendix D in Baumgarte et al. (1996).
2
By our notation h(θ,φ) we mean that h can be expressed in terms of the coordinates θ and φ via, for example, a
superposition of spherical harmonics (cf. Chapter 7.3.3). In Cartesian coordinates, it may be more convenient to express
h in terms of combinations of x , y and z via, for example, a superpositions of symmetric, tracefree “STF” tensors.
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