For linear hyperbolic equations with time independent coefficients, we know that solutions
determined by data with compact support are bounded by
, where
is independent of the
data. It is not known whether all such solutions are bounded in time, i.e. whether they are
stable.
Assuming harmonic time behavior
, a separation in angular and radial variables was
found by Teukolsky [196]:
For each complex
and positive integer
, Equation (39
) together with the boundary
conditions of regularity at the axis, determines a singular Sturm–Liouville eigenvalue problem. It has
solutions for eigenvalues
,
. The eigenfunctions are the spheroidal (oblate)
harmonics
. They exist for all complex
. For real
the spheroidal harmonics are complete
in the sense that any function of
, absolutely integrable over the interval
, can be
expanded into spheroidal harmonics of fixed
[181]. Furthermore, functions
absolutely
integrable over the sphere can be expanded into
Let us pick one such solution
and consider some solutions
of (40
) with the
corresponding
. Then
is a solution of (37
). Is it possible to obtain
“all” solutions by summing over
and integrating over
? For a solution in spacetime for
which a Fourier transform in time exists at any space point (square integrable in time), we
can expand the Fourier transform in spheroidal harmonics because
is real. The coefficient
will solve Equation (40
). Unfortunately, we only know that a solution determined
by data of compact support is exponentially bounded. Hence we can only perform a Laplace
transformation.
We proceed therefore as in Section 2. Let
be the Laplace transform of a solution
determined by data
and
, while
is analytic in
for real
, and has an analytic continuation onto the half-plane
. For real
we can expand
into a converging sum of spheroidal harmonics [148]
To define quasi-normal modes we first have to define the correct Green function of (40
) which
determines
from the data
. As usual, this is done by prescribing decay for real
for two
linearly independent solutions
and analytic continuation. Out of the Green function for
and
for real
we can build the Green function
by a
series representation like (42
). Analytic continuation defines
on the half plane
. For
non exceptional
we have a series representation. (We must define
by this complicated
procedure because the partial differential operator corresponding to (39
), (40
) is not elliptic in the
ergosphere.)
Normal and quasi-normal modes appear as poles of the analytic continuation of
. Normal modes are
determined by poles with
and quasi-normal modes by
. Suppose all such values are
different from the exceptional values. Then we have always the series expansion of the Green
function near the poles and we see that they appear as poles of the radial Green function of
.
To relate the modes to the asymptotic behavior in time we study the inverse Laplace transform and deform the integration path to include the contributions of the poles. The decay in time is dominated either by the normal mode with the largest (real) eigenfrequency or the quasi-normal mode with the largest negative real part.
It is apparent that the calculation of the QNM frequencies of the Kerr black hole is more involved than
the Schwarzschild and Reissner–Nordström cases. This is the reason that there have only been a few
attempts [135
, 185
, 123
, 160] in this direction.
The quasi-normal mode frequencies of the Kerr–Newman black hole have not yet been calculated,
although they are more general than all other types of perturbation. The reason is the complexity of the
perturbation equations and, in particular, their non-separability. This can be understood through the
following analysis of the perturbation procedure. The equations governing a perturbing massless field of spin
can be written as a set of
wavelike equations in which the various different helicity
components of the perturbing field are coupled not only with each other but also with the
curvature of the background space, all with four independent variables as coordinates over
the manifold. The standard problem is to decouple the
equations or at least some
physically important subset of them and then to separate the decoupled equations so as to
obtain ordinary differential equations which can be handled by one of the previously stated
methods. For a discussion and estimation of the QNM frequencies in a restrictive case refer
to [124
].
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