Radial Teukolsky Equation and Physical Solutions
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The separated radial Teukolsky equation becomes a physical problem only after its basis solutions, asymptotic phases, and flux normalization are declared. “Ingoing” and “upgoing” name global solutions by what is absent at a past boundary, not merely by the sign of a local exponential. This page fixes those meanings for , derives the constant weighted Wronskian, and distinguishes retarded scattering data from quasinormal and bound-state conditions.
Required background. Frames, Coframes, and Anholonomy supplies the tetrad weights needed to interpret horizon asymptotics.
Helpful background. Black-Hole Geometry and Mechanics supplies Kerr horizon generators; PDEs and Green Functions for Gravitation supplies Green functions, Wronskians, and boundary-value problems; Formulations of General Relativity supplies characteristic fluxes and constraints.
Radial operator and characteristic frequencies
Section titled “Radial operator and characteristic frequencies”In the subextremal Kerr exterior define
and use the radial equation
where and . The field convention and projected source normalization are those fixed in the derivation page; rescaling rescales every amplitude below.
Choose a tortoise coordinate by
Then at the future event horizon and at spatial infinity. The horizon generator is , with , so the horizon-frame frequency is
The factor is ingoing at the future horizon when combined with and a horizon-regular angular coordinate. Powers of additionally depend on and on whether the Kinnersley or a regular tetrad component is used. Teukolsky gives these Frobenius behaviors and their physical interpretation at both boundaries Teukolsky 1973, § V, Eqs. (5.1)–(5.8), (5.10)–(5.11), printed pp. 642–643.
In and up bases
Section titled “In and up bases”The radial powers can be derived rather than memorized. Put , and . Near the horizon, and . Inserting in the homogeneous equation gives, with ,
The roots give and . At infinity, insert , where . The first uncancelled coefficient, after division by , is . Thus the incoming power is and the outgoing power is .
For real nonzero away from thresholds, fix an “in” solution by
and an “up” solution by
For , these reduce to the familiar transmitted factor and outgoing factor. Sasaki and Tagoshi give exactly this gravitational normalization and use it to construct the retarded sourced solution Sasaki–Tagoshi 2003, § 2.1, Eqs. (14)–(20), printed p. 9. Different rescaled variables have different powers; phases and fluxes, after reconstruction, are the invariant comparison.
The names describe causal scattering bases. has no wave emerging from the past horizon; has no wave incident from past null infinity. Teukolsky and Press emphasize that opposite-spin representations can be mathematically better conditioned in different asymptotic regions Teukolsky–Press 1974, §§II–IV, pp. 444–453.
Wronskian and Green function
Section titled “Wronskian and Green function”Call the zeroth-order bracket in the raw radial equation . Multiplying the homogeneous equation by puts its derivative part in Sturm–Liouville form:
For any two solutions of the same equation,
is independent of . Differentiate it, substitute both equations, and the potential terms cancel. This weighted Wronskian is the normalization invariant needed for variation of parameters; the unweighted expression is generally not constant.
Let and, for definiteness, take to have compact radial support strictly inside the exterior. Distributions with that support are allowed. The ingoing/outgoing radial solution is
The factors of follow from the exact source normalization; importing a formula for without translating the equation changes the amplitude. Outside the source the solution is outgoing at infinity and ingoing at the horizon. Noncompact sources require separate convergence and boundary hypotheses. The retarded time-domain field is obtained by causal Fourier–Laplace inversion, continuing the resolvent from the upper half-plane (the prescription where its boundary value exists); a bare real-frequency formula does not select that contour.
Flux normalization and Starobinsky identities
Section titled “Flux normalization and Starobinsky identities”A raw Teukolsky amplitude is not itself energy flux. We now make the conversion explicit for a vacuum gravitational in-scattering mode with real , , and regular angular eigenfunctions. The rates are quadratic, cycle-averaged Killing-energy fluxes; an eternal monochromatic wave does not have finite total radiated energy. Keep the chapter’s angular normalization:
There is no in this separation. Hence the squared norm of on the full sphere is . The complex curvature field encodes two real strains; do not take its real part as though it were one real scalar and insert an extra factor into the following rates.
Opposite-spin amplitudes
Section titled “Opposite-spin amplitudes”Write , and for the coefficients. For the companion physical , let , and multiply the respective branches , and . Put and
Choose the relative angular phases used by Teukolsky and Press. The Starobinsky constant is then specified by
The angular adjoint identity makes the radicand nonnegative for the regular real-frequency eigenfunction; makes nonzero in this sector. Notice the in the last term: the original printed Eq. (3.23) omits the mass square. The dimensionally consistent expression is printed in Sasaki–Tagoshi 2003, § 5.6, Eq. (176), p. 41, PDF.
Define . For the physical-field radial functions, the complete fourth-order identities are
These identities relate the same physical perturbation, not independently normalized arbitrary solutions. Teukolsky and Press’s intermediate negative-spin radial function is multiplied by when forming their physical field; that factor has already been absorbed into our Teukolsky–Press 1974, § III, Eqs. (3.22), (3.28)–(3.30), pp. 447–448, PDF. Applying the identities to the endpoint expansions gives
For example, acting on the incoming infinity phase has leading factor ; its fourth power and the outer factor four give . Near the horizon the four factors acting on are for . Their product gives the last line. The outgoing relation follows most directly from the second fourth-order identity Teukolsky–Press 1974, Eqs. (4.10)–(4.11), (4.42), pp. 449, 451, PDF.
Physical rates and superradiance
Section titled “Physical rates and superradiance”At infinity use retarded time . In the Kinnersley frame the outgoing curvature obeys . Integrating over the sphere therefore gives the reflected rate below. The incoming Kinnersley curvature has the corresponding coefficient two, rather than one half. At the horizon one instead uses the regular-tetrad shear and the area balance. The symmetric null frame in Metric Reconstruction and Radiative Observables instead gives an outgoing coefficient one. Its boost to the asymptotic Kinnersley frame multiplies the outgoing null leg by and the ingoing leg by , halving ; physical strain and power do not change. With the endpoint conversions already applied, the rates are
Infinity reflection is positive outward; horizon transmission is positive inward. The horizon expression includes the boost from the Kinnersley to the regular Hawking–Hartle tetrad and the shear response; it is not a raw Weyl amplitude squared Teukolsky–Press 1974, Eqs. (4.12)–(4.16), (4.38)–(4.44), pp. 449–451, PDF. If instead one uses the unit-sphere harmonic , the radial coefficients become . The familiar expression is then the same reflected rate, not a competing normalization.
The horizon rate has the sign of for . Moreover,
Thus permits negative Killing-energy flux into the hole while the generator flux stays nonnegative. This is not a negative local energy measured by every horizon-crossing observer.
The conserved relation proving balance
Section titled “The conserved relation proving balance”The unconjugated same-spin Wronskian used for the Green function is not itself an energy current. To obtain the physical balance, set
Direct substitution gives , where
For real frequency and , these potentials satisfy . Consequently
is constant: differentiation cancels the two identical potentials. Its endpoint values, in the physical amplitude convention above, are
Substitute the three Starobinsky amplitude relations and multiply the equality by . Every coefficient is then a physical flux coefficient:
This is the radial proof of gravitational scattering balance Teukolsky–Press 1974, § V, Eqs. (5.2)–(5.8), p. 452, PDF. For , define energy reflection and transmission fractions:
Superradiance means and when transmission is nonzero. The unequal dimensions of the raw coefficients provide a quick warning against identifying amplitude ratios with energy fractions: since has dimension , the dimensions of are respectively .
Other physical domains
Section titled “Other physical domains”Boundary conditions define different problems on the same ODE:
- A retarded sourced solution is future-horizon ingoing and future-null-infinity outgoing, with the frequency contour fixed by causal continuation.
- A quasinormal mode satisfies the same homogeneous boundary directions but only at discrete complex where on the stated analytic sheet.
- A scattering solution at real retains an incident component at one past boundary and measures reflected and transmitted flux.
- A massive bound or quasibound state would require a different field equation and an exponentially decaying infinity condition; the massless Teukolsky equation written here does not acquire that condition by relabeling its solutions.
Thresholds and , extremality , and complex frequency change the Frobenius structure and must be treated separately. The formulas above assume subextremality and ordinary nonzero characteristic frequencies.
Exercises
Section titled “Exercises”For and real , suppose at infinity and at the horizon. Derive the constant-current relation and decide when reflected flux exceeds incident flux. Repeat the normalization using .
Solution
For the potential is real at real , so the conserved current is
Since , the infinity falloff cancels the leading factor there. The incident/reflected cross terms cancel in the current, giving
where outward radial orientation is positive. At the horizon,
Constancy gives
The horizon area factor is not a common factor that can be cancelled at both ends. For , direct differentiation instead gives exactly. Its horizon amplitude is , so the same result is . If and transmission is nonzero, then . For the complex same-spin potential precludes this scalar-current argument; the opposite-spin conversion above is essential.
Set in the gravitational flux conversion. Show that the Starobinsky constant has the expected spherical polynomial and explain why the raw reflection amplitude still is not an energy fraction.
Solution
Now and , so
It is nonzero for . The ratio has dimension ; the factor is still needed to form . Since , and , giving as expected for Schwarzschild scattering.
References
Section titled “References”- Sasaki, Misao, and Hideyuki Tagoshi. “Analytic Black Hole Perturbation Approach to Gravitational Radiation.” Living Reviews in Relativity 6 (2003): article 6. DOI. Open PDF.
- Teukolsky, Saul A. “Perturbations of a Rotating Black Hole. I. Fundamental Equations for Gravitational, Electromagnetic, and Neutrino-Field Perturbations.” Astrophysical Journal 185 (1973): 635–647. DOI.
- Teukolsky, Saul A., and William H. Press. “Perturbations of a Rotating Black Hole. III. Interaction of the Hole with Gravitational and Electromagnetic Radiation.” Astrophysical Journal 193 (1974): 443–461. ADS record and PDF.