Two equal masses orbiting their centre of mass at radius have separation . Newton's law of universal gravitation gives the displayed orbital frequency. Their mass quadrupole moment varies at twice that frequency, producing gravitational radiation with two gravitational wave polarizations. For inclination , its leading plus and cross amplitudes are proportional to and , respectively. Face-on radiation is circularly polarized; edge-on radiation is linearly polarized.
For a plane gravitational wave in linearized gravity with , Lorenz gauge in linearized gravity gives . Under , choose for , , and . This residual gauge symmetry of linearized gravity removes all time and longitudinal entries and the transverse trace. The remaining amplitudes are the two gravitational wave polarizations. The formula uses the plus-sign convention for ; reversing the definition of reverses the gauge change.
For a null tetrad , one common curvature-sign convention defines . In an outgoing wave zone it encodes the two transverse gravitational wave polarizations as one complex scalar.
Use , background Minkowski spacetime metric tensor , and with small metric perturbation. All indices and derivatives in this linear approximation use . The linearized inverse metric is , and the linearized Levi-Civita connection is
Define the trace-reversed metric perturbation , with .
An infinitesimal coordinate change gives the linearized coordinate gauge transformation
The metric perturbation therefore has redundant components. The gauge invariance of the linearized Riemann tensor follows because its change contains third derivatives of cancelling by commutation of partial derivatives. Conversely, flat linearized metric perturbations are locally pure gauge on a contractible patch. Thus linearized curvature, rather than a particular coordinate value of , detects the physical disturbance. Gauge freedom can also be restricted by global topology or boundary conditions.
Keeping the paper's curvature sign convention, its linearized Ricci tensor and scalar are
These are the negatives of the alternative frequently used curvature convention. Put . The Linearized Einstein equations in vacuum are
Under a gauge change , so solving imposes the Lorenz gauge in linearized gravity. The field equations then become . The remaining residual gauge symmetry of linearized gravity has ; Lorenz gauge does not exhaust the coordinate freedom.
A Fourier mode obeys and . Hence the plane gravitational waves in linearized gravity propagate on the background light cones. Four transversality conditions and four residual gauge amplitudes leave physical degrees of freedom. The explicit plane-wave reduction to transverse-traceless gauge can set , spatial trace zero and . For a wave in the direction, write its physical spatial strain as , so the spatial metric tensor is :
There are two gravitational wave polarizations, plus polarization and cross polarization. Rotating transverse axes through rotates their amplitude pair through . Nonconstant profiles with nonzero second derivative have nonzero linearized Riemann curvature tensor and cannot be removed as pure gauge.
The TT coordinate separation and measured separation distinction explains a detector's response. Freely falling particles initially at rest can keep fixed TT coordinates, since , while their proper separation changes. For a short arm along a unit vector ,
This is the tidal response described by geodesic deviation; coordinate motion by itself is not the measured signal.
Finally, gravitational-wave energy is second order in the perturbation, so it is absent from a first-order vacuum equation. In a short-wavelength averaging regime the averaged stress-energy of transverse gravitational waves is
For a plane wave its energy flux is . The averaging scale and weak-field assumptions matter: this does not assign a coordinate-independent local gravitational energy density to an arbitrary first-order perturbation.
Work to first order in a metric perturbation , with , raising perturbation indices with and discarding quadratic terms. The Christoffel symbols are
Using the printed curvature convention gives the linearized Riemann curvature operator
For definiteness contract . The corresponding first-order Ricci tensor is
This is the reversed sign convention specified in curvature-sign convention in Killing derivative identities; the vacuum equation is unaffected by an overall curvature sign.
An infinitesimal passive coordinate change changes the perturbation by . Substitution into gives zero change, since partial derivatives commute. Equivalently the change in curvature is the Lie derivative of the background curvature, which vanishes in Minkowski spacetime. Thus linearized curvature, and the linearized Weyl tensor in vacuum, are gauge-invariant tidal observables, whereas individual components of are generally gauge dependent.
The trace-reversed metric perturbation transforms by . Its divergence changes by . Solving therefore imposes Lorenz gauge in linearized gravity, . With the stated sign convention the Einstein tensor is
so the linearized vacuum field equation becomes . The residual gauge symmetry of linearized gravity has . This makes a hyperbolic evolution problem after the gauge condition and its initial consistency constraints have been imposed.
To separate actual gauge invariants from a gauge choice, use gauge-invariant Minkowski perturbations. For spatial indices contracted with , decompose
where , and . Spatial falloff or Fourier-mode conventions fix the decomposition. Write and with . Direct substitution in the gauge change gives
Hence the invariant combinations are
A representative with has , and . The explicit vacuum constraints for gauge-invariant Minkowski perturbations follow from
For a nonzero spatial Fourier mode, or regular decaying fields on all space, forces , then forces , and the spatial trace gives , hence . Only remains. This removal of the scalar and vector sectors does not exclude singular Coulomb perturbations outside a source, boundary-driven harmonic potentials or spatially homogeneous modes; those require separate boundary and gauge conventions.
For a propagating plane mode , the wave equation gives . A transverse-traceless spatial tensor perpendicular to a fixed propagation direction has two independent components. For propagation along , define the physical strain in this mostly-minus convention, so the spatial line element is . It has the form
These are the two gravitational wave polarizations, plus polarization and cross polarization. A rotation in the transverse plane rotates the polarization pair through twice the angle; cross is plus rotated through degrees. Lorenz constraints and residual gauge freedom give the same count: ten symmetric metric components minus four constraints and four gauge freedoms leave two radiative degrees of freedom.
In transverse-traceless gauge, particles initially at rest keep fixed spatial coordinates since , but their measured separation changes. For a short separation of length in unit direction , . The gauge-invariant curvature gives the corresponding geodesic deviation:
Here the last equation is in a freely falling orthonormal frame, with the printed reversed curvature convention. Coordinate separation and physical separation must not be confused. The linearized vacuum equations describe propagation and tidal measurements; wave energy transfer and an effective wave stress-energy tensor arise at quadratic order, beyond the linear approximation.
Let , using spatial indices . Stress-energy conservation, symmetry of the stress-energy tensor and integration by parts give
and a second derivative gives
All boundary terms vanish by compact support. This proves the stress-energy quadrupole identity,
The support is understood to remain bounded over the time interval used for differentiating these integrals.
For the radiation calculation set , write and use the trace-reversed metric perturbation in Lorenz gauge in linearized gravity. With the curvature and field-equation signs in this paper, the linear equation is
The retarded solution with no incoming radiation is consequently
Let be the distance from the source's centre of mass, and let be its size. In the radiation zone, . The leading multipole expansion additionally assumes slow internal motion, or small compared with the radiation wavelength. These assumptions allow in the denominator and the common retarded time at leading quadrupole order. Thus
Define the trace-free mass quadrupole moment by
To make the requested normalization explicit, write the trace-free spatial metric coefficient as . Trace reversal only adds a spatial trace, so the preceding equations give the far-zone quadrupole strain coefficient
The supplied scan does not contain the referenced perturbation handout. The definition above fixes the normalization of directly. If denotes the physical transverse-traceless tensor in that handout, the right-hand side is also to be transversely projected for the observation direction. Trace-free alone does not imply transverse. With , put
The transverse-traceless projector gives and the physical spatial strain is . This also states the result without relying on omitted handout notation. The retarded construction and direction-dependent transverse projection are described in Carroll's general relativity lectures, with the appropriate changes of metric-sign convention.
For the equal-mass binary star, its centre of mass is at the origin and the separation is . The gravitational force on either star is , while its centripetal force is . Hence
At leading Newtonian order, is the sum of the two point-mass densities. Its moments are
so the trace-free mass quadrupole moment is
The Newtonian bound system is treated in the usual leading weak-field quadrupole approximation; an exactly conserved effective source also includes the interaction stresses. Accelerated point-mass dust alone would not satisfy the conservation hypothesis.
Differentiating twice and evaluating at gives
For an observer on the axis this is already transverse and traceless. Its alternating plus polarization and cross polarization have a phase difference of , giving circularly polarized gravitational radiation at twice the orbital frequency. The amplitude decays as , as expected for outgoing radiation in three spatial dimensions.
More generally take the line of sight in the plane at inclination to the orbital angular-momentum axis. In the transverse basis , , define . Projection gives the physical gravitational wave polarizations
Thus a generic view is elliptically polarized, the face-on view is circularly polarized and the edge-on view is linearly polarized. This is circular-binary quadrupole radiation; an overall sign or transverse-axis rotation only changes the polarization convention.
A linearized coordinate gauge transformation changes the identification of points of the perturbed spacetime with its Minkowski spacetime background. With , the same physical metric has perturbation
These changes are coordinate freedom, not extra physical gravitational wave polarizations. Raising indices with , define and the trace-reversed metric perturbation . Then
The first-order Levi-Civita connection is . Contracting the Riemann curvature tensor in the stated convention gives
Put . The corresponding Einstein tensor is
Under the linearized coordinate gauge transformation, . Choosing a solution of imposes Lorenz gauge in linearized gravity, . Thus the vacuum Einstein field equations reduce to
There remains residual gauge symmetry of linearized gravity with .
For the transverse profiles, write both symmetric off-diagonal entries as and the diagonal entries as . The trace-reversed metric perturbation has zero trace and therefore equals . Its divergence vanishes: its only nonzero index directions are , while its coefficients depend only on . Also for every twice differentiable profile . These are consequently plane gravitational waves in linearized gravity in transverse-traceless gauge, with the two independent gravitational wave polarizations and .
To calculate the detector response, use a parallel-propagated orthonormal frame along the centre of a short nonrotating stick. To first order its clock reads , and the tidal curvature is
For a sliding-bead gravitational wave detector, the stick constrains transverse motion but supplies no axial restoring force. Projecting geodesic deviation along an -directed stick gives
Here is the proper separation and , with . Integrating with those actual initial conditions yields
For beads at rest before an incident wave, both initial profile terms vanish and the familiar result is . The cross polarization produces a transverse tidal force, balanced by the guide, and no axial first-order displacement in this orientation. In transverse-traceless gauge the same plus response can be read from the proper line element, ; coordinate distances alone are not measured distances. When a cross polarization is present, keeping the guide physically nonrotating may require transverse coordinate adjustments, which do not change the axial answer at this order.
For a -directed stick, and the wave is transverse. Therefore beads initially at rest retain their proper separation to first order: . The tidal calculation is the usual linear detector limit, with bead spacing small compared with the wavelength; it does not treat a macroscopic rigid body as exactly rigid over arbitrary relativistic distances.
For a nonzero, nonconstant vacuum plane gravitational wave in linearized gravity with real wave covector , the Linearized Einstein equations and Lorenz gauge in linearized gravity require
The zero-amplitude solution places no restriction on ; a constant mode is not a propagating wave. Under the sign convention for the infinitesimal change specified here, the trace-reversed metric perturbation changes by
Thus the residual gauge symmetry of linearized gravity is characterized by . The proposed plane-wave form obeys this for every constant complex , because is null. Changing the sign used to name would reverse both gauge formulas, with no physical consequence.
Rotate the spatial axes so the wave propagates along , choosing with . The Lorenz gauge in linearized gravity says ; in particular , and for . The amplitude change is
Choose
Indeed, and cancel the time components, while cancels the transverse trace. The preserved Lorenz gauge in linearized gravity then cancels all longitudinal components. This is an explicit plane-wave reduction to transverse-traceless gauge, yielding
The trace-reversed metric perturbation has zero trace in this transverse-traceless gauge, so . The null dispersion relation is , giving the speed of light. Only components perpendicular to the direction of propagation remain, and the two independent amplitudes give the plus and cross gravitational wave polarizations.
These are physical transverse tidal distortions, rather than just a convenient display of the metric perturbation: in transverse-traceless gauge, , so a freely falling detector has at first order. There is no longitudinal tidal acceleration. The plus polarization stretches one transverse axis while compressing the other; the cross polarization does the same along axes rotated by .
The phase is
Because the transverse-traceless gauge perturbation has no component along
only the third term of the linearized Riemann curvature operator contributes to the required contraction:
The derivatives and transverse polarization contraction are
Therefore the Newman--Penrose scalar Psi4 is
Its real and imaginary parts encode the plus and cross gravitational wave polarizations, up to the stated Riemann curvature tensor and complex null tetrad conventions.
A spatial rotation and rescaling put the future null vector in the form , so the profile depends on . Transversality gives four linear relations among the ten symmetric components. The four residual gauge functions satisfying remove the time and longitudinal components; the remaining trace can be removed by the residual transformation indicated in the question. The resulting transverse-traceless gauge is
The two arbitrary functions are the plus and cross gravitational-wave polarizations. They are the two physical degrees of freedom left after the four gauge conditions and four residual coordinate freedoms are removed.
On the positive axis, and . Taking this limit in the spatial components gives
with evaluated at retarded time . A wave propagating toward the observer along the direction has polarization matrix
Consequently the observed gravitational wave polarization amplitudes are
The mode and the orthogonal combination of do not contribute on this symmetry axis. The observer therefore sees a purely plus-polarized wave; a rotation of the transverse axes would represent the same physical polarization as the corresponding spin-two mixture of plus and cross.
With the reversed convention in curvature-sign convention in Killing derivative identities, choose the representative , , . The linearized Einstein components are , and . On all space with regular decaying fields, or for nonzero spatial Fourier modes, the vacuum constraints remove the scalar and vector parts, leaving two radiative gravitational wave polarizations. Singular Coulomb fields, spatial boundaries and homogeneous modes are not covered by that removal argument.