Linearized gravity writes with and discards terms quadratic in and its derivatives.
Expand the Einstein tensor about the Minkowski metric. The quadratic term in the metric perturbation defines , a symmetric tensor relative to the background. For a first-order vacuum solution, the expanded contracted Bianchi identity gives . Equivalently, a second-order correction obeys , whose flat divergence vanishes identically. This conservation is an on-shell statement. The local depends on perturbative gauge and the background split; conservation alone does not make it a gauge-independent local gravitational stress-energy tensor.
A massless Fierz-Pauli action is the quadratic flat-background action for a symmetric metric perturbation that yields the vacuum Linearized Einstein equations. One normalization, up to a total derivative, is
Varying the symmetric field with compact support gives the displayed linearized Einstein tensor coefficient. Its linearized coordinate-gauge symmetry is consistent with the contracted Bianchi identity. It is the massless gravitational action, distinct from imposing the massive Fierz-Pauli equations with five polarizations.
An infinitesimal coordinate change generated by changes a metric perturbation about Minkowski spacetime by , in the passive sign convention. For a passive coordinate change , the first-order change is minus the Lie derivative of a tensor field of the background metric, equivalently the pullback by the inverse flow. The gauge invariance of the linearized Riemann tensor follows because the added terms have commuting third derivatives, which cancel in the curvature antisymmetrizations. Gauge choices alter the metric components while preserving linearized tidal effects.
For a perturbation , with all other components zero, the linearized Vacuum Einstein equations give . Put and choose , , , . Under the linearized coordinate gauge transformation, the mixed time/transverse and longitudinal/transverse components cancel, while the other time/longitudinal changes are proportional to . The remaining components are , , , a transverse-traceless gauge perturbation of plus polarization. This explicitly removes a nonzero affine trace without assuming it vanishes by boundary conditions. If too, all linearized curvature vanishes.
The weak-field approximation requires every dimensionless component of the metric perturbation to have magnitude much smaller than one, so terms quadratic in the perturbation may be neglected.
The retarded source solution of the Linearized Einstein equations is selected by excluding added incoming or freely specified homogeneous gravitational waves. A homogeneous wave can satisfy Lorenz gauge in linearized gravity while having no source mass quadrupole moment. Thus a formula for the retarded source field is not an identity for every solution of the sourced wave equation.
For a compact slowly moving source in the weak-field approximation, with no incoming homogeneous wave and , the retarded Linearized Einstein equations give this leading far-zone trace-reversed metric perturbation. The key consequence of stress-energy conservation is . The physical gravitational wave is obtained by the transverse-traceless projector.
Dropping the position-dependent source delay in the leading far-zone retarded field requires source size to be small compared with its variation time , in units . The retarded quadrupole field also requires . For a typical nonrelativistic bound source, implies this long-wavelength condition; an arbitrarily rapidly oscillating small displacement is not controlled merely by its instantaneous speed.
If , then , with indices on raised using the background metric.
About a Cartesian flat background,
The linearized Riemann tensor defines an operator on two-forms by
Unlike the metric perturbation itself, this operator is invariant under linearized gauge transformations.
Under , every contribution to the linearized Riemann tensor contains three commuting derivatives of and cancels pairwise. Linearized curvature is therefore gauge invariant about flat spacetime.
In four dimensions, the trace-reversed perturbation is
Trace reversal simplifies the linearized Einstein equations.
The Lorenz condition reduces the vacuum field equation to . A plane-wave amplitude therefore satisfies and .
An infinitesimal coordinate change generated by changes
It preserves Lorenz gauge exactly when .
A vacuum mode has a null wavevector and a transverse symmetric amplitude. Residual gauge freedom can further reduce it to two physical transverse-traceless polarizations.
Transverse-traceless gauge sets the time and longitudinal components and the spatial trace of a vacuum gravitational-wave perturbation to zero.
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.
In transverse-traceless gauge, particles initially at rest have fixed spatial coordinates because . Their separation measured in a parallel-propagated orthonormal frame changes: to first order . Hence the physical geodesic deviation is , whereas the coordinate displacement obeys . The extra term in the coordinate expansion of the second covariant derivative reconciles the two results. This applies to infinitesimal separations and linear metric perturbations.
A gravitational wave in four-dimensional general relativity has two independent linear polarizations, conventionally called plus and cross. A rotation by angle in the transverse plane rotates their pair by .
A transverse-traceless spatial tensor is orthogonal to its Fourier mode wavevector in each index and has zero trace. The transverse-traceless projector extracts this part. Trace terms and symmetrized coordinate-displacement gradients have no such part, explaining the linear gauge invariance of tensor cosmological perturbations.
A gravitational wave of plus polarization has opposite transverse strain or geodesic deviation eigenvalues along two fixed perpendicular axes. For a sinusoidal periodic function profile, the stretching and compressing roles alternate every half-period.
The cross polarization is the plus pattern rotated through degrees in the transverse plane.
The transverse-traceless projector maps a symmetric tensor to the part orthogonal to a chosen wavevector and with zero trace. It is the identity on physical gravitational-wave polarizations.
A polarization completeness relation expresses a projector as a sum of outer products of an orthonormal polarization basis. For transverse-traceless tensors, is the transverse-traceless projector up to the chosen normalization.
To first order around flat spacetime,
and
For a weak, static field produced by nonrelativistic matter, is the dominant stress-energy component. The field equations and the slow-particle geodesic equation imply
where the Poisson equation is .
For smooth spatial and , the only nonzero Christoffel symbols are and . Consequently the Levi-Civita connection converges smoothly on compact sets as although the metric itself diverges in these coordinates. The limiting torsion-free connection has only and gives when is an affine parameter. With , its Ricci tensor is : quadratic connection terms vanish and . Thus zero Ricci tensor is the Laplace equation, while full flatness would require the entire Hessian to vanish.
For a point mass in a positive cosmological constant, the inward Newtonian acceleration balances the outward cosmological acceleration at the static radius .
For a point mass and , write
The vacuum scalar-curvature equation gives , so . The remaining vacuum equations fix in the corresponding Schwarzschild gauge.
Far from a slowly rotating isolated body of mass and angular momentum , the scalar part of the metric is the linearized point-mass field while is the dipole field of . For rotation about the z-axis, the cross term is in a common convention.

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Linearized gravity is an approximation of general relativity that simplifies the complex equations describing the gravitational field. It is based on the idea that the gravitational field can be treated as a small perturbation around a flat spacetime, typically Minkowski spacetime, which describes a region of spacetime without significant gravitational effects. In the framework of general relativity, the gravitational field is represented by the geometry of spacetime, which is described by the Einstein field equations.