Let be the positive Euclidean spatial background metric. Write a tensor-sector metric perturbation as , , with and . Spatial indices here are raised with , and .
Substitute the linearized Levi-Civita connection into the cover's curvature definition. To first order,
In the transverse-traceless tensor sector and , so and
The tensor part of the Linearized Einstein equations therefore gives
In a calculation strictly confined to the tensor sector, the source on this equation means its tensor projection; it is already trace-free there.
For a generic compact source, trace-free is not the same as transverse-traceless. For example, the static compactly supported spatial stress , with smooth compactly supported , is divergence-free, but its trace-free part has divergence , generally nonzero. There is a precise way to reproduce the unprojected trace-free formula used in the question while retaining this distinction. In Lorenz gauge in linearized gravity, the trace-reversed metric perturbation obeys
Define its spatial trace-free half-strain by
Then its wave equation has exactly the displayed trace-free source . The physical tensor radiation is obtained afterwards with the transverse-traceless projector. Without that projection, this is a Lorenz-gauge trace-free coefficient, not necessarily a transverse tensor mode. At leading far-zone order, the same directional projector is applied to both sides of the quadrupole field formula below.
The flat contracted Bianchi identity implies stress-energy conservation, . Let
Compact support removes boundary terms. Differentiate and integrate by parts once:
A second time derivative, another integration by parts and symmetry of the stress-energy tensor give
Take the spatial trace-free part. The mass quadrupole moment satisfies the stress-energy quadrupole identity
Inserting this into the assumed leading retarded quadrupole field gives
This is the requested spatial half-strain convention; the measured transverse-traceless strain is . The formula selects the retarded source field and does not include an independently added homogeneous gravitational wave. Dropping the source-dependent part of retardation also needs the long-wavelength source approximation, besides .
For a slowly moving weakly self-gravitating source, the virial theorem or the dynamical balance gives . A varying nonspherical mass quadrupole moment has characteristic size and dynamical time , so . Consequently the quadrupole strain scaling of a weak self-gravitating source is
This is a characteristic scale, not a nonzero lower bound: a stationary or exactly spherical source does not radiate. Slow motion gives , justifying the long-wavelength approximation; for a radiation-zone strain one also takes .
Use , select the retarded source field with no added homogeneous radiation, and work to leading order in the weak-field approximation and long-wavelength source approximation. The retarded fundamental solution of the Linearized Einstein equations in Lorenz gauge in linearized gravity is
For , the denominator is to leading order. The delay is , where . In the usual slowly evolving source regime, its characteristic time obeys , so the source-size part of the delay is negligible:
The stress-energy conservation equation is required at the approximation order used; it follows from the divergence of the gauge-fixed field equation. Compact support removes the integration by parts surface terms. Since and in this signature,
Combining these identities gives the retarded quadrupole field
For an ordinary nonrelativistic bound source, makes . More generally the size relative to the variation timescale must also be small; speed alone does not exclude a rapidly varying small-amplitude motion.
The radiation boundary condition for linearized gravity is essential for a statement about the full field. Without it, the displayed implication is false: take and add , , all other components zero. This weak plane gravitational wave satisfies both the homogeneous wave equation and Lorenz gauge in linearized gravity, while every is zero. The proved formula is for the retarded source contribution, with the standard slow-source qualification. Its transverse–traceless projection gives the physical radiative strain.