The Lorenz Gauge in Linearized Gravity
The full Einstein field equations are ten coupled, nonlinear partial differential equations, and in general they cannot be solved without a computer or a symmetry. Yet the gravity of everyday experience — the Sun holding the planets, the tides, the faint ripple of a merging black-hole binary passing through a detector — is weak. The metric barely departs from flat: write with and keep only terms linear in , and the equations become linear. But "linear" is not yet "simple". The linearized Einstein tensor still bundles four different second-derivative structures that stir the components of together, so the ten equations refuse to separate. The Lorenz gauge is the single choice of coordinates that unstirs them. Its power comes from an exact structural parallel with electromagnetism. Linearized gravity inherits a gauge symmetry — an infinitesimal coordinate change shifts without touching the physical curvature — that is the two-index copy of . Just as one imposes to clean up Maxwell's equations, one imposes on the trace-reversed perturbation here. The reward is dramatic: the linearized Einstein equations collapse to , ten independent flat-space wave equations solved by the familiar retarded Green's function — gravity, like light, propagates at and carries radiation. And the construction is self-consistent for one deep reason, local conservation of energy-momentum , which is why the Lorenz gauge is the launch pad for the Newtonian limit, the post-Newtonian expansion, and the whole theory of gravitational waves.
- In linearized gravity the metric is with ; the natural field variable is the trace-reversed perturbation , which in four dimensions obeys .
- The Lorenz (harmonic) gauge condition kills every cross term in the linearized Einstein tensor, collapsing the field equations to .
- Each of the ten components then obeys an independent flat-space wave equation with source, solved by the retarded integral — the exact analogue of the electromagnetic retarded potential.
- The gauge is always reachable: solving has a retarded solution on flat spacetime, and a residual freedom with survives — the freedom later used for the transverse-traceless gauge.
- Consistency is not automatic; it holds because forces , the linearized shadow of the contracted Bianchi identity.
- In vacuum the equation becomes ; counting the ten components against four gauge conditions and four residual functions leaves exactly two physical polarizations.
- Key idea: trade the component-mixing linearized Einstein equations for ten independent flat-space wave equations by choosing coordinates so that .
Trade the nonlinear, component-mixing linearized Einstein equations for ten independent flat-space wave equations by choosing coordinates so that the divergence of the trace-reversed perturbation vanishes, .
Where this lives today
The Lorenz-gauge wave equation is not a historical curiosity — it is the working front end of gravitational-wave astronomy. Every waveform template that LIGO, Virgo, and KAGRA match against their data begins life as a solution of , expanded in the far zone into the quadrupole formula and pushed to high post-Newtonian order for the slow inspiral of two compact objects. The 2015 detection of GW150914 — black holes of about and solar masses merging billion light-years away, peak strain — was recognized because theorists had computed, decades in advance, exactly what such a signal should look like with this machinery. The residual gauge freedom is not academic either: fixing it to the transverse-traceless frame is what tells a detector that a passing wave stretches one arm while squeezing the perpendicular one. The same equation grounds the post-Newtonian expansion behind the orbital decay of binary pulsars — the Hulse–Taylor system matches the quadrupole prediction to better than a percent — and the relativistic corrections that keep GPS accurate, whose clocks live in exactly the regime of the worked example. Harmonic coordinates, the exact-theory cousin of the Lorenz gauge, are also the standard choice in numerical relativity for keeping the evolution equations well-posed as two black holes spiral together.
The physical picture
The cleanest way to see the Lorenz gauge is to hold electromagnetism in the other hand. There, the four-potential carries a gauge redundancy ; Maxwell's equations written for contain a troublesome term that mixes the components, and imposing deletes it, leaving . Linearized gravity is the same story told with one more index. The metric perturbation plays the role of , the gauge vector plays the role of , and the Lorenz condition is the tensor copy of . The payoff is identical in form and even in the constant out front: a decoupled wave equation with a conserved source.
Why trace-reverse first? Because the linearized Einstein tensor contains both and its trace , and the combination whose divergence appears in every unwanted cross term is not but . Setting the divergence of that bundle to zero deletes all four mixing terms at a stroke; imposing on the raw perturbation would not. The trace reversal is bookkeeping that lines the variables up with the geometry. The gauge is always attainable because reaching it means solving a wave equation , which on flat spacetime always has a retarded solution. The coordinate freedom is four functions' worth — the four components of — exactly the number of conditions in . That matched count is also why a residual freedom survives: gauge vectors with change nothing in the Lorenz condition, and in vacuum that leftover strips the ten components down to the two physical polarizations of a gravitational wave.
The core equations
Linearized gravity begins with one modeling choice — that spacetime is nearly flat — and every equation below unfolds from it. We write the metric as a flat background plus a small perturbation and drop everything beyond first order.
where: — flat Minkowski metric, signature ; — small symmetric perturbation, kept to first order. Reading: gravity lives as a weak field on a fixed flat stage, so indices are raised and lowered with , not . The field variable that tidies the equations is not itself but its trace-reversed cousin — literally so, since taking the trace flips the sign, as shown just below.
where: — trace-reversed perturbation; — the trace ; note . Reading: and carry the same information, but is the combination the Einstein tensor is naturally written in. Linearized gravity is a field defined only up to a gauge transformation, exactly as in electromagnetism. An infinitesimal coordinate change acts on the perturbation as follows and leaves all curvature invariants untouched.
where: — infinitesimal gauge vector; — its lowered form. Reading: two perturbations differing by describe the same spacetime in different coordinates. Translating that rule into the trace-reversed variable adds one extra trace term — the term that makes transform so conveniently under a divergence.
where: — four-divergence of the gauge vector. Reading: the extra is what, under a divergence, combines the derivatives of into a single d'Alembertian. The Lorenz gauge sets the divergence of to zero — four conditions, one per free index .
where: — the flat-space divergence. Reading: the tensor analogue of the electromagnetic , also called the harmonic or De Donder gauge. The payoff is visible in the linearized Einstein tensor: written in it is one clean d'Alembertian plus three terms, each carrying a divergence of .
where: — Einstein tensor to first order; — flat d'Alembertian. Reading: the last three terms are the mixing that keeps the ten equations coupled — and all three vanish in Lorenz gauge. Imposing the gauge and inserting leaves the centerpiece of the subject: ten decoupled, sourced wave equations.
where: — stress-energy tensor (source); — Newton's constant, . Reading: each component of is driven by the matching component of , with no coupling between components. Reaching the gauge from an arbitrary perturbation means solving one wave equation for the gauge vector — always possible on flat spacetime.
where: — the perturbation before the gauge change. Reading: whatever divergence you start with, this manufactures the coordinate shift that cancels it; a residual freedom then remains. Finally, the decoupled equation is solved by the retarded Green's function — the metric as an integral of the source over its past light cone, the gravitational retarded potential.
where: — retarded time (with ); the field at a point is built from the source configuration on its past light cone. Reading: gravity propagates causally at , exactly as the electromagnetic retarded potential does.
The goal is to prove the central claim of the article: that imposing the single condition turns the tangled linearized Einstein equations into ten independent flat-space wave equations . We start from the exact first-order Einstein tensor in the trace-reversed variable, note that every term but the d'Alembertian carries a divergence of , kill those with the gauge, and fix the constant by matching to .
Step 1. Begin with the linearized Einstein tensor, . Notice the structure: one term is the pure wave operator acting on , and the other three each contain a factor — the divergence of the trace-reversed perturbation on one index. Why: writing the Einstein tensor in rather than is what isolates the divergence as the common factor in every mixing term.
Step 2. Impose the Lorenz condition . Then , and likewise and . All three mixing terms vanish identically. Why: the gauge is engineered so that its one condition annihilates every term that couples different components — one deletion does the work of many.
Step 3. Only the d'Alembertian survives, so . The left side no longer mixes components: the operator acts on each separately. Why: this is the moment of decoupling — ten scalar wave equations in disguise, distinguished only by which component of and which component of the source they carry.
Step 4. Insert the field equations to get , hence . The factor of two out front is exactly the factor of two hidden in the trace reversal, and the sign is fixed by the signature . Why: the numerical constant is not decorative — it is what makes the static limit reproduce Newton's , checked in the worked example below. *The coefficient follows directly from with , and the sign is consistent with the signature.*
Go deeper · Derivation B · 1 minReaching the gauge and the residual freedom
The goal is to prove two things at once: that the Lorenz gauge can be reached from any starting perturbation, and that even after reaching it a genuine freedom remains. We compute how the divergence responds to a gauge transformation, find the change is a pure d'Alembertian of the gauge vector, and conclude both that a suitable always exists to zero it and that harmonic leave the condition intact — the residual freedom used later for the transverse-traceless gauge.
Step 1. Under the gauge transformation, . This is equation (4), obtained by trace-reversing the raw rule . Why: we work with the transformation of directly because it is , not , that the gauge sets to zero.
Step 2. Take the divergence of both sides: . The final two terms are identical up to a dummy relabeling and cancel exactly, leaving . Why: the trace term in equation (4) is exactly what makes the two single-derivative pieces cancel, so the entire change in the divergence is the clean wave operator — no leftover clutter.
Step 3. Demand ; this is the equation . On flat spacetime a retarded solution always exists, so the Lorenz gauge is reachable from any starting configuration. Why: reaching the gauge is not a lucky special case — it is the guaranteed solvability of the flat-space wave equation, the same fact that underlies retarded potentials everywhere in physics.
Step 4. Suppose the Lorenz condition already holds and ask which further transformations preserve it. From Step 2 with , the condition stays true iff . Four functions of harmonic gauge freedom survive. Why: this residual freedom is not a defect — in vacuum it is exactly enough to impose the transverse-traceless conditions and expose the two physical polarizations, so forgetting it leads directly to overcounting the degrees of freedom. *The cancellation of the terms is exact, and the four residual harmonic functions match the four Lorenz conditions one-for-one.*
Go deeper · Derivation C · 1 minConsistency demands energy-momentum conservation
The goal is to show that the Lorenz-gauge wave equation is not merely convenient but structurally consistent, and to trace that consistency to a physical law rather than an accident. We take the divergence of , use commuting derivatives and the gauge condition to show the left side vanishes identically, and conclude the source must be divergence-free — the linearized law that the contracted Bianchi identity guarantees.
Step 1. Differentiate the field equation: . On the left, the flat-space derivatives all commute, so . Why: commuting the divergence past the d'Alembertian is what lets the gauge condition, which constrains , act on the left-hand side at all.
Step 2. In Lorenz gauge , so . The left side of the differentiated equation vanishes identically, for every . Why: the gauge condition is not just imposed at one instant — it is maintained by the dynamics, so its d'Alembertian is zero throughout spacetime.
Step 3. The right side must therefore also vanish: , i.e. . Consistency of the Lorenz-gauge equation with the field equations is possible only if energy-momentum is locally conserved. Why: this is the linearized shadow of the contracted Bianchi identity — the same geometric identity that forces conservation in the full theory reappears here as the integrability condition for the wave equation. *The chain is the flat-space limit of .*
Limiting cases
The single equation contains several familiar theories as special cases. Reading across the table is a good check that the Lorenz gauge really is the common root of Newtonian gravity, gravitational waves, and everything between.
| Case | Result | Meaning |
|---|---|---|
| Vacuum | Source-free region; each component is a homogeneous wave — the equation of gravitational-wave propagation. | |
| Newtonian / static | Time derivatives drop and dominates; with this is Poisson's equation . | |
| Residual gauge | preserved | Leftover coordinate freedom that keeps the gauge; the handle used to reach the transverse-traceless frame. |
| Transverse-traceless (vacuum, residual gauge fixed) | The ten components collapse to two physical polarizations and . | |
| Slow-motion far zone | Expanding the retarded integral yields the quadrupole formula, the workhorse of binary-inspiral predictions. |
Worked examples
1 · The Newtonian limit at the surface of the Sun (fully worked)
Take the Sun as a static source and use the Lorenz-gauge equation to (a) recover Newton's law of gravity and (b) estimate the size of the metric perturbation at the solar surface, checking that linearization is justified. Use , , .
Step 1. Specialize the field equation. For a static, slowly moving source the dominant stress-energy component is (mass-energy density) and all time derivatives vanish, so . The component of becomes in units where .
Step 2. Introduce the Newtonian potential. Write (with the dimensionless potential). Substituting, , which rearranges to — exactly Poisson's equation for Newtonian gravity. The trace-reversed variable is essential here: had we used directly, the trace terms would have spoiled the clean factor of .
Step 3. Read off the metric. Undoing the trace reversal gives . With only non-negligible one finds , so — the standard weak-field time-time metric, the piece that produces gravitational time dilation.
Step 4. Put in the numbers. At the solar surface the potential is :
The perturbation is therefore .
Step 5. Check linearization. Since , the weak-field expansion is superbly justified at the Sun's surface — the linear theory is accurate to parts in , and the neglected second-order terms are of order . The Lorenz gauge reproduces Newton exactly in the static limit, and confirms that the Solar System is deep in the weak-field regime. (For comparison, the same estimate at Earth's surface gives , and only at a neutron-star surface, , does linearization finally break down.)
2 · Counting the polarizations of a plane gravitational wave
A gravitational wave in vacuum is . Show how the wave equation, the Lorenz condition, and the residual gauge cut the ten amplitudes down to two.
Step 1. The wave equation fixes the frequency. Substituting into gives , so is null — the wave travels at the speed of light, . A symmetric starts with independent components.
Step 2. The Lorenz condition removes four. becomes : the amplitude is transverse to the propagation direction. These are four linear constraints (one per ), leaving .
Step 3. The residual gauge removes four more. Harmonic vectors satisfy automatically and shift without leaving Lorenz gauge. The four functions let us impose the transverse-traceless conditions (traceless) and (purely spatial), removing four more amplitudes. That leaves .
Step 4. Name the survivors. For a wave along , the two remaining amplitudes are (the plus mode ) and (the cross mode ). A gravitational wave has exactly two physical polarizations, both transverse and traceless, in one-to-one correspondence with the counting of the second figure.
Physics of the portrait
The gauge that tames linearized gravity is named for a nineteenth-century Danish physicist most people have never heard of, and whose name is routinely misspelled into that of a more famous contemporary. The story is worth telling because it is a small monument to how physics remembers — and misremembers — the people who build its tools.
Origins · 1 minLudvig Lorenz and how this was discovered
Ludvig Valentin Lorenz was a Danish physicist working largely in isolation in Copenhagen, and in 1867 he introduced the gauge condition — the condition that turns the electromagnetic potentials into decoupled wave equations with retarded solutions. He arrived, independently of Maxwell and by a different route, at the idea that light is an electromagnetic disturbance propagating at a finite speed. The gauge is his. Yet for more than a century it was almost universally attributed to Hendrik Antoon Lorentz, the Dutch physicist of the Lorentz transformation — a far more famous name, differing by a single letter and also bound up with electrodynamics. The misattribution became so entrenched that "Lorentz gauge" appears in generations of textbooks; careful historical work by J. D. Jackson and others restored the correct name. When general relativity was linearized, the same mathematical condition reappeared — — and inherited the name by analogy, sitting alongside the equivalent "harmonic" or "De Donder" coordinate condition that Théophile De Donder introduced for gravity in 1921. Lorenz's gauge is now one of the most-used tools in all of field theory — the quiet workhorse behind retarded potentials, gravitational waves, and quantum field theory in covariant gauges.
Going further
References. Misner, Thorne & Wheeler, Gravitation, §18.1–18.2 · Wald, General Relativity, §4.4 · Carroll, Spacetime and Geometry, §7.1 · Schutz, A First Course in General Relativity, §8.3 · Hartle, Gravity, §21.4 · Maggiore, Gravitational Waves, Vol. 1, §1.2 (linearized theory and gauge fixing). Key checkpoints in the derivations: the trace identity holds in four dimensions (equation 2); all three mixing terms vanish under (Derivation 1); the pieces cancel exactly in the divergence of (Derivation 2, Step 2); the coefficient follows from with ; the Newtonian normalization recovers the correct Poisson equation; and the solar-surface numbers are , (Worked Example 1). The historical attribution of the gauge to Ludvig Lorenz (not H. A. Lorentz) is due to J. D. Jackson.
Prerequisites. The Weak-Field Approximation · The Einstein Field Equations · The Einstein Tensor · Local Conservation of Energy-Momentum · The Stress-Energy Tensor. Leads to. The Newtonian Limit · Gravitational Waves · Post-Newtonian Expansion.
Ask the tutor: Ask me to walk through why the four "mixing" terms in the linearized Einstein tensor all vanish under , or to count a gravitational wave's polarizations from ten components down to two.
Is the Lorenz gauge the same thing as the harmonic gauge?
Yes — two names for the same condition from different directions. "Lorenz gauge" emphasizes the electromagnetic analogy, mirroring . "Harmonic" (or "De Donder") gauge emphasizes the coordinate viewpoint: it is equivalent to requiring each coordinate function to satisfy the covariant wave equation , i.e. to be harmonic. At linear order the two coincide exactly, which is why textbooks use the names interchangeably. The harmonic phrasing generalizes cleanly to the full nonlinear theory, where it stays a well-posed choice for numerical relativity.
Why is it "Lorenz" and not "Lorentz"?
Because the gauge is due to Ludvig Lorenz, a Danish physicist, who introduced in 1867 — not to Hendrik Antoon Lorentz, the Dutch physicist of the Lorentz transformation. The two names differ by a single letter, both belong to nineteenth-century electrodynamicists, and Lorentz was by far the more famous, so for over a century the condition was misattributed to him and printed as "Lorentz gauge" in countless textbooks. Historians of physics, notably J. D. Jackson, traced the condition correctly to Lorenz, and modern usage has largely restored the right spelling. It is a genuine attribution error, not a variant spelling — so "Lorenz gauge" is correct even though your older textbook may say otherwise.
Does choosing a gauge change the physics?
No — that is the point of it being a gauge. The physical content lives in the curvature (the linearized Riemann tensor and its invariants), which is unchanged by any . Two perturbations related this way describe the identical spacetime in different coordinates. Choosing the Lorenz gauge adds and removes no physics; it merely selects coordinates in which the equations decouple. Any observable — a tidal force, a wave's strain, an orbital precession — comes out the same in every gauge. The gauge is a powerful convenience, never a physical input.
Why trace-reverse — why not just impose ∂μhμν = 0 directly?
Because the divergence in the mixing terms of the linearized Einstein tensor is that of , not of . The cross terms involve . Setting leaves the piece behind and fails to decouple the equations; setting kills the whole combination at once. The trace reversal is exactly the bookkeeping that aligns the gauge condition with the structure of the equations, and it gives the clean normalization with the raw as source.
Does the Lorenz gauge fix the coordinates completely?
No — a subtle but important point. The four conditions use up the four functions of coordinate freedom you started with, but they leave a residual: any gauge vector satisfying preserves the Lorenz condition. In a source-free region that residual is exactly what you spend to reach the transverse-traceless gauge, where a wave shows its true two-polarization character. Treat the Lorenz gauge as a complete fixing and you will overcount — concluding a gravitational wave has six modes, or four, when it has two. The residual freedom is essential, not a loose end.
Why the factor −16πG, and not −8πG as in the Einstein equations?
The factor of two comes directly from the trace reversal. The Einstein field equations read , and at linear order in Lorenz gauge (Derivation 1, Step 3). Setting these equal gives , so . The extra factor of two is the same that appears in the definition of the trace-reversed variable, now inverted. You can double-check the constant physically: it is exactly what makes the static component collapse to Poisson's equation with the correct Newtonian coefficient, as Worked Example 1 shows.
Is the wave equation □h̄μν = −16πG Tμν exact or approximate?
It is exact within linearized gravity, but linearized gravity is itself an approximation to the full nonlinear theory. It drops all terms of second order and higher in — including the energy carried by the gravitational field itself, a second-order effect that does not appear as a source here. For weak fields this is superb: at the Sun's surface , so the neglected terms are . It breaks down where gravity is strong — near a horizon or in a merger's final plunge — and there one adds post-Newtonian corrections order by order or solves the full equations numerically. The linearized equation is the leading term of a controlled expansion, not a standalone law.