Transverse-traceless gauge
The coordinate choice that strips a gravitational wave down to its two physical degrees of freedom.
Definition
The transverse-traceless (TT) gauge is a choice of coordinates in linearized general relativity that isolates the genuine, gauge-invariant content of a gravitational wave from coordinate artifacts. Of the ten components of the symmetric metric perturbation h_{μν}, gauge freedom — the ability to relabel spacetime points via x^μ → x^μ + ξ^μ — allows eight to be eliminated, leaving exactly two physical degrees of freedom. The TT gauge accomplishes this in vacuum by imposing three conditions: the perturbation is purely spatial (h_{0μ} = 0), transverse or divergence-free (∂^i h_{ij} = 0), and traceless (h^i{}_i = 0).
In the TT gauge the coordinates ride along with freely-falling test masses, so the time coordinate of a free particle remains unchanged and every remaining wobble in h_{ij} is real tidal physics rather than coordinate noise. The two surviving components correspond to the 'plus' and 'cross' polarizations of the wave — for a wave traveling along z, a symmetric traceless 2×2 matrix in the transverse x–y plane. This is the gravitational analogue of fixing the Lorenz gauge ∂_μ A^μ = 0 in electromagnetism, which reduces Maxwell's equations to a clean wave equation and exposes the photon's two transverse polarizations.
The TT gauge is what makes a gravitational-wave detection meaningful. A detector like LIGO measures the gauge-invariant change in proper distance between mirrors — precisely the quantity the TT gauge isolates — so theoretical templates computed in the TT gauge can be matched directly against recorded strain. Historically, the inability to distinguish physical waves from gauge artifacts was the core of the confusion that led Einstein to doubt gravitational waves in 1936; the systematic gauge-fixing embodied by the TT gauge is the resolution of that confusion.
History
Developed through the 1950s and 1960s as theorists (Pirani, Bondi, Trautman, and others) clarified the gauge-invariant meaning of gravitational radiation following the 1936 Einstein–Rosen controversy and the 1957 Chapel Hill conference where the sticky-bead argument was aired.