For the plane gravitational wave in linearized gravity, the chain rule gives . The Lorenz gauge in linearized gravity, called wave gauge in the paper, imposes zero divergence of the trace-reversed metric perturbation. HenceThe wave equation itself holds for any smooth profile of , because for the constant null vector .
Use the active sign convention for the linearized coordinate gauge transformation, . The paper's prescribed generator has precisely this sign; using the passive convention would require its negative. Direct partial differentiation givesThe middle terms cancel when the indices are symmetrized. ThereforeTo test both equations (3), put , the trace of the original metric perturbation. Since is a null vector, and its trace-reversed metric perturbation equals . Differentiating the result of part (a) givesIn the second identity, the term with is zero. ThusIn general does not satisfy (3). On an open interval of , both equations hold exactly when there: the first equation forces this for , and smoothness gives it at as well. A linearized coordinate gauge transformation preserves the linearized vacuum Einstein equations, but only a residual gauge symmetry of linearized gravity preserves the imposed Lorenz gauge in linearized gravity.
For an explicit failure, use the null coordinates of part (c) and take only nonzero. Then , the original field obeys (3), but gives and .
With and , the Minkowski metric and the specified null vector becomeThe Minkowski wave operator in null coordinates is . All components of the original metric perturbation still depend only on , since this coordinate change is linear. The result of part (a), differentiated once, readsIt follows that and . Taking the trace givesExpanding the scalar in these null coordinates therefore yieldswhere the coefficients are explicitlyThe quadratic transverse term is a harmonic quadratic plane-wave profile. In particular , and , consistently reproducing the failure of wave gauge in part (b).
Continue with the active sign convention for the linearized coordinate gauge transformation. Choose local functions of by integration so thatFor example, for any fixed one may takeA generator, specified as a covector with components in the null coordinates , isIndeed, with , the mixed components cancel:All components without a index vanish as well, andSince , only the component needs changing. ThusYes, satisfies both equations (3). Its trace is zero, gives zero divergence, and the harmonic quadratic plane-wave profile givesThe two surviving functions encode the two gravitational wave polarizations; constant and linear transverse terms have been removed by the explicit linearized coordinate gauge transformation.
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