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. Hence
The 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 gives
The middle terms cancel when the indices are symmetrized. Therefore
To 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) gives
In the second identity, the term with is zero. Thus
In 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 become
The 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, reads
It follows that and . Taking the trace gives
Expanding the scalar in these null coordinates therefore yields
where the coefficients are explicitly
The 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 that
For example, for any fixed one may take
A generator, specified as a covector with components in the null coordinates , is
Indeed, with , the mixed components cancel:
All components without a index vanish as well, and
Since , only the component needs changing. Thus
Yes, satisfies both equations (3). Its trace is zero, gives zero divergence, and the harmonic quadratic plane-wave profile gives
The 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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