Past exam of the mathematics course of the University of Cambridge 2001 iii Paper 68 2 Solution Created 2026-10-03 Updated 2026-10-14
Use , background Minkowski spacetime metric tensor , and with small metric perturbation. All indices and derivatives in this linear approximation use . The linearized inverse metric is , and the linearized Levi-Civita connection isDefine the trace-reversed metric perturbation , with .
An infinitesimal coordinate change gives the linearized coordinate gauge transformationThe metric perturbation therefore has redundant components. The gauge invariance of the linearized Riemann tensor follows because its change contains third derivatives of cancelling by commutation of partial derivatives. Conversely, flat linearized metric perturbations are locally pure gauge on a contractible patch. Thus linearized curvature, rather than a particular coordinate value of , detects the physical disturbance. Gauge freedom can also be restricted by global topology or boundary conditions.
Keeping the paper's curvature sign convention, its linearized Ricci tensor and scalar areThese are the negatives of the alternative frequently used curvature convention. Put . The Linearized Einstein equations in vacuum areUnder a gauge change , so solving imposes the Lorenz gauge in linearized gravity. The field equations then become . The remaining residual gauge symmetry of linearized gravity has ; Lorenz gauge does not exhaust the coordinate freedom.
A Fourier mode obeys and . Hence the plane gravitational waves in linearized gravity propagate on the background light cones. Four transversality conditions and four residual gauge amplitudes leave physical degrees of freedom. The explicit plane-wave reduction to transverse-traceless gauge can set , spatial trace zero and . For a wave in the direction, write its physical spatial strain as , so the spatial metric tensor is :There are two gravitational wave polarizations, plus polarization and cross polarization. Rotating transverse axes through rotates their amplitude pair through . Nonconstant profiles with nonzero second derivative have nonzero linearized Riemann curvature tensor and cannot be removed as pure gauge.
The TT coordinate separation and measured separation distinction explains a detector's response. Freely falling particles initially at rest can keep fixed TT coordinates, since , while their proper separation changes. For a short arm along a unit vector ,This is the tidal response described by geodesic deviation; coordinate motion by itself is not the measured signal.
Finally, gravitational-wave energy is second order in the perturbation, so it is absent from a first-order vacuum equation. In a short-wavelength averaging regime the averaged stress-energy of transverse gravitational waves isFor a plane wave its energy flux is . The averaging scale and weak-field assumptions matter: this does not assign a coordinate-independent local gravitational energy density to an arbitrary first-order perturbation.