Past exam of the mathematics course of the University of Cambridge 2016 iii Paper 309 4 iii Solution Created 2026-10-03 Updated 2026-10-06
Put and write , where , and . Physical fields are the real parts. Use here, and take the initial separation at equal time, so . For propagation in the positive direction one may set ; only enters the answer.
The linearized Levi-Civita connection in this transverse-traceless gauge has the potentially nonzero componentswith all others zero to this order. In particular , so a particle initially at rest has fixed spatial coordinates in transverse-traceless gauge, and equals its proper time. Expanding the Riemann curvature tensor givesThe plus sign in the last expression agrees with in the geodesic deviation convention above.
For the separation measured in a parallel-propagated orthonormal frame, write . The frame removes the connection terms from the time derivative, so the geodesic deviation equation reduces to at first order. The observable transverse relative acceleration isThese are the plus polarization and cross polarization tidal patterns; there is no longitudinal acceleration. The curvature is evaluated along the reference worldline, and replacing by on the right changes only second-order terms. This is the infinitesimal-separation approximation intrinsic to geodesic deviation.
There is an important component distinction if the symbols are instead interpreted literally in the transverse-traceless gauge coordinate basis. Expanding the left side, rather than replacing a covariant derivative by an ordinary derivative, givesThus in TT coordinatesWith zero initial coordinate displacement and velocity, throughout. This does not remove the physical gravitational wave strain. To first order an orthonormal coframe in spacetime along the reference worldline is ; its dual frame is parallel propagated because . Henceafter choosing the initial flat-frame reference. The TT coordinate separation and measured separation distinction accounts exactly for the apparently different accelerations. In a region initially free of the wave, the measured displacement is with the corresponding initial conditions.