A passing gravitational wave can shake a static electric field and make it radiate, study finds
The paper studies how a single electric charge that is freely falling in a passing gravitational wave stops having a perfectly static Coulomb field and instead develops a time‑varying electromagnetic field that radiates. The authors treat the gravitational wave as a small disturbance of flat spacetime and solve Maxwell’s equations for the electromagnetic potential of the point charge to first order in that small disturbance. In plain terms, the gravity wave perturbs the space around the charge and this makes the charge’s electric field change in time and send out electromagnetic waves.
To get concrete results the authors work in the standard weak‑field approximation: the metric of spacetime is the Minkowski metric (flat spacetime used in special relativity) plus a small perturbation representing the gravitational wave. They keep only first‑order terms in that perturbation. The charge is placed at the coordinate origin and, in these coordinates, a freely falling charge that was initially at rest remains at rest; the changing physical distance comes from the metric change. Using this setup they rewrite Maxwell’s equations in the gravitational‑wave background and derive an effective source current. The disturbance of the usual Coulomb potential is then expressed as volume integrals (the paper calls these solutions “in quadratures,” i.e., given by explicit integrals) over that effective current.
A notable technical issue that previous authors encountered is that if a gravitational wave is assumed to fill all space and time, the electromagnetic radiation produced by a point charge can formally become infinite. To avoid this divergence, the authors introduce a regularization motivated by the Shapiro time delay. The Shapiro effect is the fact that gravity slows the coordinate speed of light seen by a distant observer, producing a time delay for signals; here a similar idea is used so that the effective travel time of electromagnetic signals through the perturbed region makes the integrals converge. In the linear approximation the coordinate speed differs from the vacuum speed only at second order, so the authors explain that the regularizing assumption is what makes the energy and radiation intensity finite in their calculation.