Gravitational Waves sourced by Gauge Fields during Inflation
Martin Teuscher, Ruth Durrer, Killian Martineau, Aurélien Barrau
TL;DR
This work shows that Abelian gauge fields amplified during slow-roll inflation through non-minimal kinetic and axial couplings generate a secondary gravitational-wave background that is scale invariant on super-horizon scales. The authors derive analytic expressions for the gauge-field mode functions, their unequal-time anisotropic-stress spectra, and the resulting GW power spectra, including a full treatment of the evolution through multiple post-inflationary eras. A key result is that a sizeable axial coupling exponentially boosts one GW helicity, yielding a strongly polarized, potentially observable GW signal that can dominate over the standard inflationary background for suitable parameters, while back-reaction constraints limit the allowed region of parameter space. The methodology—combining Whittaker-function solutions, unequal-time correlators, a UV-cutoff consistent with the electromagnetic horizon, and a general multi-era matching formalism—provides a comprehensive framework to predict and constrain gauge-field–sourced GWs in the early Universe with clear observational implications for Planck bounds and next-generation detectors like LiteBIRD.
Abstract
We study the inflationary gravitational wave background induced by Abelian gauge fields generated by non-minimal kinetic and axial couplings to the inflaton. We show that the gravitational wave spectrum is scale invariant and derive its amplitude for generic gauge field coupling parameters, within the slow-roll approximation. We constrain the coupling values and the scale of inflation for which the induced gravitational wave background is observable, while ensuring that back-reaction on the inflationary dynamics remains negligible. We find that a sizeable axial coupling can boost this secondary gravitational wave signal above the standard inflationary background. In the course of our analysis, we also show how to analytically match tensor perturbations across an arbitrary number of eras with different equations of state.
