Gravitational-wave parameter inference with the Newman-Penrose scalar

Abstract

Current detection and parameter inference of gravitational-wave signals relies on the comparison of the incoming detector strain data d(t)d(t) to waveform templates for the gravitational-wave strain h(t)h(t) that ultimately rely on the resolution of Einstein's equations via numerical relativity simulations. These, however, commonly output a quantity known as the Newman-Penrose scalar ψ4(t)\psi_4(t) which, under the Bondi gauge, is related to the gravitational-wave strain by ψ4(t)=d2h(t)/dt2\psi_4(t)=\mathrm{d}^2h(t) / \mathrm{d}t^2. Therefore, obtaining strain templates involves an integration process that introduces artefacts that need to be treated in a rather manual way. By taking second-order finite differences on the detector data and inferring the corresponding background noise distribution, we develop a framework to perform gravitational-wave data analysis directly using ψ4(t)\psi_4(t) templates. We first demonstrate this formalism through the recovery numerically simulated signals from head-on collisions of Proca stars injected in Advanced LIGO noise. Next, we re-analyse the event GW190521 under the hypothesis of a Proca-star merger, obtaining results equivalent to those in Ref [1], where we used the classical strain framework. Our framework removes the need to obtain the strain from numerical relativity simulations therefore avoiding the associated systematic errors.Comment: 18 pages, 9 Figure

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