The Missing Multipole Problem: Investigating biases from model starting frequency in gravitational-wave analyses
Ryan Ursell, Charlie Hoy, Ian Harry, Laura K. Nuttall
TL;DR
The paper investigates biases introduced when time-domain gravitational-wave templates start at frequencies that omit low-frequency content from higher-order multipoles, focusing on heavy ($M\gtrsim 200\,M_\odot$) binary black holes. Using zero-noise injections with NRSur7dq4 across $200\le M\le 450\,M_\odot$, $0.25\le q\le1$, and varying spins and inclinations, it demonstrates that starting at $f_{22}=20$ Hz biases recovery for $M\gtrsim 250$–$300\,M_\odot$, while including $(3,3)$ via $f_{22}=13$ Hz or lower mitigates biases up to $\rho\lesssim70$, and including $(4,4)$ with $f_{22}=10$ Hz becomes essential at higher masses or SNRs. The study quantifies biases using the Mahalanobis recovery score and Bayesian evidences, and confirms findings on a real event GW231123_135430, offering practical guidelines for selecting template starting frequencies in current and future gravitational-wave analyses. Overall, it highlights the importance of including higher-order multipoles for accurate parameter estimation in short-duration, high-mass systems and provides mass-, spin-, inclination-, and SNR-dependent recommendations to minimize systematic biases.
Abstract
Our ability to infer the true source properties of colliding black holes from gravitational wave observations requires not only accurate waveform models but also their correct use. A key property when evaluating time-domain models is when to start the waveform: choosing a time that is too late can omit low-frequency power from higher order multipoles. By focusing on binary systems with total mass $\ge 200 \, M_{\odot}$, we show that current detectors are sensitive to this missing power and biased source properties can be obtained. We show that for systems with total mass $\lesssim 300 \, M_{\odot}$, mass ratio $\gtrsim 0.33$, and signal-to-noise ratio $ρ\gtrsim 20$, templates starting at $20 \, \mathrm{Hz}$ recover biased source properties. As the total mass increases, and the component masses become more asymmetric, templates starting from $13 \, \mathrm{Hz}$ recover biased properties. If the gravitational-wave signal is observed at signal-to-noise ratio $ρ< 20$, time-domain models can start from $20\, \mathrm{Hz}$ as statistical uncertainties dominate.
