Estimating Stochastic Gravitational Wave Backgrounds with Sagnac Calibration
Craig J. Hogan, Peter L. Bender
TL;DR
The paper presents a noise-calibration strategy for space-based detectors like LISA using the symmetrized Sagnac observable $\zeta$ to distinguish instrumental noise from a broadband stochastic gravitational-wave background. By formulating estimators such as $E_k = \eta_k^2 - D(f)|\zeta_k|^2$ (and high-/low-frequency variants like $E_k = \eta_k^2 - [S_{ave}/S_\zeta]_{est}|\zeta_k|^2$) and exploiting bandwidth averaging with $B \approx f/2$, the approach can substantially enhance sensitivity to isotropic GW backgrounds beyond traditional single-frequency estimates. The method has direct implications for astrophysical backgrounds from galactic/extragalactic binaries and primordial backgrounds, predicting improvements in detectable $h_{rms}$ levels by up to an order of magnitude in pivotal bands and offering insights into star-formation history, binary evolution, and early-Universe physics. The paper also discusses a high-frequency follow-on mission with shorter arms and superior noise performance, which could extend Sagnac-calibrated measurements to higher frequencies (up to ~0.1 Hz) and tighten constraints on primordial backgrounds, potentially rivaling cross-correlation methods with a single antenna.
Abstract
Armstrong et al. have recently presented new ways of combining signals to precisely cancel laser frequency noise in spaceborne interferometric gravitational wave detectors such as LISA. One of these combinations, the symmetrized Sagnac observable, is much less sensitive to external signals at low frequencies than other combinations, and thus can be used to determine the instrumental noise level. We note here that this calibration of the instrumental noise permits smoothed versions of the power spectral density of stochastic gravitational wave backgrounds to be determined with considerably higher accuracy than earlier estimates, at frequencies where one type of noise strongly dominates and is not substantially correlated between the six main signals generated by the antenna. We illustrate this technique by analyzing simple estimators of gravitational wave background power, and show that the instrumental sensitivity to broad-band backgrounds at some frequencies can be improved by more than an order of magnitude over the standard method, comparable to that which would be achieved by cross-correlating two separate antennas. The applications of this approach to studies of astrophysical gravitational wave backgrounds generated after recombination and to searches for a possible primordial background are discussed.
