Detection of the stochastic gravitational wave background with the space-borne gravitational-wave detector network
Jun Cheng, En-Kun Li, Jianwei Mei
TL;DR
This work develops a Bayesian cross-correlation framework for stochastic gravitational-wave background detection using two space-based detectors (TianQin and LISA) and time-varying overlap reduction functions. By segmenting data to handle orbital motion and computing the ORFs numerically, the authors demonstrate improved parameter estimation and detection limits for isotropic SGWB models (power-law, flat, and single-peak) within a three-month observation. The TianQin–LISA network yields notably tighter constraints on spectral parameters and achieves detectable amplitudes down to $\Omega_{\rm PL}=6.0\times10^{-13}$, $\Omega_{\rm Flat}=2.0\times10^{-12}$, and $\Omega_{\rm SP}=1.2\times10^{-12}$, outperforming a single detector. The study highlights the value of detector networks for SGWB science in the mHz band and points to future extensions incorporating full A,E,T channels and astrophysical foregrounds.
Abstract
The stochastic gravitational wave background (SGWB) is one of the main detection targets for future millihertz space-borne gravitational-wave observatories such as the \ac{LISA}, TianQin, and Taiji. For a single LISA-like detector, a null-channel method was developed to identify the SGWB by integrating data from the A and E channels with a noise-only T channel. However, the noise monitoring channel will not be available if one of the laser interferometer arms fails. By combining these detectors, it will be possible to build detector networks to search for SGWB via cross-correlation analysis.In this work, we developed a Bayesian data analysis method based on \ac{TDI} Michelson-type channel. We then investigate the detectability of the TianQin-LISA detector network for various isotropic SGWB. Assuming a three-month observation, the TianQin-LISA detector network could be able to confidently detect SGWB with energy density as low as $Ω_{\rm PL} = 6.0 \times 10^{-13}$, $Ω_{\rm Flat} = 2.0 \times 10^{-12}$ and $Ω_{\rm SP} = 1.2 \times 10^{-12}$ for power-law, flat and single-peak models, respectively.
