Detecting gravitational waves from mountains on neutron stars in the Advanced Detector Era

TL;DR

This paper predicts gravitational wave signals from neutron star mountains in low mass X-ray binaries, suggesting persistent systems could be detectable by advanced detectors, with implications for understanding neutron star physics.

Contribution

It introduces a new analysis of GW emission from crustal and magnetic mountains in neutron stars, challenging previous assumptions about spin regulation mechanisms.

Findings

Thermal crustal mountains in transient LMXBs unlikely detectable

Persistent LMXBs are promising GW detection candidates

Magnetic mountain GW signals are generally weak unless magnetic fields are unusually strong

Abstract

Rapidly rotating Neutron Stars (NSs) in Low Mass X-ray Binaries (LMXBs) are thought to be interesting sources of Gravitational Waves (GWs) for current and next generation ground based detectors, such as Advanced LIGO and the Einstein Telescope. The main reason is that many of the NS in these systems appear to be spinning well below their Keplerian breakup frequency, and it has been suggested that torques associated with GW emission may be setting the observed spin period. This assumption has been used extensively in the literature to assess the strength of the likely gravitational wave signal. There is now, however, a significant amount of theoretical and observation work that suggests that this may not be the case, and that GW emission is unlikely to be setting the spin equilibrium period in many systems. In this paper we take a different starting point and predict the GW signal strength for two physical mechanisms that are likely to be at work in LMXBs: crustal mountains due to thermal asymmetries and magnetically confined mountains. We find that thermal crustal mountains in transient LMXBs are unlikely to lead to detectable GW emission, while persistent systems are good candidates for detection by Advanced LIGO and by the Einstein Telescope. Detection prospects are pessimistic for the magnetic mountain case, unless the NS has a buried magnetic field of $B\approx 10^{12}$ G, well above the typically inferred exterior dipole fields of these objects. Nevertheless, if a system were to be detected by a GW observatory, cyclotron resonant scattering features in the X-ray emission could be used to distinguish between the two different scenarios.