Nonlinear tails of massive scalar fields around a black hole
Caiying Shao, Zhen-Tao He, Jiageng Jiao, Jingqi Lai, Jun-Xi Shi, Yu Tian, Dandan Yuan, Hongbao Zhang
TL;DR
This work investigates nonlinear tails in massive scalar perturbations around a Schwarzschild black hole, addressing how nonlinear effects modify late-time decay and whether they leave observable imprints in ringdown signals. Using two setups—a moving-source toy model and a cubic self-interacting scalar field—the authors evolve perturbations with a double-null finite-difference scheme and perform perturbative analyses to second order. They find that, unlike the massless case, the intermediate-time tails for massive fields decay at the same rate as their linear counterparts, $t^{-l-3/2}$, with oscillations set by the mass $\mu$, and largely independent of source details; quadratic QNMs provide a distinct nonlinear signature with frequencies roughly doubling the linear QNMs. The results suggest linear theory suffices for tail modeling in this regime, while nonlinearities reveal themselves primarily through quadratic QNMs, motivating extensions to massive gravitational perturbations of rotating black holes for future gravitational-wave observational tests.
Abstract
Nonlinear effects play a fundamental role in the late-time ringdown of black holes, with direct implications for gravitational-wave observations. For massive fields, these dynamics become richer, yet their nonlinear signatures remain poorly understood. Here, we systematically study nonlinear tails of massive scalar perturbations, from a toy model with ingoing and outgoing sources to a self-interacting scalar model, revealing nonlinear tails and contrasting the results with their linear counterparts. We find that the nonlinear tails of massive scalar fields, opposite to massless ones, decay as the same rate as linear tails in the intermediate time, independent of source parameters or initial conditions. Nevertheless, quadratic quasinormal modes could serve as a probe to the nonlinear effects of massive fields.
