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Nonlinear effect of absorption on the ringdown of a spinning black hole
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The ringdown gravitational wave signal arising e.g., in the final stage of a black hole binary merger, contains important information about the properties of the remnant, and can potentially be used to perform clean tests of general relativity. However, interpreting the ringdown signal, in particular when it is the loudest, requires understanding the role of nonlinearities and their potential impact on modelling this phase using quasinormal modes. Here, we focus on a particular nonlinear effect arising from the change in the black hole's mass and spin due to the partial absorption of a quasinormal perturbation. We isolate and systematically study this third-order, secular effect by evolving the equations governing linear metric perturbations on the background of a spinning black hole, but allowing the properties of the background to evolve in a prescribed way. We find that this leads to the excitation of quasinormal modes with higher polar angular number, retrograde modes (counter-rotating with respect to the black hole), and overtones, as well as giving rise to a component of the signal at early times that cannot be fully described using quasinormal modes. Quantifying these effects, we find that they may be relevant in analyzing the ringdown in black hole mergers.
Forward citations
Cited by 3 Pith papers
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Probing Direct Waves in Black Hole Ringdowns
Merger gravitational wave signals contain a 'direct wave' from the plunging companions, screened by the remnant's potential, with frequency near the superradiant value for high-spin remnants and SNR above 10 in GW1509...
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Perturbations of Plane Waves and Quadratic Quasinormal Modes on the Lightring
Second-order gravitational perturbations on plane waves are solved with a GHP master equation and tensor harmonics, yielding quadratic quasinormal mode ratios and selection rules.
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Constraining deviations from the Teukolsky equation with GW250114
GW250114's fundamental ringdown mode bounds theory-agnostic deviations from the Teukolsky equation to be consistent with zero at characteristic scales of 60-100 km.
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