News release
From:
Springer Nature
Astronomy: Gravitational wave signal from a black hole collision
The identification of the wave component of the gravitational-wave signal produced from the collision between two black holes is presented in Nature this week. Observations of the binary black hole merger event called GW250114 provides information about the remnant black hole event horizon —the ‘point of no return’.
Understanding the physics that guide a black hole event horizon is difficult as most observations are indirect; gravitational waves, which are formed by the collision of two black holes, could offer a clearer picture. Previous research has suggested that direct waves, a type of gravitational wave that can characterize the behaviour of the remnant black hole, could be emitted during this process, but no observation has been recorded.
Sizheng Ma and colleagues analysed gravitational wave data from GW250114, a signal from the collision of two merging black holes, detected by the Laser Interferometer Gravitational-Wave Observatory (LIGO) in January 2025. They observed a direct wave from the collision, which behaved like a dampened oscillation with a frequency linked to the horizon’s rotation and a decay rate related to its surface gravity.
Careful modelling of the direct wave can tell us the mass and spin rate of the remnant black hole, and the authors make a preliminary attempt with some simplifying assumptions. Future work will require more accurate waveform models and studies across multiple events to assess the robustness and universality of these signals.
Journal/
conference:
Nature
Organisation/s:
The Australian National University, Perimeter Institute for Theoretical Physics, Canada
Funder:
This material is based on work supported by NSF’s LIGO Laboratory, which is a major
facility fully funded by the National Science Foundation. We are grateful for computational
resources provided by the LIGO Laboratory and supported by National Science Foundation
grants PHY–0757058 and PHY–0823459. N.L., O.J.P. and L.S. acknowledge support for this
research from the Australian Research Council Centre of Excellence for Gravitational Wave
Discovery (OzGrav), project no. CE230100016. L.S. is also supported by the Australian
Research Council Discovery Early Career Researcher Award, project no. DE240100206. O.J.P.
is supported by the Spanish Ministerio de Ciencia, Innovacion y Universidades Ramon y Cajal,
RYC2023-044489-I funded by MCIN/AEI/10.13039/501100011033 and the FSE+ and cofinanced
by the Universitat de les Illes Balears (UIB). This work was supported by UIB with funds from
the Programa de Foment de la Recerca i la Innovació de la UIB 2024-2026 (supported by the
yearly plan of the Tourist Stay Tax ITS2023-086); the Spanish Agencia Estatal de Investigación
grants RED2024-153978-E, RED2024-153735-E, funded by MICIU/AEI/10.13039/501100011033
and the ERDF/EU; and the Comunitat Autónoma de les Illes Balears through the Conselleria
d’Educació i Universitats with funds from the ERDF (SINCO2022/18146). S.M. acknowledges
support for this research at Perimeter Institute, in part from the Government of Canada
through the Department of Innovation, Science and Economic Development and by the
Province of Ontario through the Ministry of Colleges and Universities. Y.C. is supported by
the Brinson Foundation, the Simons Foundation (award no. 568762), and by US NSF grants
PHY–2309211 and PHY–2309231. This paper carries LIGO document no. DCC–P2500608.