Fast analysis

of long gravitational wave signals

Jacopo Tissino

GSSI

2026-07-20

Outline

  • GW250114: what we learned from the best\(^*\) black hole coalescence ever;
  • as seen by the Lunar Gravitational Wave Antenna:
    • the arrival time problem;
  • as seen by the Einstein Telescope:
    • multimodalities and configuration comparison.

GW250114: the clearest signal yet

11 years ago: GW150914

A decade of improvement

What the detectors saw

How we modelled it

How we interpreted it

Two black holes colliding, with masses \(m_1 = 33.6_{-0.8}^{+1.2} M_{\odot}\) and \(m_2 = 32.2_{-1.3}^{+0.8} M_{\odot}\).

Small spins \(|\chi_{1, 2}| \leq 0.26\), negligible eccentricity \(e_{13 \text{Hz}} \leq 0.03\).

How we analyzed it

Bayesian inference, accounting for our uncertainty on:

  • source masses \(m_i\) and spins \(\vec{\chi}_i\);
  • source location \((\alpha, \delta)\) and distance \(d_L\);
  • source inclination \(\theta_{\text{JN}}\) and polarization \(\psi\);
  • coalescence phase \(\phi_c\) and merger time \(t_c\);
  • eccentricity \(e\) and eccentric anomaly \(\zeta\);
  • detector calibration.

The observed ringdown

Modelling the ringdown

A superposition of damped sinusoids: quasinormal modes.

\[ \begin{aligned} h_{+}(t)-ih_{\times}(t) &\approx \sum_{\ell=2}^{\infty} \sum_{m=-\ell}^{\ell} \sum_{n=0}^{\infty} h_{\ell m n} S_{\ell mn} \\ h_{\ell m n} &= A_{\ell mn} \exp\left[i(\omega_{\ell mn}(t-t_\text{ref})+\phi^{x}_{\ell mn})\right] \\ \omega_{\ell mn} &= 2 \pi f_{\ell mn} + i / \tau _{\ell mn} \end{aligned} \]

For earlier signals, \(\ell mn = 220\) was sufficient.

Testing the Kerr hypothesis

For GW250114, the overtone \(\ell mn = 221\) was also required to explain the data.

Under the Kerr assumption, perturbation theory predicts the spectrum \(f_{\ell mn} (M_f, \chi_f)\).

We parameterize deviations as

\[ f_{221} = e^{\delta f_{221}} f_{221}^{\text{Kerr}} \]

Testing the Kerr hypothesis

We’ll come back to GW250114.

To get long gravitational wave signals, we need lower frequencies, which require a quiet place.

Lunar Gravitational Wave Antenna

The lunar north pole

Detector configuration

Measuring seismic motion at 4 locations inside a lunar crater, with cryogenics and seismic noise cancellation.

Watt’s linkage

Pendulum + inverted pendulum.

We measure horizontal displacement between the ground and this inertial mass, along two axes.

The Moon as a sensor

The displacement measured at the detector is

\[ s(t _{\text{det}}; f) = h_{ij}(t; f) D_{ij}(t _{\text{det}}) L(f) + \text{noise} \]

with

\[ D = \text{vertical} \otimes \text{horizontal} \]

\[ L(f) = \frac{\text{ground displacement}}{\text{GW strain}} \]

Sensitivity curve

The deci-Hertz band

GW250114 with the LGWA

The signal’s arrival time

When did the signal arrive?

Detector motion causes a nonlinear relation between source-frame and detector-frame time,

\[ t _{\text{det}} = t + t_0 - \frac{\hat{n} \cdot \vec{r}(t _{\text{det}})}{c}\,, \]

  • \(\vec{r}\) connects the origin and the detector’s position,
  • \(\hat{n}\) points to the GW source.

The timing parameter is:

\[ t _{\text{ref}} = \text{time when a reference event reaches the origin}\,. \]

What origin?

Standard approaches:

  • space-based detectors: the Solar System Barycenter (SSB),
  • ground-based detectors: the center of the Earth,
    • only valid assuming a short observation, such that \(\vec{r}_{\text{Earth}} \approx \vec{r}_0 + \vec{v} t\).

New approach:

  • SSB with a constant shift of origin.

Why does it matter? An experiment

  • correlations between \(t_{\text{ref}}\) and sky position lead to:
    • increased uncertainty on \(t_{\text{ref}}\) (requires a larger prior)
    • a more complex likelihood surface (difficult sampling)
Likelihood evaluations Sampling time [min] Timing uncertainty [s] Prior width [s] Origin
\(0.8\times 10^6\) 17 0.075 0.5 shifted
\(1.5\times 10^6\) 33 0.075 27 shifted
\(9.1\times 10^6\) 199 4.733 27 SSB

What reference event?

Impact of a different reference event

Recap: combining the two

Uncertainty on \(t_{\text{ref}}\) is a proxy for sampling efficiency.

It depends on origin position \(\vec{r}_0\) and reference frequency \(f\).

As a function of \(f\), we can compute

\[ \vec{r}_{\text{opt}}(f) = \text{argmin}_{\vec{r}_0} \text{var} [t_{\text{ref}}(\vec{r}_0, f)] \]

and reframe this as \(\vec{r}_{\text{opt}}(t)\) using the signal’s \(t(f)\).

Multi-band with the Einstein Telescope

The multi-band concept

The multi-band horizon

Einstein Telescope configurations

  • ET-\(\Delta\): equilateral triangle with 10km arms;
    • location: EMR region.
  • ET-2L: two L-shaped detectors with 15km arms;
    • locations: Sardinia and Saxony;
    • misaligned arms by \(45^\circ\).

GW250114, now and in the future

We compare:

  • The LVK detection of GW250114 (SNR 77–80);
  • a zero-noise injection with the LGWA (SNR 35);
  • a zero-noise injection with ET-\(\Delta\) (SNR 682);
  • a zero-noise injection with ET-2L (SNR 835).

Intrinsic parameters

  • LGWA complementary with ET on mass;
  • LGWA more precise than LVK on effective spin.
  • ET extremely precise on mass ratio and spin.

Extrinsic parameters

  • LGWA localization tighter and “rounder” than LVK;
  • inclination not well constrained by LGWA;
  • ET-2L: tight, near Gaussian.
  • ET-\(\Delta\): tight, bimodal!

Multimodalities with Einstein Telescope

GW250114 with ET-\(\Delta\)

Symmetry in the antenna patterns

The GW signal is obtained as

\[ h(t) = F_+ h_+(t) + F_{\times} h_{\times}(t) \]

The antenna patterns \(F_{+ / \times}^{\text{ET-}\Delta}\), a function of the local sky coordinates, altitude \(\beta\) and azimuth \(\lambda\), are symmetric1 under:

  • \(\beta \to - \beta\),
  • \(\lambda \to \lambda + \pi / 2\).

Massive BBH: sky posterior

Massive BBH: multimodalities

Sky localization modes for high mass

(\(150 M_{\odot} \lesssim \mathcal{M} \leq 1100 M_{\odot}\))

and distant (\(D_L \gtrsim 6 \text{Gpc}\)) BBH.

How to resolve these multimodalities?

  • imprint of the rotation of the Earth;
  • imprint of frequency-dependent antenna patterns;
  • short-baseline triangulation;
  • other detectors.

GW250114: arrival times at the vertices

Summary

  • The Kerr metric is still compatible with observations;
  • the LGWA could have measured GW250114 and provided strong constraints:
    • standard analysis assumptions need to be revised for deci-Hertz observations;
  • the Einstein Telescope could have exquisitely measured GW250114:
    • but in its \(\Delta\) configuration it would have exhibited a multimodality.

Extra information

Ask me about

  • Hawking’s area theorem constrained with GW250114;
  • caveats to LGWA analyses;
  • the LGWA’s localization capabilities;
  • the variation of timing uncertainty with position.

The thesis is available as a website at https://jacopok.github.io/thesis.

Testing Hawking’s area theorem

The area of a black hole is:

\[ \mathcal{A}(M, \chi) = 8 \pi \left( \frac{GM}{c^{2}} \right)^{2} \left( 1+\sqrt{ 1-\chi^{2} } \right) \]

Hawking’s area theorem implies:

\[ \mathcal{A_i} = \mathcal{A}_1 + \mathcal{A}_2 < \mathcal{A_f} \]

We tested this ignoring the strong-field portion of the signal.

Testing Hawking’s area theorem

  • Data before \(t_<\) leads to \((1+z)^2 \mathcal{A_i}\).
  • Data after \(t_>\) leads to \((1+z)^2 \mathcal{A_f}\).

A violation of the theorem would be

\[ \frac{\mathcal{A_f} - \mathcal{A_i}}{\mathcal{A_i}} < 0. \]

Main caveats for LGWA

  • Assuming a known lunar response \(L(f)\);
  • assuming no data gaps due to lunar events;
  • assuming stationary noise;
  • assuming a simple geometry for seismic wave propagation;
  • working directly in the frequency domain with a heterodyned likelihood;
  • only considering the dominant, \(\ell |m| = 22\) mode of GW emission with a Post-Newtonian model;
  • performing zero-noise injections.

Moonquakes

On the zero-noise assumption

On the zero-noise assumption

Analytical timing uncertainty

Length scale of the timing uncertainty variation:

\[ r \sim c \frac{\sigma_t}{\sigma_\theta} \]

  • \(r\) is the displacement to get a doubling of the timing variance;
  • \(\sigma_t\) is the minimal timing uncertainty;
  • \(\sigma_\theta\) is the angular parameter uncertainty along a given axis.

Timing uncertainty ellipses

Analytical angular resolution

\[ \Delta \Omega \approx \frac{c^{2}}{(f_0 \rho_{T})^{2} A_s(T)} \]

\[ A_s(T)= 2\pi \sqrt{\mathrm{Var}(r_\theta)\mathrm{Var}(r_\phi)-\mathrm{Cov}^2(r_\theta,r_\phi)} \]

  • \(f_0\) is the monochromatic signal’s frequency
  • \(\rho_T\) is the signal-to-noise ratio

Validating the expression

Trajectories and areas

References