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Published November 15, 2019 | Published + Accepted Version
Journal Article Open

Noise spectral estimation methods and their impact on gravitational wave measurement of compact binary mergers

Abstract

Estimating the parameters of gravitational wave signals detected by ground-based detectors requires an understanding of the properties of the detectors' noise. In particular, the most commonly used likelihood function for gravitational wave data analysis assumes that the noise is Gaussian, stationary, and of known frequency-dependent variance. The variance of the colored Gaussian noise is used as a whitening filter on the data before computation of the likelihood function. In practice the noise variance is not known and it evolves over timescales of dozens of seconds to minutes. We study two methods for estimating this whitening filter for ground-based gravitational wave detectors with the goal of performing parameter estimation studies. The first method uses large amounts of data separated from the specific segment we wish to analyze and computes the power spectral density of the noise through the mean-median Welch method. The second method uses the same data segment as the parameter estimation analysis, which potentially includes a gravitational wave signal, and obtains the whitening filter through a fit of the power spectrum of the data in terms of a sum of splines and Lorentzians. We compare these two methods and conclude that the latter is a more effective spectral estimation method as it is quantitatively consistent with the statistics of the data used for gravitational wave parameter estimation while the former is not. We demonstrate the effect of the two methods by finding quantitative differences in the inferences made about the physical properties of simulated gravitational wave sources added to LIGO-Virgo data.

Additional Information

© 2019 American Physical Society. Received 15 July 2019; published 5 November 2019. We thank Max Isi for comments on the manuscript. This research has made use of data, software and/or web tools obtained from the Gravitational Wave Open Science Center, a service of LIGO Laboratory, the LIGO Scientific Collaboration and the Virgo Collaboration. LIGO is funded by the U.S. National Science Foundation (NSF). Virgo is funded by the French Centre National de Recherche Scientifique (CNRS), the Italian Istituto Nazionale della Fisica Nucleare (INFN), and the Dutch Nikhef, with contributions by Polish and Hungarian institutes. The authors are grateful for computational resources provided by the LIGO Laboratory and supported by National Science Foundation Grants No. PHY-0757058 and No. PHY-0823459, and for resources provided by the Open Science Grid [47,48], which is supported by the National Science Foundation Grant No. 1148698, and the U.S. Department of Energy's Office of Science. The Flatiron Institute is supported by the Simons Foundation. C.-J. H. acknowledges support of the MIT physics department and the LIGO Laboratory, which is operated under Grant No. PHY-1764464 from the National Science Foundation. S. G. acknowledges support from NSF Grant No. PHY-1809572. J. A. Clark acknowledges support from NSF Grant No. OAC-1841479 and No. PHY-1700765. N. C. acknowledges support from NSF Grant No. PHY-1607343. Parts of this research were conducted by the Australian Research Council Centre of Excellence for Gravitational Wave Discovery (OzGrav), through Grant No. CE170100004. Plots in this manuscript have been made with matplotlib [49].

Attached Files

Published - PhysRevD.100.104004.pdf

Accepted Version - 1907.06540.pdf

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Additional details

Created:
August 19, 2023
Modified:
October 20, 2023