Systematic calibration error requirements for gravitational-wave detectors via the Cramér-Rao bound
arXiv:1712.09719 · doi:10.1088/1361-6382/ab368c
Abstract
Gravitational-wave (GW) laser interferometers such as Advanced LIGO transduce spacetime strain into optical power fluctuation. Converting this optical power fluctuations back into an estimated spacetime strain requires a calibration process that accounts for both the interferometer's optomechanical response and the feedback control loop used to control the interferometer test masses. Systematic errors in the calibration parameters lead to systematic errors in the GW strain estimate, and hence to systematic errors in the astrophysical parameter estimates in a particular GW signal. In this work we examine this effect for a GW signal similar to GW150914, both for a low-power detector operation similar to the first and second Advanced LIGO observing runs and for a higher-power operation with detuned signal extraction. We set requirements on the accuracy of the calibration such that the astrophysical parameter estimation is limited by errors introduced by random detector noise, rather than calibration systematics. We also examine the impact of systematic calibration errors on the possible detection of a massive graviton.
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Cited by in corpus (8)
- Characterization of systematic error in Advanced LIGO calibration
- Possible Causes of False General Relativity Violations in Gravitational Wave Observations
- Accumulating errors in tests of general relativity with gravitational waves: overlapping signals and inaccurate waveforms
- physiCal: A physical approach to the marginalization of LIGO calibration uncertainties
- An implementation of Galactic white dwarf binary data analysis for MLDC-3.1
- Impact of overlapping signals on parameterized post-Newtonian coefficients in tests of gravity
- Impact of calibration uncertainties on Hubble constant measurements from gravitational-wave sources
- Effects of calibration uncertainties on the detection and parameter estimation of isotropic gravitational-wave backgrounds