Artículos de revistas
Reconstruction of the gravitational wave signal h(t) during the Virgo science runs and independent validation with a photon calibrator
Fecha
2014-08-21Registro en:
Classical And Quantum Gravity. Bristol: Iop Publishing Ltd, v. 31, n. 16, 30 p., 2014.
0264-9381
10.1088/0264-9381/31/16/165013
WOS:000341421600013
Autor
Univ Savoie
Complesso Univ Monte S Angelo
Univ Salerno
Nikhef
Ist Nazl Fis Nucl
Univ Siena
European Gravitat Observ
Univ Paris Diderot
Univ Pisa
CAMK PAN
Warsaw Univ
Univ Genoa
Univ Paris 11
Univ Nice Sophia Antipolis
Univ Rennes 1
Univ Lyon
Univ Urbino Carlo Bo
Univ Paris 06
Vrije Univ Amsterdam
Univ Naples Federico II
Univ Roma Tor Vergata
Univ Roma La Sapienza
Wigner RCP
Univ Trento
Univ Perugia
Radboud Univ Nijmegen
Bialystok Univ
IM PAN
NCBJ
CALTECH
CNRS
Univ Camerino
Inst Astron
Universidade Estadual Paulista (Unesp)
Institución
Resumen
The Virgo detector is a kilometer-scale interferometer for gravitational wave detection located near Pisa (Italy). About 13 months of data were accumulated during four science runs (VSR1, VSR2, VSR3 and VSR4) between May 2007 and September 2011, with increasing sensitivity. In this paper, the method used to reconstruct, in the range 10 Hz-10 kHz, the gravitational wave strain time series h(t) from the detector signals is described. The standard consistency checks of the reconstruction are discussed and used to estimate the systematic uncertainties of the h(t) signal as a function of frequency. Finally, an independent setup, the photon calibrator, is described and used to validate the reconstructed h(t) signal and the associated uncertainties. The systematic uncertainties of the h(t) time series are estimated to be 8% in amplitude. The uncertainty of the phase of h(t) is 50 mrad at 10 Hz with a frequency dependence following a delay of 8 mu s at high frequency. A bias lower than 4 mu s and depending on the sky direction of the GW is also present.