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@Article{OliveiraMaPiXaFrMaAg:2010:SeMoSi,
               author = "Oliveira, F. G. and Marinho Jr., R. M. and Pires, R. and Xavier, 
                         V. S. and Frajuca, C. and Magalhaes, N. S. and Aguiar, Odylio 
                         Denys",
          affiliation = "{Instituto Tecnol{\'o}gico de Aeron{\'a}utica (ITA)} and 
                         {Instituto Tecnol{\'o}gico de Aeron{\'a}utica (ITA)} and 
                         Instituto Federal de Educa{\c{c}}{\~a}o, Ci{\^e}ncia e 
                         Tecnologia de S{\~a}o Paulo and Instituto Federal de 
                         Educa{\c{c}}{\~a}o, Ci{\^e}ncia e Tecnologia de S{\~a}o Paulo 
                         and Instituto Federal de Educa{\c{c}}{\~a}o, Ci{\^e}ncia e 
                         Tecnologia de S{\~a}o Paulo and {Universidade Federal de S{\~a}o 
                         Paulo (UNIFESP)} and {Instituto Nacional de Pesquisas Espaciais 
                         (INPE)}",
                title = "Search for monochromatic signals using data from the allegro 
                         gravitational wave detector",
              journal = "International Journal of Modern Physics D",
                 year = "2010",
               volume = "19",
               number = "8-10",
                pages = "1293--1297",
                month = "Aug.",
                 note = "{Proceedings Paper}",
             keywords = "Gravitational waves, Doppler shift, data analysis, 
                         FOURIER-TRANSFORM.",
             abstract = "We present a data analysis method for searching monochromatic 
                         signals in temporal series. With this method it is possible to 
                         estimate the power spectrum by using averaged modified 
                         periodograms which reinforce the presence of peaks due to 
                         monochromatic signals. In particular we use ALLEGRO's 
                         gravitational wave data for the year 1999 taking into account the 
                         effect due to the orbital motion of the Earth. We tested the 
                         method injecting a simulated signal in real data and we were able 
                         to detect it. Then we seeked for candidate signals within the 
                         noise but nothing was found. The method showed useful for 
                         applications in the search for continuous gravitational waves.",
                  doi = "10.1142/S0218271810017305",
                  url = "http://dx.doi.org/10.1142/S0218271810017305",
                 issn = "0218-2718",
             language = "en",
           targetfile = "oliveira_search.pdf",
        urlaccessdate = "25 jan. 2021"
}


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