@InProceedings{SanchezJuarez:2023:RaDeOb,
               author = "Sanchez Juarez, Sa{\'u}l Alejandro",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "Rapid detection observation and simulation of co-seismic 
                         ionospheric disturbances",
            booktitle = "Resumos...",
                 year = "2023",
               editor = "Santos, Rafael Duarte Coelho dos and Calheiros, Alan James Peixoto 
                         and J{\'u}nior, Valdivino Alexandre de Santiago",
         organization = "Workshop dos Cursos de Computa{\c{c}}{\~a}o Aplicada do INPE, 
                         22. (WORCAP)",
            publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
             abstract = "Co-seismic Ionospheric disturbances (CID, or {"}ionoquakes{"}) are 
                         disturbances in the electron density or total electron content 
                         (TEC) of the ionosphere, produced by the ground motion due to 
                         earthquakes. Usually, ionoquakes are detected in the 
                         near-epicentral region within 8-10 minutes after an earthquake 
                         onset time. In this work, we present a new methodology that allows 
                         to estimate the ionoquakes arrival time based on determining the 
                         ionoquakes peak time in TEC measurements with respect to the peak 
                         time of seismic waves registered by the nearest seismic station. 
                         Our methodology also allows to understand the altitude of GNSS 
                         detection that otherwise remains ambiguous. We apply the newly 
                         developed techniques to detect ionoquakes signatures associated 
                         with large earthquakes. We show that for the analyzed earthquakes, 
                         the ionoquakes arrive 250-430 seconds after the time of the 
                         seismic wave peak, or 350-700 s after the earthquake onset time. 
                         Our analysis shows that the first ionoquakes are detected at the 
                         altitudes of 150-300 km.",
  conference-location = "S{\~a}o Jos{\'e} dos Campos",
      conference-year = "11-15 set. 2023",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "8JMKD3MGPDW34P/4A4HKN8",
                  url = "http://urlib.net/ibi/8JMKD3MGPDW34P/4A4HKN8",
           targetfile = "Sanchez_rapid.pdf",
        urlaccessdate = "21 maio 2024"
}