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@InProceedings{ResendeBaDeCaAnCh:2015:StBlSp,
               author = "Resende, Laysa Cristina Ara{\'u}jo and Batista, Inez Staciarini 
                         and Denardini, Clezio Marcos and Carrasco, Jos{\'e} Alexander and 
                         Andrioli, V{\^a}nia de F{\'a}tima and Chen, Sony Su",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de 
                         Pesquisas Espaciais (INPE)} and {University of Los Andes} and 
                         {Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)}",
                title = "Study of the blanketing sporadic layer formation considering the 
                         influence of the tidal winds",
                 year = "2015",
         organization = "IUGG General Assembly, 26.",
             abstract = "This work presents a study about the formation of blanketing 
                         sporadic E-layers, Esb, considering the tidal winds for two 
                         Brazilian ionospheric regions: S{\~a}o Lu{\'{\i}}s, a quasi- 
                         equatorial station, and Cachoeira Paulista, located at low 
                         latitude. For this study we have used a theoretical model for the 
                         E region, called MIRE, that calculate the densities for the main 
                         molecular (NO+, O2+, N2+ ) and metallic ions (Fe+, Mg+) by solving 
                         the continuity and momentum equations for each one of these 
                         species. Therefore, it was possible to simulate the dynamics of 
                         Esb layers under the action of tidal winds. Afterwards, the Es 
                         layer blanketing frequency parameter (fbEs) was obtained from 
                         ionograms in order to compare the evolution of the Esb layer with 
                         the model results. The analysis shows that the Es layer parameters 
                         computed using the tidal winds in the improved MIRE have a good 
                         agreement with the observed fbEs parameter, mainly for Cachoeira 
                         Paulista. Lastly, the comparison has interesting results that it 
                         becomes possible to better understand the Es layer formation 
                         mechanisms in the Brazilian sector.",
  conference-location = "Prague, Czech Republic",
      conference-year = "22 June - 02 July",
        urlaccessdate = "28 mar. 2024"
}


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