@Article{TakahashiLWBOABA:2012:IoRe2d,
               author = "Takahashi, Hisao and Lima, L M and Wrasse, C M and Batista, Inez 
                         Staciarini and Onohara, Amelia Naomi and Aquino, Maria Goreti dos 
                         Santos and Batista, Paulo Prado and Abdu, Mangalathayil A.",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and 
                         Universidade estadual de Paraiba, Campina Grande, PB, Brazil and 
                         Instituto de pesquisa Vale, S{\~a}o Jos{\'e} dos Campos, Brazil 
                         and {Instituto Nacional de Pesquisas Espaciais (INPE)} and 
                         {Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de 
                         Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas 
                         Espaciais (INPE)}",
                title = "Ionospheric response to 2-day planetary wave in the equatorial and 
                         low latitude regions",
              journal = "Journal of Atmospheric and Solar-Terrestrial Physics",
                 year = "2012",
               volume = "xx",
               number = "in press",
                pages = "1--8",
             keywords = "Ionosphere, 2-day planetary wave, EIA.",
             abstract = "Planetary scale 2-day waves in the mesospherelower thermosphere 
                         winds have been observed mainly from January to February in the 
                         southern hemisphere low latitude region. Meteor radar wind 
                         measurements at Cariri (7.41S, 36.51W) from the year 2005 to 2007 
                         showed a distinct 2-day oscillation in the meridional winds with 
                         the amplitude of 5080 m/s and 2030 m/s for the zonal winds. During 
                         the same period, the ionospheric F-layer maximum critical 
                         frequency (foF2) observed at Fortaleza (3.81S, 38.61W) also showed 
                         distinct 2-day oscillation, indicating in\fluence of 
                         planetary 2-day wave in the ionosphere. On the other hand, no 
                         clear signature of 2-day oscillation was observed for the F-layer 
                         bottom-side virtual height (hF). Present results suggest that the 
                         2-day wave induced meridional wind in the thermosphere could 
                         generate latitudinal transport of F-region plasma causing day to 
                         day variability of equatorial ionization anomaly (EIA).",
                  doi = "10.1016/j.jastp.2012.04.006",
                  url = "http://dx.doi.org/10.1016/j.jastp.2012.04.006",
                 issn = "1364-6826",
             language = "en",
        urlaccessdate = "30 abr. 2024"
}