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@Article{LeiZMHYLDSYLB:2016:CoBeF2,
               author = "Lei, Jiuhou and Zhong, Jiahao and Mao, Tian and Hu, Lianhuan and 
                         Yu, Tao and Luan, Xiaoli and Dou, Xiankang and Sutton, Eric and 
                         Yue, Xinan and Lin, Jian and Batista, Inez Staciarini",
          affiliation = "{University of Science and Technology of China} and {University of 
                         Science and Technology of China} and {China Meteorological 
                         Administration} and {Chinese Academy of Sciences} and {China 
                         University of Geosciences} and {University of Science and 
                         Technology of China} and {University of Science and Technology of 
                         China} and {Air Force Research Laboratory} and {Chinese Academy of 
                         Sciences} and {China Earthquake Administration} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)}",
                title = "Contrasting behavior of the F2 peak and the topside ionosphere in 
                         response to the 2 October 2013 geomagnetic storm",
              journal = "Journal of Geophysical Research: Space Physics",
                 year = "2016",
               volume = "121",
               number = "10",
                pages = "1--15",
                 note = "{Setores de Atividade: Pesquisa e desenvolvimento 
                         cient{\'{\i}}fico.}",
             keywords = "ionosfera, digissonda, camada F.",
             abstract = "In this study, the ionospheric observations from ionosondes, 
                         ground-based GPS receivers, Gravity Recovery and Climate 
                         Experiment (GRACE) and MetOp-A satellites, and Fabry-Perot 
                         interferometer over the Asian-Australian sector have been used to 
                         investigate the responses of the F2 peak and the topside 
                         ionosphere to the 2 October 2013 geomagnetic storm, particularly 
                         during the recovery phase. The comparison between the multiple 
                         simultaneous observations revealed a contrasting behavior of the 
                         topside ionosphere and the F2 peak in East Asia during the 
                         recovery phase. The upward looking total electron content from 
                         low-Earth orbit (LEO) satellites did not undergo such depletions 
                         as seen in the region near the F2 peak, and they even showed 
                         increases. Furthermore, the simulation results of the Thermosphere 
                         Ionosphere Electrodynamics General Circulation Model are used to 
                         explore the possible mechanisms responsible for the observed 
                         features. The model results and observations suggested that the 
                         contrasting behavior of the F2 peak and the topside ionosphere is 
                         mainly associated with the enhancement of the equatorward winds, 
                         albeit the disturbed electric fields could play an important role 
                         in producing it.",
                  doi = "10.1002/2016JA022959",
                  url = "http://dx.doi.org/10.1002/2016JA022959",
                 issn = "2169-9402",
                label = "lattes: 4091433441104332 11 LeiZMHYLDSYLB:2016:CoBeF2",
             language = "en",
           targetfile = "lei_contrasting.pdf",
        urlaccessdate = "23 nov. 2020"
}


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