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@InProceedings{SouzaSabaAlbr:2017:EsTeQu,
               author = "Souza, Jessica Cristina dos Santos and Saba, Marcelo 
                         Magalh{\~a}es Fares and Albrecht, Rachel Ifanger",
          affiliation = "{} and {Instituto Nacional de Pesquisas Espaciais (INPE)}",
                title = "Estudo das Tempestades que Geram Raios Ascendentes",
            booktitle = "Anais...",
                 year = "2017",
               editor = "Gherardi, Douglas Francisco Marcolino and Arag{\~a}o, Luiz 
                         Eduardo Oliveira e Cruz de",
                pages = "2799--2805",
         organization = "Simp{\'o}sio Brasileiro de Sensoriamento Remoto, 18. (SBSR)",
            publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
              address = "S{\~a}o Jos{\'e} dos Campos",
             abstract = "The study of induced lightnings are of great relevance because 
                         with the increasing of vertical cities, there may be a 
                         corresponding increase of upward lightning started from a tall 
                         structure connected to the ground toward cloud. Then, risks 
                         associated with these discharges should also be considered for the 
                         protection of persons and property. In this context, the objective 
                         of this study is to determine the characteristics of storms that 
                         generate upward lighting. From the data collected in 2012 until 
                         2016, it could be recorded 140 upward leaders that started from 
                         one of the towers located on Pico do Jaragu{\'a}, in S{\~a}o 
                         Paulo with the aid of a few ultra-fast cameras. For analysis of 
                         these discharges and corresponding storms, satellite imagery were 
                         collected and images of electromagnetic sources of lightning 
                         measured by SPLMA and LINET from January to march in 2012 and 
                         after by BrasilDAT and STARNET until june 2016 were generated. 
                         Besides that, images of reflectivity data from radar S{\~a}o 
                         Roque, FCTH and IACIT (CAPPI product) in the period of January and 
                         march 2012 that measured precipitation during the experiment 
                         CHUVA-GLM Vale do Para{\'{\i}}ba, from the radar S{\~a}o Roque 
                         (CAPPI product) from april 2012 to march 2015 and from radar FCTH 
                         (PPI product) from january 2014 to june 2016 were plotted. Based 
                         on analyzes of the horizontal structure and on the signature of 
                         the radar bright band, most of the precipitation could be 
                         categorized as stratiform, with reflectivity lower than 40 dBZ.",
  conference-location = "Santos",
      conference-year = "28-31 maio 2017",
                 isbn = "978-85-17-00088-1",
                label = "59832",
             language = "pt",
         organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                  ibi = "8JMKD3MGP6W34M/3PSLR9J",
                  url = "http://urlib.net/rep/8JMKD3MGP6W34M/3PSLR9J",
           targetfile = "59832.pdf",
                 type = "Meteorologia e climatologia",
        urlaccessdate = "24 nov. 2020"
}


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