@InProceedings{OliveiraOyam:2010:VaEnPo,
               author = "Oliveira, Fernando Pereira de and Oyama, Marcos Daisuke",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         de Aeron{\'a}utica e Espa{\c{c}}o - IAE}",
                title = "Varia{\c{c}}{\~a}o da Energia Potencial Dispon{\'{\i}}vel para 
                         Convec{\c{c}}{\~a}o e do {\'{\I}}ndice de Levantamento para o 
                         Centro de Lan{\c{c}}amento de Alc{\^a}ntara em 
                         Rela{\c{c}}{\~a}o ao N{\'{\i}}vel Inicial de Ascens{\~a}o",
            booktitle = "Anais...",
                 year = "2010",
         organization = "Congresso Brasileiro de Meteorologia (CBMET), 16.",
            publisher = "SBMET",
              address = "Rio de Janeiro",
                 note = "http://www.cbmet2010.com/anais/",
             keywords = "Par{\^a}metros Convectivos, Instabilidade Atmosf{\'e}rica, CAPE, 
                         ILEV, Convective Parameters, Atmospheric Instability.",
             abstract = "Variation of Convective Available Potential Energy and Lifted 
                         Index over the Alc{\^a}ntara Launch Center with respect to the 
                         Initial Level of Parcel Ascent In this work the variation of 
                         Convective Available Potential Energy (CAPE) and Lifted Index 
                         (ILEV) over the Alc{\^a}ntara Launch Center, located at the 
                         northern coast of Brazil, with respect to the initial level of 
                         parcel ascent were evaluated in order to verify whether a 
                         different level of ascent would become the parameters cycle more 
                         consistent to the precipitation cycle. Radiosouding data from 1989 
                         to 2008 at 1200 UTC were used. The saturated pseudoadiabatic 
                         ascent was based on the equivalent potential temperature 
                         conservation. The results show that the change of the initial 
                         level of parcel ascent does not make CAPE annual cycle similar to 
                         the precipitation cycle. ILEV annual cycle became more consistent 
                         to the precipitation cycle for a parcel that ascended from a level 
                         between 950 and 800 hPa.",
  conference-location = "Bel{\'e}m",
      conference-year = "2010",
                label = "lattes: 0953985585184181 1 OliveiraOyam:2010:VaEnPo",
             language = "pt",
           targetfile = "775_69671.pdf",
        urlaccessdate = "30 jun. 2024"
}