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@Article{TedeschiCavaGrim:2016:ENInLa,
               author = "Tedeschi, Renata Gon{\c{c}}alves and Cavalcanti, Iracema Fonseca 
                         de Albuquerque and Grimm, Am",
          affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto 
                         Nacional de Pesquisas Espaciais (INPE)}",
                title = "ENSO influence on La Plata Basin precipitation in the HadGEM2-ES 
                         model",
              journal = "Climate Research",
                 year = "2016",
               volume = "68",
               number = "2/3",
                pages = "295--307",
                 note = "{Setores de Atividade: Pesquisa e desenvolvimento 
                         cient{\'{\i}}fico.}",
             keywords = "ENSO, ANOMALIAS DE PRECIPITACAO, extremos de 
                         precipita{\c{c}}{\~a}o, La Plata Basin, EL NINO, La Nina.",
             abstract = "ENSO episodes affect South American precipitation and the 
                         frequency of extreme precipitation events, mainly in the La Plata 
                         Basin (LPB). We analyzed the representation of Central and Eastern 
                         ENSO diversity in a historical simulation of the HadGEM2-ES model, 
                         and the results showed that this model does not reflect the ENSO 
                         diversity. However, the model does represent the frequency of 
                         Eastern ENSO. Therefore, we used this model to analyze the 
                         influences of this type of ENSO on precipitation and frequency of 
                         extreme precipitation events over the LPB in simulations 
                         (historical scenario) and projections (RCP8.5 scenario), during 
                         austral summer and autumn. The HadGEM2-ES model reproduced the 
                         anomalous precipitation dipole pattern (increased precipitation 
                         over southeastern South America and decreased precipitation over 
                         the north/northeast) in eastern El Niņo during both seasons, and 
                         the opposite pattern in eastern La Niņa during the austral autumn. 
                         The model reproduced the patterns of anomalous frequency of 
                         extreme events that occur over South America during both seasons 
                         of eastern El Niņo, but failed to reproduce these patterns during 
                         eastern La Niņa. The future projections showed patterns of 
                         anomalous precipitation and frequency of extreme events that were 
                         similar to those simulated for the present, but were more intense 
                         and affected a wider area.",
                  doi = "10.3354/cr01381",
                  url = "http://dx.doi.org/10.3354/cr01381",
                 issn = "0936-577X",
                label = "lattes: 6731029375224939 2 TedeschiCavaGrim:2016:ENInLa",
             language = "en",
        urlaccessdate = "28 nov. 2020"
}


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