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@PhDThesis{ObregónPárraga:2003:DiVaCl,
               author = "Obreg{\'o}n P{\'a}rraga, Guillermo Oswaldo",
                title = "Din{\^a}mica da variabibilidade clim{\'a}tica da 
                         precipita{\c{c}}{\~a}o sobre a Am{\'e}rica do Sul",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2003",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2001-03-27",
             keywords = "variabilidade clim{\'a}tica, an{\'a}lise estat{\'{\i}}stica, 
                         precipita{\c{c}}{\~a}o, mudan{\c{c}}a clim{\'a}tica.",
             abstract = "A variabilidade clim{\'a}tica da precipita{\c{c}}{\~a}o em 
                         escalas intrasazonais, sobre o Brasil, e escalas interanual e 
                         per{\'{\i}}odos maiores sobre a Am{\'e}rica do Sul foram 
                         estudadas atrav{\'e}s da utiliza{\c{c}}{\~a}o de dados de 
                         precipita{\c{c}}{\~a}o di{\'a}ria (1979-1990) e mensal 
                         (1951-1990) utilizando diversos m{\'e}todos 
                         estat{\'{\i}}sticos. Os resultados obtidos mostram que a 
                         variabilidade da precipita{\c{c}}{\~a}o sobre a AS, em escalas 
                         sazonal e interanual apresenta caracter{\'{\i}}sticas regionais 
                         intr{\'{\i}}nsecas, com ciclo anual proeminente e persistente 
                         sobre a maior parte do dom{\'{\i}}nio. O ciclo semi-anual {\'e} 
                         predominante principalmente sobre o norte da Amaz{\^o}nia, com 
                         alta persist{\^e}ncia, e sul do Brasil com baixa 
                         persist{\^e}ncia. A distribui{\c{c}}{\~a}o sazonal da 
                         precipita{\c{c}}{\~a}o m{\'e}dia e as estat{\'{\i}}sticas 
                         probabil{\'{\i}}sticas est{\~a}o intensamente relacionadas 
                         durante todas as esta{\c{c}}{\~o}es do ano. Com 
                         rela{\c{c}}{\~a}o {\`a} variabilidade intrasazonal sobre o 
                         Brasil foi encontrado o predom{\'{\i}}nio de 
                         oscila{\c{c}}{\~o}es com per{\'{\i}}odo de 20 e 40 dias, com 
                         caracter{\'{\i}}sticas distintas. A oscila{\c{c}}{\~a}o de 20 
                         dias aparentemente mostra maior depend{\^e}ncia das ondas 
                         barocl{\'{\i}}nicas, enquanto que a de 40 dias parece mais 
                         relacionada com oscila{\c{c}}{\~o}es de escala global e, 
                         possivelmente, interage com maior intensidade com a atmosfera 
                         tropical. Quanto {\`a} variabilidade interanual nota-se que a 
                         precipita{\c{c}}{\~a}o sobre a Am{\'e}rica do Sul {\'e} 
                         modulada pelo El Niño/Oscila{\c{c}}{\~a}o Sul (ENOS), por{\'e}m 
                         esta modula{\c{c}}{\~a}o aparece em dois per{\'{\i}}odos 
                         distintos, de 3,7 e 5 anos. A oscila{\c{c}}{\~a}o de 5 anos tem 
                         predom{\'{\i}}nio sobre as regi{\~o}es equatoriais enquanto que 
                         a oscila{\c{c}}{\~a}o de 3,7 anos tem maior influ{\^e}ncia 
                         sobre o sul do Brasil, ambas moduladas pelo Atl{\^a}ntico 
                         tropical, por{\'e}m com intensidades diferentes. A tend{\^e}ncia 
                         linear e mudan{\c{c}}a clim{\'a}tica sobre a AS apresentam uma 
                         distribui{\c{c}}{\~a}o espa{\c{c}}o-temporal coerentes entre 
                         si. Observou-se tend{\^e}ncia linear negativa da 
                         precipita{\c{c}}{\~a}o anual sobre a faixa de m{\'a}xima 
                         precipita{\c{c}}{\~a}o, associada com a Zona de 
                         Converg{\^e}ncia do Atl{\^a}ntico Sul (ZCAS), e tend{\^e}ncia 
                         positiva sobre o sul do Brasil. Estes padr{\~o}es s{\~a}o 
                         resultado das tend{\^e}ncias negativas intensas concentradas 
                         durante as esta{\c{c}}{\~o}es de ver{\~a}o, na faixa de 
                         m{\'a}xima precipita{\c{c}}{\~a}o, e no sul do Brasil na 
                         primavera. Ambas as tend{\^e}ncias parecem estar associadas 
                         {\`a} mudan{\c{c}}a clim{\'a}tica abrupta observada na metade 
                         da d{\'e}cada de 70, relacionada {\`a} mudan{\c{c}}a da 
                         temperatura superficial do mar (TSM) dos oceanos, principalmente 
                         do Oceano Pac{\'{\i}}fico. Esta mudan{\c{c}}a clim{\'a}tica 
                         abrupta teve repercuss{\~o}es sobre quase toda a Am{\'e}rica do 
                         Sul, com exce{\c{c}}{\~a}o do Nordeste do Brasil, onde a 
                         precipita{\c{c}}{\~a}o apresenta alta variabilidade interanual e 
                         aparente variabilidade quase decadal. ABSTRACT: Intraseasonal 
                         time-scales of climate variability over Brazil, and interannual 
                         and larger time-scales climate variability over South America were 
                         studied using daily (1979- 1990) and monthly (1951-1990) mean 
                         rainfall data and several statistical methods. The results show 
                         that the seasonal and interannual rainfall variability over South 
                         America have intrinsic regional features with prominent and 
                         persistent annual cycle. The semiannual cycle is predominant over 
                         northern Amazon (high persistence) and Southern Brazil (low 
                         persistence). The seasonal mean rainfall distribution is strongly 
                         related to the statistics of probabilities in all seasons. With 
                         respect to intraseasonal variability over Brazil, it was found 
                         that there are two dominant oscillations with periods of 20 and 40 
                         days with distinct characteristics. The 20 day oscillation shows 
                         greater dependence on baroclinic waves, while the 40 day seems to 
                         be more related to the global scale oscillations and apparently 
                         interacts with greater intensity with the tropical atmosphere. 
                         Regarding the interannual variability, it is observed that 
                         precipitation over South America is modulated by El Niño/South 
                         Oscillation (ENSO). However, this modulation is present in the 
                         distinct periods, 3.7 and 5 years. The 5 years oscillation is 
                         predominant over equatorial regions, while the 3.7 years 
                         oscillation is predominant over Southern Brazil. Both are 
                         modulated by Tropical Atlantic, but with different intensities. 
                         The linear trends and climate change over South America show 
                         coherent space-temporal distributions. Negative trends of the 
                         annual precipitation over the maximum rainfall area, related to 
                         the climatological region of the South Atlantic Convergence Zone 
                         (SACZ), and positive trends over Southern Brazil were observed. 
                         These patterns are results of the intense negative tendency 
                         occurred in summer over the maximum rainfall area and during 
                         spring season over Southern Brazil. The trends seem to be 
                         associated with the observed climate change in the mid 70?s, which 
                         is related to the sea surface temperature change, mainly in the 
                         Pacific Ocean. This abrupt climate change affected almost the 
                         whole South America, except Northeast Brazil, where precipitation 
                         shows high interannual variability and apparent quasi-decadal 
                         variability.",
            committee = "Rao, Vadlamudi Brahmananda (presidente) and Nobre, Carlos Afonso 
                         (orientador) and Cavalcanti, Iracema Fonseca de Albuquerque and 
                         Ambrizzi, T{\'e}rcio and Morettin, Pedro Alberto",
           copyholder = "SID/SCD",
         englishtitle = "Rainfall climate variability dynamics over South America",
             language = "pt",
                  ibi = "6qtX3pFwXQZsFDuKxG/xxtn8",
                  url = "http://urlib.net/ibi/6qtX3pFwXQZsFDuKxG/xxtn8",
           targetfile = "publicacao.pdf",
        urlaccessdate = "14 maio 2024"
}


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