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@MastersThesis{Viana:2009:CoEsPr,
               author = "Viana, Denilson Ribeiro",
                title = "Comportamento espa{\c{c}}o-temporal da precipita{\c{c}}{\~a}o 
                         na Regi{\~a}o Sul do Brasil utilizando dados TRMM e SRTM",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2009",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2009-04-03",
             keywords = "precipita{\c{c}}{\~a}o, climatologia, variabilidade, 
                         tend{\^e}ncia geogr{\'a}fica, TRMM, rainfall, climatology, 
                         variability, geographic trend.",
             abstract = "Este trabalho investiga o comportamento espa{\c{c}}o-temporal da 
                         precipita{\c{c}}{\~a}o pluvial na Regi{\~a}o Sul do Brasil 
                         entre 1988 e 2007. A avalia{\c{c}}{\~a}o concentrou-se em 
                         tr{\^e}s aspectos: 1) principais caracter{\'{\i}}sticas 
                         climatol{\'o}gicas, 2) tend{\^e}ncia geogr{\'a}fica, com base 
                         nas fei{\c{c}}{\~o}es do relevo, e 3) principais modos de 
                         variabilidade. Foram utilizados dois conjuntos complementares de 
                         dados de precipita{\c{c}}{\~a}o: postos pluviom{\'e}tricos e 
                         estimativas de precipita{\c{c}}{\~a}o do sat{\'e}lite Tropical 
                         Rainfall Measuring Mission (TRMM), produto 3B43. A 
                         avalia{\c{c}}{\~a}o das fei{\c{c}}{\~o}es do relevo foi 
                         conduzida com o aux{\'{\i}}lio do Modelo Digital de 
                         Eleva{\c{c}}{\~a}o (MDE) oriundo do Shuttle Radar Topography 
                         Mission (SRTM), a partir do qual foram identificadas tr{\^e}s 
                         sub-regi{\~o}es: 1) Litoral, 2) Campanha e 3) Planalto. As 
                         caracter{\'{\i}}sticas climatol{\'o}gicas da 
                         precipita{\c{c}}{\~a}o foram avaliadas atrav{\'e}s de 
                         estat{\'{\i}}sticas descritivas (m{\'e}dia e desvio 
                         padr{\~a}o) sazonal e anual. A an{\'a}lise de tend{\^e}ncia 
                         geogr{\'a}fica foi realizada para cada sub-regi{\~a}o 
                         identificada atrav{\'e}s de regress{\~a}o linear m{\'u}ltipla 
                         da precipita{\c{c}}{\~a}o em rela{\c{c}}{\~a}o {\`a}s suas 
                         coordenadas (latitude e longitude). A variabilidade da 
                         precipita{\c{c}}{\~a}o foi avaliada por meio de 
                         Fun{\c{c}}{\~o}es Ortogonais Emp{\'{\i}}ricas (EOF), enquanto 
                         os sistemas atmosf{\'e}ricos respons{\'a}veis pelos principais 
                         modos de EOF foram investigados a partir dos boletins 
                         Climan{\'a}lise. Os resultados da climatologia, quando comparados 
                         a estudos anteriores, apontam uma diminui{\c{c}}{\~a}o da 
                         participa{\c{c}}{\~a}o da precipita{\c{c}}{\~a}o de inverno na 
                         regi{\~a}o, e um aumento nas esta{\c{c}}{\~o}es de 
                         transi{\c{c}}{\~a}o, especialmente na primavera. Os desvios em 
                         rela{\c{c}}{\~a}o {\`a} m{\'e}dia variaram entre 40% e 70%. A 
                         tend{\^e}ncia geogr{\'a}fica da precipita{\c{c}}{\~a}o foi 
                         mais expressiva na metade quente do ano no Litoral, em 
                         fun{\c{c}}{\~a}o da Zona de Converg{\^e}ncia do Atl{\^a}ntico 
                         Sul (ZCAS) e de precipita{\c{c}}{\~o}es orogr{\'a}ficas. Nos 
                         meses frios, a tend{\^e}ncia foi mais pronunciada na Campanha 
                         devido aos sistemas frontais e ciclones extratropicais. No 
                         Planalto, a tend{\^e}ncia mostrou-se moderada no ver{\~a}o 
                         devido a ZCAS; e no outono, por conta da atua{\c{c}}{\~a}o dos 
                         sistemas frontais e ciclones extratropicais. Os principais modos 
                         de variabilidade da precipita{\c{c}}{\~a}o t{\^e}m como causas 
                         distintos sistemas. No inverno, destaca-se a atua{\c{c}}{\~a}o 
                         de sistemas frontais semi-estacion{\'a}rios, favorecidos por 
                         epis{\'o}dios de bloqueios atmosf{\'e}ricos. No inverno e 
                         esta{\c{c}}{\~o}es de transi{\c{c}}{\~a}o, destaca-se a 
                         atua{\c{c}}{\~a}o dos ciclones extratropicais, em geral em 
                         associa{\c{c}}{\~a}o com sistemas frontais. Nos meses quentes, 
                         os Complexos Convectivos de Mesoescala s{\~a}o os principais 
                         respons{\'a}veis pela variabilidade observada. ABSTRACT: This 
                         work investigates the space-temporal behavior of rainfall in 
                         Southern Brazil during the 1988 and 2007 period. The evaluation 
                         was based on three features: 1) climatological aspects, 2) 
                         geographic trends from relief features, and 3) main variability 
                         modes. Two complementary data sets of rainfall were used: rain 
                         gauges and rainfall estimates from the Tropical Rainfall Measuring 
                         Mission (TRMM), product 3B43. The assessment of relief features 
                         was made using the Digital Elevation Model (MDE) from Shuttle 
                         Radar Topography Mission (SRTM), where three sub regions were 
                         identified: 1) Litoral (seacoast), 2) Campanha (countryside), and 
                         3) Planalto (plateau). The rainfall climatological features were 
                         evaluated using basic statistics parameters. The trend geographic 
                         analysis was made for each sub region identified by multiple 
                         linear regression of rainfall versus their coordinates (latitude 
                         and longitude). The rainfall variability was evaluated by 
                         Empirical Orthogonal Functions (EOF), while the weather systems 
                         analysis associated with the EOF modes were based on 
                         Climan{\'a}lise, from INPE/CPTEC. The climatological analysis 
                         show that rainfall amount is decreasing during the southern winter 
                         period, but it is increasing in the transition seasons, mainly in 
                         the southern spring. The standard deviations from the average were 
                         between 40% and 70%. The rainfall trend was most expressive in the 
                         warmest half of the year in Litoral sub region, because of South 
                         Atlantic Convergence Zone (ZCAS) and orographic precipitation. In 
                         the coldest months, the trend was more pronounced in Campanha due 
                         to frontal systems and extratropical cyclones. In the Planalto sub 
                         region, the trend was moderate in the summer due to ZCAS location, 
                         and in the autumn due to frontal systems and extratropical 
                         cyclones. The main modes of the observed rainfall variability in 
                         Southern Brazil have different causes. In the winter, the action 
                         of semi-stationary frontal systems was favored by blocking 
                         episodes. Also in the winter and transitions seasons, 
                         extratropical cyclones in association with frontal systems play an 
                         important role to the observed rainfall amount. In the warmest 
                         months, Mesoscale Convective Complexes was mainly responsible for 
                         the observed variability in the period.",
            committee = "Valeriano, M{\'a}rcio de Morisson (presidente) and Ferreira, 
                         Nelson Jesus (orientador) and Conforte, Jorge Conrado (orientador) 
                         and Sansigolo, Cl{\'o}vis Angeli and Silva, Maria Elisa 
                         Siqueira",
           copyholder = "SID/SCD",
         englishtitle = "Space-temporal behavior of rainfall in Southern Brazil using TRMM 
                         and SRTM data",
             language = "pt",
                pages = "162",
                  ibi = "8JMKD3MGP8W/359H9BE",
                  url = "http://urlib.net/ibi/8JMKD3MGP8W/359H9BE",
           targetfile = "publicacao.pdf",
        urlaccessdate = "16 jun. 2024"
}


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