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@PhDThesis{Santos:2021:PaAtVa,
               author = "Santos, Luiz Fernando dos",
                title = "Padr{\~o}es atmosf{\'e}ricos e variabilidade interanual do 
                         in{\'{\i}}cio da esta{\c{c}}{\~a}o chuvosa nas regi{\~o}es 
                         Centro-Oeste e Sudeste do Brasil",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2021",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2020-12-18",
             keywords = "mon{\c{c}}{\~a}o da Am{\'e}rica do Sul, 
                         precipita{\c{c}}{\~a}o, circula{\c{c}}{\~a}o atmosf{\'e}rica, 
                         fluxo de calor, ondas tropicais, South American monsoon, 
                         precipitation, atmospheric circulation, heat flux, tropical 
                         waves.",
             abstract = "O presente estudo investiga o comportamento do escoamento 
                         atmosf{\'e}rico, de altos e baixos n{\'{\i}}veis, desde os 
                         momentos que antecedem at{\'e} a data de in{\'{\i}}cio da 
                         esta{\c{c}}{\~a}o chuvosa nas regi{\~o}es Centro-Oeste e 
                         Sudeste do Brasil. Vale ressaltar que este tipo de an{\'a}lise 
                         {\'e} poss{\'{\i}}vel devido ao fato de ambas as regi{\~o}es 
                         estarem inseridas no Sistema de Mon{\c{c}}{\~a}o da Am{\'e}rica 
                         do Sul, na qual apresenta uma esta{\c{c}}{\~a}o seca e uma 
                         esta{\c{c}}{\~a}o {\'u}mida bem definidas. Al{\'e}m disso, 
                         foram analisadas tamb{\'e}m as convers{\~o}es de energia 
                         cin{\'e}tica entre os dist{\'u}rbios de v{\'a}rias escalas de 
                         tempo e a atua{\c{c}}{\~a}o de oscila{\c{c}}{\~o}es 
                         atmosf{\'e}ricas que interagem com a circula{\c{c}}{\~a}o na 
                         Am{\'e}rica do Sul durante este per{\'{\i}}odo. A partir da 
                         metodologia utilizada, as datas de in{\'{\i}}cio da 
                         esta{\c{c}}{\~a}o chuvosa foram obtidas com base nos dados 
                         di{\'a}rios de precipita{\c{c}}{\~a}o do Climate Prediction 
                         Center em um per{\'{\i}}odo de 39 anos (1979-2017) para ambas as 
                         regi{\~o}es. As datas foram separadas em tr{\^e}s categorias 
                         (precoce, m{\'e}dia e tardia) e, com os dados da rean{\'a}lise 
                         do Climate Forecast System Reanalysis e do Climate Forecast System 
                         version 2 investigouse os padr{\~o}es din{\^a}micos e 
                         f{\'{\i}}sicos da atmosfera e de superf{\'{\i}}cie durante o 
                         in{\'{\i}}cio da esta{\c{c}}{\~a}o chuvosa nessas categorias. 
                         A intera{\c{c}}{\~a}o entre as escalas sin{\'o}tica (2- 6 
                         dias), submensal (7-29 dias) e intrassazonal (30-90 dias) 
                         tamb{\'e}m foram investigadas, tal como os termos de 
                         convers{\~a}o de energia cin{\'e}tica nessas escalas sobre a 
                         Am{\'e}rica do Sul no trimestre de setembro a novembro. Dois 
                         n{\'u}cleos de precipita{\c{c}}{\~a}o mais intensa foram 
                         notados antes da data de in{\'{\i}}cio da esta{\c{c}}{\~a}o 
                         chuvosa de ambas as regi{\~o}es de estudo. Tais n{\'u}cleos 
                         ficam localizados a noroeste e sul do Brasil, os quais se conectam 
                         durante o in{\'{\i}}cio da esta{\c{c}}{\~a}o chuvosa, elevando 
                         abruptamente a precipita{\c{c}}{\~a}o no Sudeste e, 
                         principalmente, no Centro-Oeste. Neste mesmo per{\'{\i}}odo, 
                         observou-se tamb{\'e}m a conex{\~a}o entre a c{\'e}lula de 
                         circula{\c{c}}{\~a}o meridional Hadley, de car{\'a}ter 
                         regional, e a circula{\c{c}}{\~a}o de brisa de maior escala, que 
                         atua zonalmente, nas duas regi{\~o}es estudadas. Normalmente, o 
                         fluxo de calor sens{\'{\i}}vel se mostra superior ao fluxo de 
                         calor latente antes da data de in{\'{\i}}cio da 
                         esta{\c{c}}{\~a}o chuvosa na categoria precoce de ambas as 
                         regi{\~o}es, j{\'a} na categoria tardia o fluxo de calor latente 
                         mostrou-se mais intenso durante todo o per{\'{\i}}odo analisado. 
                         As intera{\c{c}}{\~o}es de escalas mostram 
                         combina{\c{c}}{\~o}es din{\^a}micas peculiares em cada 
                         categoria que contribuem para o in{\'{\i}}cio da 
                         esta{\c{c}}{\~a}o chuvosa. Notou-se ainda que h{\'a} um 
                         relativo equil{\'{\i}}brio entre o termo de converg{\^e}ncia do 
                         fluxo ageostr{\'o}fico com a convers{\~a}o barocl{\'{\i}}nica 
                         no balan{\c{c}}o da energia cin{\'e}tica dos dist{\'u}rbios 
                         sobre a Am{\'e}rica do Sul, tais termos s{\~a}o dominantes e 
                         apresentaram padr{\~o}es relativamente opostos durante o 
                         trimestre analisado. ABSTRACT: The present study investigates the 
                         behavior of upper and lower levels of atmospheric flow that 
                         leading up to the onset rainy season date in the Central- West and 
                         Southeast of Brazil. That analysis is possible due to the fact 
                         that both regions are part of the South American Monsoon System, 
                         whose have a welldefined dry and wet seasons. The kinetic energy 
                         conversions between eddies in different time scales and the 
                         performance of atmospheric oscillations that interact with 
                         circulation in South America during this period were also 
                         analyzed. On the methodology used, the onset rainy season were 
                         obtained based on the daily rainfall data from the Climate 
                         Prediction Center during period of 39 years (1979-2017) for both 
                         regions. The dates were separated into three categories (early, 
                         mean, and late) and, using the Climate Forecast System Reanalysis 
                         and the Climate Forecast System version 2, the dynamical and 
                         physical patterns of the atmosphere and surface were investigated 
                         during the season in these categories. The interaction between 
                         synoptic (2-6 days), submonthly (7-29 days), and intraseasonal 
                         (30-90 days) scales were also investigated, as well as the terms 
                         of kinetic energy conversion in these time scales over South 
                         America from September to November. Two strongest rainfall nuclei 
                         were noted before the onset rainy season date in both study 
                         regions. Such nuclei are located in the northwest and south of 
                         Brazil, which connect during the onset rainy season, abruptly 
                         increasing precipitation in the Southeast and, especially, in the 
                         Central-Western. In this same time, there was also a connection 
                         between the regional Hadley circulation cell and the larger-scale 
                         breeze circulation over the two studied regions. Normally, the 
                         sensible heat flux is superior to the latent heat flux before the 
                         onset rainy season date in the early category of both regions, 
                         whereas in the late category, the latent heat flux was more 
                         intense throughout the analyzed period. The scale interactions 
                         show peculiar dynamical combinations in each category and that 
                         contributes to the onset rainy season. It was also noted that 
                         there is a relative net balance between the convergence of the 
                         ageostrophic flux term with the baroclinic conversion in the eddy 
                         kinetic energy over South America, such the terms are dominant and 
                         presented relatively opposite patterns during the quarter 
                         analyzed.",
            committee = "Ferreira, Nelson Jesuz (presidente) and Gan, Manoel Alonso 
                         (orientador) and Coelho, Caio Augusto dos Santos and Silve, Adma 
                         Raia and Calheiros, S{\^a}mia Regina Garcia",
         englishtitle = "Atmospheric patterns and interannual variability of the onset 
                         rainy season in the Central-West and Southeast of Brazil",
             language = "pt",
                pages = "178",
                  ibi = "8JMKD3MGP3W34R/43UNJH2",
                  url = "http://urlib.net/ibi/8JMKD3MGP3W34R/43UNJH2",
           targetfile = "publicacao.pdf",
        urlaccessdate = "27 abr. 2024"
}


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