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@MastersThesis{Carneiro:2005:AvDeMo,
               author = "Carneiro, Gl{\'a}ucia Meira",
                title = "O jato em baixos n{\'{\i}}veis na Am{\'e}rica do Sul: 
                         avalia{\c{c}}{\~a}o do desempenho do modelo Eta/CPTEC durante o 
                         SALLJEX",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2005",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2005-04-01",
             keywords = "jato em baixos n{\'{\i}}veis (JBN), SALLJEX, NCEP, modelo Eta, 
                         crit{\'e}rio de bonner, Am{\'e}rica do Sul, Low Level Jet (LLJ), 
                         South American Low Level Jet Experiment (SALLJEX), National Center 
                         for Enveronmental Prediction (NOAA), Eta model, bonner 
                         criterion.",
             abstract = "Um dos sistemas meteorol{\'o}gicos que adquiriu maior 
                         import{\^a}ncia nos {\'u}ltimos tempos na Am{\'e}rica do Sul 
                         {\'e}, sem duvida, o Jato de Baixos N{\'{\i}}veis (JBN), devido 
                         a sua influ{\^e}ncia na variabilidade da temperatura, umidade e 
                         precipita{\c{c}}{\~a}o na regi{\~a}o central do continente. Por 
                         esse motivo a comunidade cient{\'{\i}}fica se dedicou a 
                         realiza{\c{c}}{\~a}o de campanhas intensivas de 
                         medi{\c{c}}{\~a}o, como por exemplo, o South American Low Level 
                         Jet Experiment (SALLJEX), com a inten{\c{c}}{\~a}o de mitigar, 
                         pelo menos parcialmente, a grande falta de informa{\c{c}}{\~a}o 
                         na regi{\~a}o de atua{\c{c}}{\~a}o do JBN. Este estudo tem como 
                         principal objetivo realizar uma avalia{\c{c}}{\~a}o da 
                         capacidade do modelo regional Eta/CPTEC em prever e simular os 
                         eventos de JBN. A metodologia utilizada consistiu na 
                         compara{\c{c}}{\~a}o das sa{\'{\i}}das do modelo Eta/CPTEC da 
                         vers{\~a}o operacional (40 km) e da vers{\~a}o experimental (20 
                         km) com os dados de radiossondagem realizados nas 
                         esta{\c{c}}{\~o}es de Santa Cruz, Resistencia e Santiago, 
                         coletados durante o SALLJEX. O estudo se concentrou no 
                         per{\'{\i}}odo 1 a 10 de fevereiro de 2003, o qual esteve 
                         marcado fundamentalmente, pela atua{\c{c}}{\~a}o da baixa 
                         termoorogr{\'a}fica {\`a} leste dos Andes, que permitiu a 
                         acelera{\c{c}}{\~a}o geostr{\'o}fica dos ventos de norte na 
                         regi{\~a}o subtropical. Alguns experimentos num{\'e}ricos 
                         tamb{\'e}m foram realizados com o objetivo de analisar o 
                         poss{\'{\i}}vel impacto de determinados fatores num{\'e}ricos, 
                         como a resolu{\c{c}}{\~a}o horizontal, o tamanho do 
                         dom{\'{\i}}nio de integra{\c{c}}{\~a}o e as 
                         condi{\c{c}}{\~o}es de contorno, nos resultados. Ambas as 
                         vers{\~o}es do modelo conseguiram prever com uma boa 
                         acur{\'a}cia as caracter{\'{\i}}sticas fundamentais dos JBN, 
                         ainda que o modelo Eta de 20 km n{\~a}o tenha fornecido um ganho 
                         significativo nas previs{\~o}es quando comparados com o modelo 
                         Eta 40 km. O modelo tamb{\'e}m conseguiu reproduzir 
                         satisfatoriamente as condi{\c{c}}{\~o}es meteorol{\'o}gicas nos 
                         casos de JBN inativos, embora para a esta{\c{c}}{\~a}o de 
                         Santiago o modelo apresente uma superestimativa da velocidade do 
                         vento meridional. Em geral, n{\~a}o foram detectadas grande 
                         diferen{\c{c}}as no desempenho do modelo para os distintos prazos 
                         de previs{\~a}o, evidenciando um maior {\^e}xito nas 
                         previs{\~o}es superiores a 36 horas de anteced{\^e}ncia, embora, 
                         haja uma subestimativa na condi{\c{c}}{\~a}o inicial obtida 
                         atrav{\'e}s das an{\'a}lises do NCEP. Sendo assim, ressalta-se 
                         que o modelo possui a f{\'{\i}}sica adequada para reproduzir as 
                         caracter{\'{\i}}sticas dos JBN quando a situa{\c{c}}{\~a}o de 
                         escala regional {\'e} suficientemente capturada nas 
                         condi{\c{c}}{\~o}es iniciais. A an{\'a}lise espacial mostrou 
                         novamente um bom desempenho do modelo, visto que o erro m{\'e}dio 
                         e o desvio padr{\~a}o n{\~a}o eram significativos na regi{\~a}o 
                         de atua{\c{c}}{\~a}o do JBN. As diferentes 
                         simula{\c{c}}{\~o}es realizadas com ambas as vers{\~o}es do 
                         modelo Eta/CPTEC mostraram, em geral, que o ganho com a 
                         utiliza{\c{c}}{\~a}o de condi{\c{c}}{\~o}es de contorno 
                         analisadas (an{\'a}lises do NCEP) foi pouco significativo, porque 
                         o fator determinante da qualidade da integra{\c{c}}{\~a}o de 
                         curto prazo s{\~a}o as condi{\c{c}}{\~o}es iniciais comum entre 
                         as rodadas. Atrav{\'e}s do estudo dos campos m{\'e}dios de 
                         temperatura, umidade espec{\'{\i}}fica e transporte de vapor 
                         durante o per{\'{\i}}odo analisado, utilizando as 
                         simula{\c{c}}{\~o}es realizadas com um prazo de 36 horas, 
                         p{\^o}de se comprovar que a atua{\c{c}}{\~a}o do JBN exerce uma 
                         forte influ{\^e}ncia sobre a variabilidade da 
                         precipita{\c{c}}{\~a}o na regi{\~a}o subtropical da 
                         Am{\'e}rica do Sul, {\`a} leste dos Andes, incluindo a 
                         Regi{\~a}o Sul do Brasil, Bol{\'{\i}}via, Paraguai, Uruguai e 
                         norte da Argentina. ABSTRACT: One of the meteorological systems 
                         that acquired great importance in South America during the last 
                         years is, undoubtedly, the Low Level Jet (LLJ), mostly due to its 
                         probable influence on the temperature, humidity and precipitation 
                         variability on the central region of the continent. The major 
                         attention that the scientific community gave to this system 
                         motivated the organization of intensive measure campaigns, as the 
                         experiment SALLJEX, tending to reduce at least partially, the lack 
                         of information in the LLJ region. The main objective of this study 
                         is to perform an evaluation of the ability of the Eta/CPTEC 
                         regional model to forecast and simulate some events of LLJ. To 
                         this purpose comparisons between model outputs (an operational 
                         version (40km) and a experimental one (20 km)) and radiosonde data 
                         collected at Santa Cruz, Resistencia and Santiago stations, during 
                         the SALLJEX were done. The work was concentrated in the period 
                         from February, 1st to February, 10th, 2003, which was 
                         characterize, for the presence of the thermal-orographic low to 
                         the east of Andes that allowed a geotrophic acceleration of 
                         northerly winds on the subtropical region. Some experiments has 
                         been performed in order to analyze the possible impact of some 
                         numeric factors into results, such as the horizontal resolution, 
                         the size of the integration domain and the boundary conditions. 
                         Both model versions succeeded in accurately forecasting/simulating 
                         the main features of the LLJ. The Eta 20 km version did not show a 
                         significant forecast improvement when compared to the Eta 40 km. 
                         Eta Model was also successful in reproducing the meteorological 
                         conditions in the cases of inactive LLJ, although it showed a 
                         slight tendency to overestimate the southern wind at Santiago 
                         station. In general model performance was relatively independent 
                         of the forecast lead times, even showing e slight improvement when 
                         the forecast lead-time was greater than 36 hours. This fact is 
                         possibly influenced by the systematic underestimation of the NCEP 
                         analysis, used as initial condition. Results make evident that the 
                         Eta model has an adequate physical package in order to reproduce 
                         the main features of the LLJ, if the regional scale meteorological 
                         situation is corrected captured by the initial conditions. The 
                         horizontal variability of the LLJ was also well captured by the 
                         model since mean and standard errors were no significant in the 
                         region affected by the LLJ. Both 40km and 20 km Eta/CPTEC model 
                         simulations showed that the use of analyzed boundary conditions 
                         (NCEP) did not cause a significant impact. Studying the mean 
                         fields of temperature, specific humidity and humidity transport 
                         during the analyzed period, it is possible to conclude that LLJ 
                         has a strong influence on the precipitation variability in the 
                         subtropical South America, to the east of the Andes, including the 
                         Southern Brazil, Bolivia, Paraguay, Uruguay and north of 
                         Argentina.",
            committee = "Orsini, Jos{\'e} Antonio Marengo (presidente) and Nobre, Carlos 
                         Afonso (orientador) and Seluchi, Marcelo Enrique and Chan, Chou 
                         Sin and Ambrizzi, T{\'e}rcio",
           copyholder = "SID/SCD",
         englishtitle = "The low level jet in South American: valuation of the Eta/CPTEC 
                         model performance during the SALLJEX",
             language = "pt",
                pages = "129",
                  ibi = "6qtX3pFwXQZ3P8SECKy/Gta8b",
                  url = "http://urlib.net/ibi/6qtX3pFwXQZ3P8SECKy/Gta8b",
           targetfile = "paginadeacesso.html",
        urlaccessdate = "21 maio 2024"
}


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