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@MastersThesis{Nobre:2021:ImAsDa,
               author = "Nobre, Jo{\~a}o Pedro Gon{\c{c}}alves",
                title = "Impacto da assimila{\c{c}}{\~a}o de dados conjunto-variacional 
                         na previs{\~a}o de epis{\'o}dios de chuvas intensas no Nordeste 
                         brasileiro",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2021",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2021-02-22",
             keywords = "3DVar, 3DEnVar, sistemas convectivos de mesoescala, 
                         assimila{\c{c}}{\~a}o de dados, gridpoint statistical 
                         interpolation, mesoscale convective systems, data assimilation.",
             abstract = "O Nordeste Brasileiro (NEB) encontra-se na regi{\~a}o tropical do 
                         Brasil, limitado pelo oceano Atl{\^a}ntico e com um clima e 
                         vegeta{\c{c}}{\~a}o fortemente influenciados pelo Planalto da 
                         Borborema. A presen{\c{c}}a desse planalto marca 
                         significativamente o clima da regi{\~a}o ao manter a leste massas 
                         de ar com caracter{\'{\i}}sticas mais {\'u}midas e 
                         respons{\'a}veis pela ocorr{\^e}ncia de chuvas e o lado oeste, 
                         massas de ar predominantemente secas. Este trabalho visa avaliar a 
                         performance dos diferentes sistemas de assimila{\c{c}}{\~a}o 
                         dados; 3DVar (Three-Dimensional Variational), EnKF (Ensemble 
                         Kalman Filter) e o h{\'{\i}}brido, 3DEnVar (Three-Dimensional 
                         Ensemble-Variational), no estudo de epis{\'o}dios de SCM 
                         (Sistemas Convectivos de Mesoescala), utilizando previs{\~o}es do 
                         modelo meteorol{\'o}gico de mesoescala WRF (Weather Research and 
                         Forecasting), em compara{\c{c}}{\~a}o com previs{\~o}es do WRF 
                         inicializadas com dados do GEFS (Global Ensemble Forecast System), 
                         para dois eventos de SCM ocorridos nos dias 14 e 24 de janeiro de 
                         2017. Para isso, ser{\'a} utilizada a vers{\~a}o V3.0.0 do SMR 
                         (Sistema de Modelagem Regional) do CPTEC (Centro de Previs{\~a}o 
                         de Tempo e Estudos Clim{\'a}ticos) constitu{\'{\i}}do de dois 
                         componentes: o modelo WRF e o sistema de assimila{\c{c}}{\~a}o 
                         de dados GSI (Gridpoint Statistical Interpolation). Atualmente, o 
                         SMR encontra-se configurado para fornecer condi{\c{c}}{\~o}es 
                         iniciais ao modelo WRF atualizadas pelo 3DVar, que utiliza uma 
                         matriz de covari{\^a}ncia dos erros de previs{\~a}o 
                         climatol{\'o}gica, para ponderar os erros do modelo no processo 
                         de minimiza{\c{c}}{\~a}o da fun{\c{c}}{\~a}o custo. No 
                         presente trabalho, utilizou-se o 3DEnVar no SMR, que consiste de 
                         um sistema 3DVar, cuja matriz de covari{\^a}ncia dos erros de 
                         previs{\~a}o {\'e} calculada atrav{\'e}s da 
                         combina{\c{c}}{\~a}o linear dos membros de um conjunto de 
                         previs{\~o}es que servir{\~a}o para atualizar a matriz 
                         climatol{\'o}gica do SMR, com os erros do dia. Desse modo, o 
                         presente trabalho visa melhorar a detec{\c{c}}{\~a}o e 
                         estimativa da quantidade de chuva dos casos de SCM sobre o NEB ao 
                         utilizar a an{\'a}lise do 3DEnVar na previs{\~a}o de chuva 
                         acumulada em 24 h. Resultados obtidos ilustram que o sistema de 
                         assimila{\c{c}}{\~a}o de dados h{\'{\i}}brido (3DEnVar) foi 
                         capaz de gerar melhores an{\'a}lises, se comparado a um sistema 
                         variacional puro (3DVar), para os campos de press{\~a}o 
                         superficial e umidade ao analisar estatisticamente o desempenho 
                         dos sistemas variacionais atrav{\'e}s do BIAS e RMSE (Root Mean 
                         Square Error). O melhoramento obtido na representa{\c{c}}{\~a}o 
                         dos campos de umidade atrav{\'e}s do 3DEnVar foi essencial para 
                         obten{\c{c}}{\~a}o de boas previs{\~o}es de chuva acumulada em 
                         24 horas, com o modelo WRF, ao ser comparado com a 
                         precipita{\c{c}}{\~a}o registrada por esta{\c{c}}{\~o}es 
                         meteorol{\'o}gicas em superf{\'{\i}}cie, do Instituto Nacional 
                         de Meteorologia (INMET), para os dias 14 e 24 de janeiro de 2017 
                         sobre o NEB. ABSTRACT: The Brazilian Northeast (BNE) is located in 
                         the tropical region of Brazil, it is bounded by the Atlantic 
                         Ocean, and its climate and vegetation is strongly affected by the 
                         Borborema Plateau. The presence of the plateau significantly 
                         defines the climate region. It keeps the humid air masses to the 
                         east, which is responsible for the rain episodes, and at the west 
                         side (northeastern hinterland) predominantly dry air masses are 
                         observed. This work evaluates the performance obtained from 
                         different data assimilation methods, 3DVar (Three-Dimensional 
                         Variational), EnKF (Ensemble Kalman Filter), and 3DEnVar 
                         (Three-Dimensional Ensemble Variational), in the study of 
                         Mesoscale Convective Systems (MCS) episodes. The deterministic 
                         predictions was used from the GEFS (Global Ensemble Forecast 
                         System) model to compare with the WRF (Weather Research and 
                         Forecasting) numerical weather forecast model analysis updated by 
                         different data assimilation methods for January 14th and 24th, 
                         2017 MCS episodes. For that purpose, the RMS (Regional Modeling 
                         System) 3.0.0 version from the Center for Weather Forecasting and 
                         Climate Studies was used with two components: the WRF mesoscale 
                         model and the GSI (Gridpoint Statistical Interpolation) data 
                         assimilation system. Currently, the SMR provides the WRF initial 
                         conditions using the 3DVar data assimilation methodology that uses 
                         a climatological forecast error covariance matrix to weight the 
                         model errors in the cost function minimization process. At this 
                         work, the 3DEnVar was used in the SMR, and it updates the SMR 
                         climatological covariance matrix through the forecast ensemble 
                         members with the errors of the day. To summarise, the present work 
                         studied the improvements in the detection and estimation of 24 
                         hours rain accumulated precipitation quality in MCS cases over 
                         BNE. The statistics indexes BIAS and RMSE (Root Mean Square Error) 
                         show that the hybrid data assimilation system (3DEnVar) is the 
                         best variational system in producing better analyses for the 
                         surface pressure and humidity fields. The best humidity 
                         performances with 3DEn- Var were essential in forecasting 24 hours 
                         accumulated precipitation compared with observational data from 
                         the Brazilian National Institute of Meteorology (INMET) stations, 
                         during convective storms over BNE on January 14th and 24th, 
                         2017.",
            committee = "Gon{\c{c}}alves, Lu{\'{\i}}s Gustavo Gon{\c{c}}alves de 
                         (presidente) and Herdies, Dirceu Luis (orientador) and Vendrasco, 
                         {\'E}der Paulo (orientador) and Bastarz, Carlos Frederico and 
                         Harter, Fabricio Pereira",
         englishtitle = "Ensemble-variational data assimilation impact in heavy rain 
                         forecasting episodes in brazilian Northeast",
             language = "pt",
                pages = "143",
                  ibi = "8JMKD3MGP3W34R/448DGFE",
                  url = "http://urlib.net/ibi/8JMKD3MGP3W34R/448DGFE",
           targetfile = "publicacao.pdf",
        urlaccessdate = "09 maio 2024"
}


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