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@PhDThesis{Ferreira:2021:UsAsDa,
               author = "Ferreira, Rute Costa",
                title = "Uso da assimila{\c{c}}{\~a}o de dados de radar e descargas 
                         el{\'e}tricas na previs{\~a}o de curt{\'{\i}}ssimo prazo no 
                         Sul do Brasil",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2021",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2021-02-25",
             keywords = "WRFDA, GSI, BrasilDAT, GLM.",
             abstract = "As tempestades que atuam no Sul do Brasil causam diversos danos 
                         econ{\^o}micos e sociais. Muitas vezes, estas tempestades 
                         est{\~a}o associadas a tempo severo, com rajadas de ventos, 
                         granizo e descargas el{\'e}tricas atmosf{\'e}ricas, e at{\'e} 
                         mesmo tornados. O uso da modelagem num{\'e}rica e dados 
                         observados {\'e} fundamental para aumentar o conhecimento do 
                         ambiente no qual estas se formam e, a partir da{\'{\i}}, 
                         melhorar sua previsibilidade. Neste contexto, este trabalho 
                         estudou tempestades com ocorr{\^e}ncia de descargas 
                         el{\'e}tricas do ano de 2017 e 2018 com foco na 
                         assimila{\c{c}}{\~a}o de dados de radar e de descargas 
                         el{\'e}tricas. As simula{\c{c}}{\~o}es foram feitas a partir 
                         dos dados de refletividade e velocidade radial dos radares da 
                         For{\c{c}}a A{\'e}rea Brasileira, com foco nos dados de Santiago 
                         (RS). Os dados de descargas el{\'e}tricas utilizados foram da 
                         rede de detec{\c{c}}{\~a}o BrasilDAT, e dados do instrumento GLM 
                         (Geostationary Lightning Mapper) do sat{\'e}lite 
                         geoestacion{\'a}rio GOES-16. Para comparar o campo de 
                         precipita{\c{c}}{\~a}o acumulada foram utilizados campos de 
                         estimativa de precipita{\c{c}}{\~a}o do produto MERGE do 
                         CPTEC/INPE. O modelo atmosf{\'e}rico utilizado foi o Weather 
                         Research and Forecasting model (WRF) e sua componente de 
                         assimila{\c{c}}{\~a}o dados (WRFDA), para 
                         assimila{\c{c}}{\~a}o de dados de radar e o sistema Gridpoint 
                         Statistical Interpolation (GSI) para assimila{\c{c}}{\~a}o dos 
                         dados de rel{\^a}mpagos. Os resultados foram analisados em 
                         fun{\c{c}}{\~a}o do impacto da assimila{\c{c}}{\~a}o nos 
                         campos atmosf{\'e}ricos e evolu{\c{c}}{\~a}o na previs{\~a}o 
                         de um sistema frontal em 2017, e um sistema convectivo de meso 
                         escala relacionado {\`a} instabilidade termodin{\^a}mica em 
                         2018, ocorridos no Rio Grande do Sul. Em ambas 
                         condi{\c{c}}{\~o}es atmosf{\'e}ricas, os experimentos com 
                         assimila{\c{c}}{\~a}o dos dados da BrasilDAT ou GLM indicaram um 
                         aumento dos hidrometeoros distribu{\'{\i}}dos em toda a 
                         troposfera e, consequentemente, da precipita{\c{c}}{\~a}o. A 
                         r{\'a}pida taxa de convers{\~a}o microf{\'{\i}}sica foi notada 
                         principalmente na primeira hora de previs{\~a}o. Para o caso de 
                         precipita{\c{c}}{\~a}o decorrente de instabilidade 
                         termodin{\^a}mica, os experimentos com os dados do GLM e radar 
                         assimilados mostraram melhor posicionamento dos n{\'u}cleos 
                         convectivos e desempenho ao prever os sistemas estudados. 
                         Entretanto, a assimila{\c{c}}{\~a}o de dados apenas de descargas 
                         el{\'e}tricas para simula{\c{c}}{\~a}o da frente fria indicou 
                         limita{\c{c}}{\~o}es no GSI ao gerar grandes incrementos e 
                         superestimativa de precipita{\c{c}}{\~a}o, por{\'e}m a 
                         assimila{\c{c}}{\~a}o de dados de radar foi capaz de minimizar 
                         tal limita{\c{c}}{\~a}o ao serem assimilados em algumas das 
                         simula{\c{c}}{\~o}es. Com isso, a assimila{\c{c}}{\~a}o de 
                         dados de radar p{\^o}de complementar poss{\'{\i}}veis 
                         limita{\c{c}}{\~o}es encontradas no novo operador de descargas 
                         el{\'e}tricas no GSI, se tornando complementares de acordo com as 
                         informa{\c{c}}{\~o}es que cada observa{\c{c}}{\~a}o pode 
                         fornecer ao modelo. ABSTRACT: The storms observed in the South of 
                         Brazil cause several economic and social damages. These storms are 
                         often associated with severe weather conditions, with wind gusts, 
                         hail, lightning, and even tornadoes. The use of numerical modeling 
                         and observed data is fundamental to increase the knowledge of the 
                         environment in which storms are formed and improve their 
                         predictability. In this context, this work studied storms with the 
                         occurrence of lightning in the years 2017 and 2018 with a focus on 
                         radar and lightning data assimilation. The simulations were made 
                         based on data of reflectivity and radial velocity from the radars 
                         of the Brazilian Air Force, focusing on data from Santiago (RS). 
                         The data of lightning used were from the BrasilDAT detection 
                         network, and data from the GLM (Geostationary Lightning Mapper) 
                         instrument of the geostationary satellite GOES-16. To compare the 
                         accumulated precipitation field, estimation fields of 
                         precipitation of the MERGE product from CPTEC / INPE were used. 
                         The Weather Research and Forecasting (WRF) model - together with 
                         its data assimilation component (WRFDA) - was used to assimilate 
                         radar data. The Gridpoint Statistical Interpolation (GSI) system 
                         was used to assimilate lightning data. The results were analyzed 
                         according to the impact of assimilation in the atmospheric fields 
                         and evolution in the forecast of studied cases. The cases were: a 
                         frontal system in 2017, and a mesoscale convective system related 
                         to thermodynamic instability in 2018, both occurred in Rio Grande 
                         do Sul. In both atmospheric conditions, the experiments with 
                         assimilation of data from BrasilDAT or GLM indicated an increase 
                         in hydrometeors distributed throughout the troposphere and, 
                         consequently, in precipitation. The rapid rate of microphysical 
                         conversion was noticed mainly in the first hour of forecast. For 
                         the case of precipitation due to thermodynamic instability, the 
                         experiments with the data from the GLM and assimilated radar 
                         showed better positioning of the convective nuclei and performance 
                         when predicting the studied systems. However, the assimilation of 
                         data only from lightning for the simulation of the cold front 
                         indicated limitations in the GSI when generating large increments 
                         and overestimation of precipitation, however, the assimilation of 
                         radar data was able to minimize such limitation when they were 
                         assimilated in some of the simulations. With this, the 
                         assimilation of radar data could complement possible limitations 
                         found in the new lightning operator in GSI, becoming complementary 
                         according to the information that each observation can provide to 
                         the model.",
            committee = "Vila, Daniel Alejandro (presidente) and Herdies, Dirceu Luis 
                         (orientador) and Vendrasco, {\'E}der Paulo (orientador) and 
                         Arav{\'e}quia, Jos{\'e} Antonio and Quadro, M{\'a}rio Francisco 
                         Leal de and Beneti, Cesar Augustus Assis",
         englishtitle = "Use of radar and lightning data assimilation in very short-term 
                         forecast in Southern Brazil",
             language = "pt",
                pages = "171",
                  ibi = "8JMKD3MGP3W34R/44CQ5PL",
                  url = "http://urlib.net/ibi/8JMKD3MGP3W34R/44CQ5PL",
           targetfile = "publicacao.pdf",
        urlaccessdate = "05 maio 2024"
}


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