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@PhDThesis{Palharini:2021:AnExPr,
               author = "Palharini, Rayana Santos Araujo",
                title = "Analysis of extreme precipitation events estimated by satellite 
                         and its relationship with mesoscale convective systems over South 
                         America",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2021",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2021-02-24",
             keywords = "satellite, extreme rainfall, estimates, MCS, sat{\'e}lite, chuva 
                         extrema, estimativas.",
             abstract = "Climate change is increasing the intensity and frequency of 
                         extreme events around the world and our society is vulnerable to 
                         the dangers of natural disasters. According to the Brazilian Atlas 
                         of Natural Disasters, a total of 38,996 disasters were recorded 
                         during the period 1991-2012. According to this database, 
                         approximately 40% of hydrometeorological events were caused by 
                         floods, landslides, hail, local storms and windstorms. One of the 
                         main meteorological variables associated with natural disasters is 
                         precipitation. Understanding the behavior and improving the 
                         prediction of these events is of fundamental importance as heavy 
                         rainfall causes irreparable damage and causes great economic 
                         losses for a country. With the objective of improve the 
                         understanding about extreme rainfall of Brazil a daily 1°x1° 
                         gridded precipitation database was used to assess the performance 
                         of different precipitation products to retrieval extreme rainfall 
                         at different regions of Brazil, as well as an analysis of the 
                         Mesoscale Convective Systems and their influence on extreme rain. 
                         The products evaluated in this investigation were 3B42 RT v7.0, 
                         3B42 RT v7.0 uncalibrated, CMORPH V1.0 RAW, CMORPH V1.0 CRT, 
                         GSMAP-NRT-no gauge v6.0, GSMAP-NRT- gauge v6.0, CHIRP V2.0, CHIRPS 
                         V2.0, PERSIANN CDR v1 r1, CoSch and TAPEER v1.5 from Frequent 
                         Rainfall Observations on GridS (FROGS) database. Some products 
                         considered in this investigation are adjusted with rain gauge 
                         values and others only with satellite information. In this study, 
                         these two sets of products were considered. In addition, 
                         gauge-based daily precipitation data, provided by Brazils National 
                         Institute for Space Research, were used as reference in the 
                         analyses. In order to compare gauge-based daily precipitation and 
                         satellite-based data for extreme values, statistical techniques 
                         were used to evaluate the performance the selected satellite 
                         products over the tropical region of South America. According to 
                         the results, the threshold for rain to be considered an extreme 
                         event in South America presented high variability, ranging from 20 
                         to 150 mm/day, depending on the region and the percentile 
                         threshold chosen for analysis. In addition, the results showed 
                         that the ability of the satellite estimates to retrieve rainfall 
                         extremes depends on the geographical location and large-scale 
                         rainfall regimes. Each region of Brazil is characterized by 
                         extremes of rain with different intensities. The regions with the 
                         highest values are south and north regions of Brazil with values 
                         around 125.0 mm/day. In both regions, the GSMAP product (with and 
                         without rain gauges adjustments) have a better performance. On the 
                         other hand, the regions with the lowest intensities are the 
                         northeastern region (inland and coast) with more frequent extreme 
                         values around the 35.0 mm/day. In those regions 3B42RT v7.0 and 
                         3B42RT v7.0 uncalibrated demonstrated a better performance 
                         respectively. It is worth mentioning that the precipitation values 
                         found in this work do not necessarily cause disasters or generate 
                         impacts in the analyzed regions, they were considered extreme from 
                         a statistical point of view, considering the analyzed database. In 
                         order to describe the morphological characteristics of the MCS and 
                         identify the influence of these systems on extreme rain during the 
                         period 2012-2016 in the tropical region of South America, the 
                         dataset used in this investigation was the CACATOES dataset. It is 
                         a level-3 product derived from the Tracking Of Organized 
                         Convection Algorithm through 3D segmentatioN (TOOCAN). According 
                         to results, small systems with a duration smaller than 12 hours 
                         are the ones that occurred with a higher frequency. However, 
                         systems that have duration above 12 hours are the ones that most 
                         contributed to the extreme rain. A significant influence of the 
                         MCS was identified over a large part of the South America regions. 
                         In addition, the influence of the MCS over the investigated region 
                         presented a significant variability. In order to analyze five case 
                         studies associated to extreme rain which caused natural disaster 
                         in five different regions of Brazil was analysed. The regions were 
                         defined based on previous studies according to the climatological 
                         distribution of rainfall in each region. To be considered 
                         statistically extreme, the cases were analyzed considering rain 
                         values above the 99th percentile during the period 2012-2016. 
                         Three databases were used: Precipitation from (i) rain gauges 
                         stations and (ii) different satellite-based estimates and (iii) 
                         Mesoscale convective tracking data. The methodology was based in 
                         identifying events, analyzing the performance of satellite 
                         precipitation estimates to detect the observed extreme rain and 
                         finally quantifying the influence of convective systems on the 
                         extreme rain that occurred. Although all regions of Brazil are 
                         subject to the occurrence of natural disasters caused by extreme 
                         rains, the results suggest that the impacts caused in each region 
                         have different magnitudes. It was noticed that the convective 
                         systems influenced above 90.0 % of the extreme rains in the case 
                         analysed in South region of Brazil while it influenced about 60.0 
                         % to 90.0 % of the extreme rains in the case analysed in Northeast 
                         region of Brazil. In general, satellite products have identified 
                         rain events, however, in the southern region of Brazil, products 
                         have tended to overestimate rainfall, while other regions have 
                         tended to underestimate extreme rain values. It can be seen then 
                         that it is still a challenge for the methods used in the satellite 
                         precipitation estimation products to accurately identify specific 
                         extreme rain events. RESUMO: As mudan{\c{c}}as clim{\'a}ticas 
                         est{\~a}o aumentando a intensidade e a frequ{\^e}ncia de eventos 
                         extremos em todo o mundo. Cada vez mais, a sociedade est{\'a} 
                         vulner{\'a}vel aos perigos dos desastres naturais. De acordo com 
                         o Atlas Brasileiro de Desastres Naturais, um total de 38.996 
                         desastres foram registrados no per{\'{\i}}odo de 1991 a 2012. De 
                         acordo com esta base de dados, aproximadamente 40% dos eventos 
                         hidrometeorol{\'o}gicos foram causados por 
                         inunda{\c{c}}{\~o}es, deslizamentos de terra, granizo, 
                         tempestades locais e vendavais. Uma das principais vari{\'a}veis 
                         meteorol{\'o}gicas associadas aos desastres naturais {\'e} a 
                         precipita{\c{c}}{\~a}o. Entender o comportamento e melhorar a 
                         previs{\~a}o desses eventos {\'e} de fundamental 
                         import{\^a}ncia, pois chuvas intensas causam danos 
                         irrepar{\'a}veis e grandes perdas econ{\^o}micas para um 
                         pa{\'{\i}}s. Com o objetivo de melhorar o entendimento sobre as 
                         chuvas extremas do Brasil, um banco de dados di{\'a}rio de 
                         precipita{\c{c}}{\~a}o em grade de 1°x1° foi usado para avaliar 
                         a habilidade de diferentes produtos de estimativas de 
                         precipita{\c{c}}{\~a}o por sat{\'e}lite em detectar as chuvas 
                         extremas em diferentes regi{\~o}es do Brasil, bem como a 
                         an{\'a}lise da sistemas convectivos de mesoescala e sua 
                         influ{\^e}ncia nas chuvas extremas. Os produtos avaliados nesta 
                         investiga{\c{c}}{\~a}o foram 3B42 RT v7.0, 3B42 RT v7.0 n{\~a}o 
                         calibrado, CMORPH V1.0 RAW, CMORPH V1.0 CRT, GSMAP-NRT-sem 
                         pluviometro v6.0, GSMAP-NRT-com pluviometro v6.0 , CHIRP V2.0, 
                         CHIRPS V2.0, PERSIANN CDR v1 r1, CoSch e TAPEER v1.5 do banco de 
                         dados Frequent Rainfall Observations on GridS (FROGS). Alguns 
                         produtos considerados nesta investiga{\c{c}}{\~a}o s{\~a}o 
                         ajustados com valores de pluvi{\^o}metro e outros apenas com 
                         informa{\c{c}}{\~o}es de sat{\'e}lite. Neste estudo, esses dois 
                         conjuntos de produtos foram considerados. Al{\'e}m disso, dados 
                         de precipita{\c{c}}{\~a}o di{\'a}ria baseados em indicadores, 
                         fornecidos pelo Instituto Nacional de Pesquisas Espaciais do 
                         Brasil, foram usados como refer{\^e}ncia nas an{\'a}lises. A fim 
                         de comparar a precipita{\c{c}}{\~a}o di{\'a}ria baseada em 
                         pluvi{\^o}metro e os dados de sat{\'e}lite para valores 
                         extremos, t{\'e}cnicas estat{\'{\i}}sticas foram usadas para 
                         avaliar o desempenho dos produtos de sat{\'e}lite selecionados na 
                         regi{\~a}o tropical da Am{\'e}rica do Sul. De acordo com os 
                         resultados, o limiar para chuva ser considerada um evento extremo 
                         na Am{\'e}rica do Sul apresentou grande variabilidade, variando 
                         de 20,0 a 150,0 mm/dia, dependendo da regi{\~a}o e do limiar de 
                         percentil escolhido para an{\'a}lise. Al{\'e}m disso, os 
                         resultados mostraram que a capacidade das estimativas de 
                         sat{\'e}lite de recuperar os extremos de chuva depende da 
                         localiza{\c{c}}{\~a}o geogr{\'a}fica e dos regimes de chuva em 
                         grande escala. Cada regi{\~a}o do Brasil {\'e} caracterizada por 
                         extremos de chuva com intensidades diferentes. As regi{\~o}es com 
                         os maiores valores s{\~a}o as regi{\~o}es Sul e Norte do Brasil 
                         com valores em torno de 125,0 mm / dia. Em ambas as regi{\~o}es, 
                         o produto GSMAP (com e sem ajustes de pluvi{\^o}metros) tem 
                         melhor desempenho. Por outro lado, as regi{\~o}es com as menores 
                         intensidades s{\~a}o a regi{\~a}o Nordeste (interior e litoral) 
                         com valores extremos mais frequentes em torno dos 35,0 mm/dia. 
                         Nessas regi{\~o}es, o 3B42RT v7.0 e o 3B42RT v7.0 n{\~a}o 
                         calibrado demonstraram um melhor desempenho, respectivamente. Vale 
                         ressaltar que os valores de precipita{\c{c}}{\~a}o encontrados 
                         neste trabalho n{\~a}o necessariamente causam desastres ou geram 
                         impactos nas regi{\~o}es analisadas, foram considerados extremos 
                         do ponto de vista estat{\'{\i}}stico, considerando a base de 
                         dados analisada. Com o objetivo de descrever as 
                         caracter{\'{\i}}sticas morfol{\'o}gicas do MCS e identificar a 
                         influ{\^e}ncia desses sistemas nas chuvas extremas durante o 
                         per{\'{\i}}odo de 2012-2016 na regi{\~a}o tropical da 
                         Am{\'e}rica do Sul, o conjunto de dados utilizado nesta 
                         investiga{\c{c}}{\~a}o foi o conjunto de dados CACATOES. {\'E} 
                         um produto de n{\'{\i}}vel 3 derivado do Algoritmo de 
                         Rastreamento de Convec{\c{c}}{\~a}o Organizada por meio da 
                         segmenta{\c{c}}{\~a}o 3D (TOOCAN). De acordo com os resultados, 
                         pequenos sistemas com dura{\c{c}}{\~a}o inferior a 12 horas 
                         s{\~a}o os que ocorreram com maior frequ{\^e}ncia. Por{\'e}m, 
                         os sistemas que t{\^e}m dura{\c{c}}{\~a}o acima de 12 horas 
                         s{\~a}o os que mais contribuem para as chuvas extremas. Foi 
                         identificada uma influ{\^e}ncia significativa do MCS em grande 
                         parte das regi{\~o}es sul-americanas. Al{\'e}m disso, a 
                         influ{\^e}ncia do MCS sobre a regi{\~a}o investigada apresentou 
                         uma variabilidade significativa. Com o objetivo de analisar cinco 
                         estudos de caso associados {\`a}s chuvas extremas que causaram 
                         desastres naturais em cinco diferentes regi{\~o}es do Brasil 
                         foram analisados. As regi{\~o}es foram definidas com base em 
                         estudos anteriores de acordo com a distribui{\c{c}}{\~a}o 
                         climatol{\'o}gica das chuvas em cada regi{\~a}o. Para serem 
                         considerados estatisticamente extremos, os casos foram analisados 
                         considerando-se valores de chuva acima do percentil 99 durante o 
                         per{\'{\i}}odo de 2012-2016. Tr{\^e}s bancos de dados foram 
                         usados: Precipita{\c{c}}{\~a}o de (i) esta{\c{c}}{\~o}es 
                         pluviom{\'e}tricas e (ii) diferentes estimativas baseadas em 
                         sat{\'e}lite e (iii) dados de rastreamento convectivo de 
                         mesoescala. A metodologia baseou-se na identifica{\c{c}}{\~a}o 
                         de eventos, na an{\'a}lise do desempenho das estimativas de 
                         precipita{\c{c}}{\~a}o por sat{\'e}lite para detectar as chuvas 
                         extremas observadas e, por fim, quantificar a influ{\^e}ncia dos 
                         sistemas convectivos nas chuvas extremas ocorridas. Embora todas 
                         as regi{\~o}es do Brasil estejam sujeitas {\`a} ocorr{\^e}ncia 
                         de desastres naturais causados por chuvas extremas, os resultados 
                         sugerem que os impactos causados em cada regi{\~a}o t{\^e}m 
                         magnitudes diferentes. Percebeu-se que o sistema convectivo 
                         influenciou acima de 90,0 % das chuvas extremas no caso analisado 
                         na regi{\~a}o Sul do Brasil enquanto influenciou cerca de 60,0 % 
                         a 90,0 % das chuvas extremas no caso analisado na regi{\~a}o 
                         Nordeste do Brasil. Em geral, os produtos de sat{\'e}lite 
                         identificam eventos de chuva, no entanto, na regi{\~a}o sul do 
                         Brasil, os produtos tendem a superestimar as chuvas, enquanto 
                         outras regi{\~o}es tendem a subestimar os valores extremos de 
                         chuva. Pode-se ver ent{\~a}o que ainda {\'e} um desafio para os 
                         m{\'e}todos usados nos produtos de estimativa de 
                         precipita{\c{c}}{\~a}o por sat{\'e}lite identificar com 
                         precis{\~a}o eventos espec{\'{\i}}ficos de chuva extrema.",
            committee = "Gan, Manoel Alonso (presidente) and Vila, Daniel Alejandro 
                         (orientador) and Ferreira, Nelson Jesuz and Rodrigues, Daniele 
                         T{\^o}rres and Mattos, Enrique Vieira",
         englishtitle = "An{\'a}lise de eventos extremos de precipita{\c{c}}{\~a}o 
                         estimados por sat{\'e}lite e sua rela{\c{c}}{\~a}o com sistemas 
                         convectivos de mesoescala sobre a Am{\'e}rica do Sul",
             language = "en",
                pages = "168",
                  ibi = "8JMKD3MGP3W34R/4465CAB",
                  url = "http://urlib.net/ibi/8JMKD3MGP3W34R/4465CAB",
           targetfile = "publicacao.pdf",
        urlaccessdate = "01 maio 2024"
}


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