Fechar

@MastersThesis{SucaHuallata:2022:PrClSa,
               author = "Suca Huallata, Lenin Abimael",
                title = "Previs{\~a}o clim{\'a}tica sazonal de precipita{\c{c}}{\~a}o 
                         para o Peru com abordagem estat{\'{\i}}stica",
               school = "Instituto Nacional de Pesquisas Espaciais (INPE)",
                 year = "2022",
              address = "S{\~a}o Jos{\'e} dos Campos",
                month = "2022-09-12",
             keywords = "an{\'a}lise de correla{\c{c}}{\~a}o can{\^o}nica (ACC), 
                         modelos estat{\'{\i}}sticos, precipita{\c{c}}{\~a}o sazonal, 
                         preditores oce{\^a}nicos e atmosf{\'e}ricos, canonical 
                         correlation analysis (ACC), statistical models, seasonal 
                         precipitation, oceanic and atmospheric predictors.",
             abstract = "Previs{\~o}es clim{\'a}ticas fornecem informa{\c{c}}{\~o}es 
                         antecipadas que podem ajudar a reduzir os impactos negativos 
                         associados a per{\'{\i}}odos de excesso ou d{\'e}ficit de 
                         precipita{\c{c}}{\~a}o em diversos setores da sociedade, e 
                         fortalecer o desenvolvimento socioecon{\^o}mico de uma 
                         determinada regi{\~a}o. Neste contexto, o objetivo deste estudo 
                         foi desenvolver e avaliar procedimentos para a 
                         produ{\c{c}}{\~a}o de previs{\~o}es clim{\'a}ticas sazonais de 
                         precipita{\c{c}}{\~a}o para o Peru; usando uma abordagem 
                         estat{\'{\i}}stica baseada na an{\'a}lise de 
                         correla{\c{c}}{\~a}o can{\^o}nica (ACC) com diferentes 
                         preditores, como a temperatura da superf{\'{\i}}cie do mar (TSM) 
                         e vari{\'a}veis de circula{\c{c}}{\~a}o atmosf{\'e}rica em 
                         n{\'{\i}}veis baixos (850 hPa), m{\'e}dio (500 hPa) e alto (200 
                         hPa) da atmosfera. Os resultados mostraram que as principais 
                         vari{\'a}veis atmosf{\'e}ricas e oce{\^a}nicas analisadas no 
                         m{\^e}s de outubro, que foram identificadas como relevantes 
                         preditoras para a previs{\~a}o de precipita{\c{c}}{\~a}o no 
                         trimestre Dezembro-Janeiro-Fevereiro (DJF) posterior ao m{\^e}s 
                         de outubro sobre o Peru foram a TSM com influ{\^e}ncia em setores 
                         da Costa Norte, Costa Central, toda a Serra, Selva Norte e Selva 
                         Central do Peru; a vari{\'a}vel de Altura Geopotencial em (850 
                         hPa) baixos n{\'{\i}}veis (AG850) com influ{\^e}ncia na Costa 
                         Norte, Costa Central, todos os setores da Serra e Selva Peruana; a 
                         vari{\'a}vel de Press{\~a}o ao N{\'{\i}}vel m{\'e}dio do Mar 
                         (PNM) com influ{\^e}ncia nos setores de toda a Costa e Serra 
                         Peruana al{\'e}m da Selva Norte e Selva Sul do Peru; a 
                         vari{\'a}vel Vento Zonal em baixos n{\'{\i}}veis (850 hPa) com 
                         influ{\^e}ncia em setores da Costa Norte e toda Serra do Peru; e 
                         o Vento Zonal (200 hPa) em altos n{\'{\i}}veis (VZ200) com 
                         influ{\^e}ncia na Costa Norte, Costa Sul, e toda a Serra do Peru. 
                         Como a vari{\'a}vel oce{\^a}nica (TSM) foi identificada como o 
                         preditor predominante de precipita{\c{c}}{\~a}o sobre o Peru, 
                         essa vari{\'a}vel foi combinada com outras vari{\'a}veis 
                         atmosf{\'e}ricas (AG850, VZ850 e PNM), sendo os maiores 
                         {\'{\i}}ndices de habilidade preditiva para o setor Serra Sul 
                         obtidos atrav{\'e}s da combina{\c{c}}{\~a}o de TSM e VZ850, 
                         enquanto as combina{\c{c}}{\~o}es de TSM e PNM, e TSM e AG850 
                         apresentaram os maiores valores para o setor Serra Norte. Ao 
                         combinar as duas vari{\'a}veis atmosf{\'e}ricas (PNM, VZ850 e 
                         PNM, AG850) que se destacaram com melhor desempenho com a 
                         vari{\'a}vel oce{\^a}nica (TSM), resultados semelhantes aos 
                         obtidos atrav{\'e}s das combina{\c{c}}{\~o}es anteriores foram 
                         encontrados nos diferentes setores do Peru. Portanto, para a 
                         produ{\c{c}}{\~a}o de previs{\~o}es sazonais 
                         estat{\'{\i}}sticas de precipita{\c{c}}{\~a}o para DJF sobre o 
                         Peru, recomenda-se a combina{\c{c}}{\~a}o da TSM com pelo menos 
                         uma vari{\'a}vel atmosf{\'e}rica para contemplar os mecanismos 
                         f{\'{\i}}sicos do sistema clim{\'a}tico acoplado que modulam a 
                         variabilidade clim{\'a}tica da precipita{\c{c}}{\~a}o sazonal. 
                         ABSTRACT: Climate forecast provide advanced information that can 
                         help reduce the negative impacts associated with periods of excess 
                         or deficit of precipitation in different sectors of society, and 
                         strengthen the socioeconomic development of a given region. In 
                         this context, the objective of this study was to develop and 
                         evaluate procedures for the production of seasonal precipitation 
                         forecasts for Peru; using a statistical approach based on 
                         canonical correlation analysis (CCA) with different predictors 
                         such as sea surface temperature (SST) and atmospheric circulation 
                         variables at low (850 hPa), medium (500 hPa) and high (200 hPa) 
                         levels of the atmosphere. The results showed that the main 
                         atmospheric and oceanic variables analyzed in the month of 
                         October, which were identified as relevant predictors for the 
                         forecast of precipitation in the December-January- February (DJF) 
                         quarter after the month of October over Peru, were the SST with 
                         influence in sectors of the North Coast, Central Coast, all 
                         Sierra, Selva Norte and Selva Central of Peru; the Geopotential 
                         Height variable at (850 hPa) low levels (AG850) with influence on 
                         the North Coast, Central Coast, all sectors of the Sierra and 
                         Peruvian Jungle; the Mean Sea Level Pressure (PNM) variable with 
                         influence on the sectors of the entire Coast and Sierra Peruana as 
                         well as the Selva Norte and Selva Sul of Peru; the Zonal Wind 
                         variable at low levels (850 hPa) with influence in sectors of the 
                         North Coast and the entire Sierra do Peru; and Zonal Wind (200 
                         hPa) at high levels (VZ200) with influence on the North Coast, 
                         South Coast, and the entire Sierra del Peru. As the oceanic 
                         variable (SST) was identified as the predominant predictor for 
                         precipitation over Peru, this variable was combined with other 
                         atmospheric variables (AG850, VZ850 and PNM), with the highest 
                         predictive ability indices for the Sierra Sul sector obtained 
                         through the combination of SST and VZ850, while the combinations 
                         of SST and PNM, and SST and AG850 showed the highest values for 
                         the Sierra Norte sector. By combining the two atmospheric 
                         variables (PNM, VZ850 and PNM, AG850) that stood out with the best 
                         performance with the oceanic variable (SST), results similar to 
                         those obtained through the previous combinations were found in the 
                         different sectors of Peru. Therefore, for the production of 
                         statistical seasonal forecasts of precipitation for DJF over Peru, 
                         it is recommended to combine the SST with at least one atmospheric 
                         variable to contemplate the physical mechanisms of the coupled 
                         climate system that modulate the climate variability of seasonal 
                         precipitation.",
            committee = "Pezzi, Luciano Ponzi (presidente) and Coelho, Caio Augusto dos 
                         Santos (orientador) and Vasconcelos Junior, Francisco das Chagas",
         englishtitle = "Seasonal precipitation forecast for Peru with statistical 
                         approach",
             language = "pt",
                pages = "89",
                  ibi = "8JMKD3MGP3W34T/47N3QDB",
                  url = "http://urlib.net/ibi/8JMKD3MGP3W34T/47N3QDB",
           targetfile = "publicacao.pdf",
        urlaccessdate = "04 maio 2024"
}


Fechar