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dc.contributor.authorSantos, Luiz Octavio Fabricio dospt_BR
dc.contributor.authorMachado, Nadja Gomespt_BR
dc.contributor.authorBiudes, Marcelo Sacardipt_BR
dc.contributor.authorGeli, Hatim M. E.pt_BR
dc.contributor.authorQuerino, Carlos Alexandre Santospt_BR
dc.contributor.authorRuhoff, Anderson Luispt_BR
dc.contributor.authorIvo, Israel Oliveirapt_BR
dc.contributor.authorLotufo Neto, Néviopt_BR
dc.date.accessioned2023-04-07T03:26:28Zpt_BR
dc.date.issued2023pt_BR
dc.identifier.issn2073-4433pt_BR
dc.identifier.urihttp://hdl.handle.net/10183/256821pt_BR
dc.description.abstractThe Brazilian Midwest has significant spatiotemporal variability in terms of precipitation and air temperature, making it more vulnerable to the occurrence of extreme weather events. The objective of this study is to characterize the trend of extreme climatic events regarding precipitation and air temperature in the Brazilian Midwest, and to analyze their relationship with Pacific and Atlantic Sea Surface Temperature anomalies (SSTAs). We used daily precipitation and air temperature data measured at 24 conventional weather stations. Pacific and Atlantic SSTA data were obtained from the Climate Prediction Center. The frequency of hot extremes had increased, while that of cold extremes had decreased significantly, thus highlighting the consistent warming across the Brazilian Midwest. The precipitation extremes had greater variability than the temperature extremes. Precipitation intensity increased in Amazonia, with no change in annual precipitation volume. The precipitation extremes in the Brazilian Savanna, Pantanal, and the Atlantic Forest did not have a welldefined pattern but indicated a trend towards a decrease in days with intense precipitation events. In general, the Equatorial Pacific and Atlantic Ocean (TNAI and TSAI) SSTAs were negatively correlated with precipitation extreme indices and positively correlated with air temperature extreme indices in the Amazon. However, the North Atlantic SSTAs were positively correlated with precipitation and air temperature extreme indices in the Brazilian Savanna and Pantanal. In addition, the Pacific SSTAs were positively correlated with precipitation intensity in the Atlantic Forest. Thus, the variability of the trends of precipitation and air temperature extreme indices in the Brazilian Midwest was observed, and it was surmised that this measure was significantly related to Pacific and Atlantic SSTAs.en
dc.format.mimetypeapplication/pdfpt_BR
dc.language.isoengpt_BR
dc.relation.ispartofAtmosphere. Basel. Vol. 14, no. 3 (Mar. 2023), [article] 426, 20 p.pt_BR
dc.rightsOpen Accessen
dc.subjectSST anomaliesen
dc.subjectEventos extremospt_BR
dc.subjectPrecipitationen
dc.subjectTemperatura do arpt_BR
dc.subjectAir temperatureen
dc.subjectPrecipitaçãopt_BR
dc.subjectClimate variabilityen
dc.subjectVariabilidade climáticapt_BR
dc.subjectTemperatura da água do marpt_BR
dc.subjectBrasil, Região Centro-Oestept_BR
dc.titleTrends in precipitation and air temperature extremes and their relationship with sea surface temperature in the brazilian midwestpt_BR
dc.typeArtigo de periódicopt_BR
dc.identifier.nrb001164111pt_BR
dc.type.originEstrangeiropt_BR


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