Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America

Abstract The oceanic South Atlantic Convergence Zone (SACZ) has played a major role during South America’s 2021/2022 summer extreme rainy season, being responsible for more than 90% of the precipitation in some regions of Southeast Brazil and in some regions of the Southwestern Atlantic Ocean (SWA)....

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Main Authors: Luciano P. Pezzi, Mario F. L. Quadro, Everaldo B. Souza, Arthur J. Miller, Vadlamudi B. Rao, Eliana B. Rosa, Marcelo F. Santini, Andréia Bender, Ronald B. Souza, Mylene J. Cabrera, Claudia K. Parise, Jonas T. Carvalho, Luciana S. Lima, Maria Rita L. de Quadros, Douglas M. Nehme, Jaime F. António
Format: Article
Language:English
Published: Nature Portfolio 2023-01-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-023-28803-w
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author Luciano P. Pezzi
Mario F. L. Quadro
Everaldo B. Souza
Arthur J. Miller
Vadlamudi B. Rao
Eliana B. Rosa
Marcelo F. Santini
Andréia Bender
Ronald B. Souza
Mylene J. Cabrera
Claudia K. Parise
Jonas T. Carvalho
Luciana S. Lima
Maria Rita L. de Quadros
Douglas M. Nehme
Jaime F. António
author_facet Luciano P. Pezzi
Mario F. L. Quadro
Everaldo B. Souza
Arthur J. Miller
Vadlamudi B. Rao
Eliana B. Rosa
Marcelo F. Santini
Andréia Bender
Ronald B. Souza
Mylene J. Cabrera
Claudia K. Parise
Jonas T. Carvalho
Luciana S. Lima
Maria Rita L. de Quadros
Douglas M. Nehme
Jaime F. António
author_sort Luciano P. Pezzi
collection DOAJ
description Abstract The oceanic South Atlantic Convergence Zone (SACZ) has played a major role during South America’s 2021/2022 summer extreme rainy season, being responsible for more than 90% of the precipitation in some regions of Southeast Brazil and in some regions of the Southwestern Atlantic Ocean (SWA). The summer of 2021/2022 was unique and rare and considered an abnormally humid season as verified by official Brazilian Institutes. First, the unusual number of cases of SACZ episodes (seven), was the highest recorded in the last decade. Second, all the cases that occurred were oceanic SACZ that assumed characteristics of an Atmospheric River and produced an excessively anomalous amount of precipitation during this period. Excess precipitation along with the regions located in mountainous and very uneven relief, which by orographic effects favors high precipitation volumes, were responsible for amplifying the observed impacts, such as landslides and floods that caused several losses to society. We also showed the main effects of coupling and interaction between the waters of the surface layer of the SWA and the atmosphere. Our learning from this study ends with the unprecedented results of how the marine atmospheric boundary layer (MABL) is locally modulated by the sea surface temperature (SST) that lies just below it. Until the present moment, we emphasize that this important mechanism has not been widely highlighted in the literature, showing that even though the ocean is colder than before oceanic SACZ is established, it is still warmer than the overlying air, thus, the ocean continues to be an active source of heat and moisture for the atmosphere and enhances the MABL instability process.
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spelling doaj.art-4b5865b538e1490f87ceca1024f09c662023-01-29T12:08:31ZengNature PortfolioScientific Reports2045-23222023-01-0113111610.1038/s41598-023-28803-wOceanic SACZ produces an abnormally wet 2021/2022 rainy season in South AmericaLuciano P. Pezzi0Mario F. L. Quadro1Everaldo B. Souza2Arthur J. Miller3Vadlamudi B. Rao4Eliana B. Rosa5Marcelo F. Santini6Andréia Bender7Ronald B. Souza8Mylene J. Cabrera9Claudia K. Parise10Jonas T. Carvalho11Luciana S. Lima12Maria Rita L. de Quadros13Douglas M. Nehme14Jaime F. António15Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)Federal Institute of Santa Catarina (IFSC)Federal University of Para (UFPA)Scripps Institution of Oceanography (SIO), University of California San Diego (UCSD)Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)National Center for Monitoring and Early Warning of Natural Disasters (CEMADEN)Earth System Numerical Modeling Division, National Institute of Space Research (INPE)Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)Laboratory for Climate Studies and Modelling, Department of Oceanography, Federal University of Maranhão (UFMA)Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)Federal Institute of Santa Catarina (IFSC)Federal University of Rio de Janeiro (UFRJ)Laboratory of Ocean and Atmosphere Studies (LOA), Earth Observation and Geoinformatics Division (DIOTG), National Institute for Space Research (INPE)Abstract The oceanic South Atlantic Convergence Zone (SACZ) has played a major role during South America’s 2021/2022 summer extreme rainy season, being responsible for more than 90% of the precipitation in some regions of Southeast Brazil and in some regions of the Southwestern Atlantic Ocean (SWA). The summer of 2021/2022 was unique and rare and considered an abnormally humid season as verified by official Brazilian Institutes. First, the unusual number of cases of SACZ episodes (seven), was the highest recorded in the last decade. Second, all the cases that occurred were oceanic SACZ that assumed characteristics of an Atmospheric River and produced an excessively anomalous amount of precipitation during this period. Excess precipitation along with the regions located in mountainous and very uneven relief, which by orographic effects favors high precipitation volumes, were responsible for amplifying the observed impacts, such as landslides and floods that caused several losses to society. We also showed the main effects of coupling and interaction between the waters of the surface layer of the SWA and the atmosphere. Our learning from this study ends with the unprecedented results of how the marine atmospheric boundary layer (MABL) is locally modulated by the sea surface temperature (SST) that lies just below it. Until the present moment, we emphasize that this important mechanism has not been widely highlighted in the literature, showing that even though the ocean is colder than before oceanic SACZ is established, it is still warmer than the overlying air, thus, the ocean continues to be an active source of heat and moisture for the atmosphere and enhances the MABL instability process.https://doi.org/10.1038/s41598-023-28803-w
spellingShingle Luciano P. Pezzi
Mario F. L. Quadro
Everaldo B. Souza
Arthur J. Miller
Vadlamudi B. Rao
Eliana B. Rosa
Marcelo F. Santini
Andréia Bender
Ronald B. Souza
Mylene J. Cabrera
Claudia K. Parise
Jonas T. Carvalho
Luciana S. Lima
Maria Rita L. de Quadros
Douglas M. Nehme
Jaime F. António
Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America
Scientific Reports
title Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America
title_full Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America
title_fullStr Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America
title_full_unstemmed Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America
title_short Oceanic SACZ produces an abnormally wet 2021/2022 rainy season in South America
title_sort oceanic sacz produces an abnormally wet 2021 2022 rainy season in south america
url https://doi.org/10.1038/s41598-023-28803-w
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