Severe Weather Events over Southeastern Brazil during the 2016 Dry Season

Author:

Rehbein Amanda1,Dutra Lívia Márcia Mosso1,Ambrizzi Tercio1ORCID,da Rocha Rosmeri Porfírio1,Reboita Michelle Simões2,da Silva Gyrlene Aparecida Mendes3ORCID,Gozzo Luiz Felippe4,Tomaziello Ana Carolina Nóbile1,Campos José Leandro Pereira Silveira1,Mayta Victor Raul Chavez1,Crespo Natália Machado1,Bueno Paola Gimenes1ORCID,Aliaga Nestares Vannia Jaqueline1,Machado Laís Tabosa1,De Jesus Eduardo Marcos1,Pampuch Luana Albertani5,Custódio Maria de Souza4,Carpenedo Camila Bertoletti6

Affiliation:

1. Departamento de Ciências Atmosféricas, Instituto de Astronomia, Geofísica e Ciências Atmosféricas da Universidade de São Paulo, São Paulo, SP, Brazil

2. Instituto de Recursos Naturais da Universidade Federal de Itajubá, Itajubá, MG, Brazil

3. Departamento de Ciências do Mar da Universidade Federal de São Paulo, São Paulo, SP, Brazil

4. Departamento de Física da Universidade Estadual Paulista Júlio de Mesquita Filho, Campus de Bauru, SP, Brazil

5. Instituto de Ciência e Tecnologia da Universidade Estadual Paulista Júlio de Mesquita Filho, Campus de São José dos Campos, São Paulo, SP, Brazil

6. Instituto de Geografia da Universidade Federal de Uberlândia, Uberlândia, MG, Brazil

Abstract

Southeastern Brazil is the most populated and economically developed region of this country. Its climate consists of two distinct seasons: the dry season, extending from April to September, the precipitation is significantly reduced in comparison to that of the wet season, which extends from October to March. However, during nine days of the 2016 dry season, successive convective systems were associated with atypical precipitation events, tornadoes and at least one microburst over the southern part of this region. These events led to flooding, damages to buildings, shortages of electricity and water in several places, many injuries, and two documented deaths. The present study investigates the synoptic and dynamical features related to these anomalous events. The convective systems were embedded in an unstable environment with intense low-level jet flow and strong wind shear and were supported by a sequence of extratropical cyclones occurring over the Southwest Atlantic Ocean. These features were intensified by the Madden–Julian oscillation (MJO) in its phase 8 and by intense negative values of the Pacific South America (PSA) 2 mode.

Funder

Conselho Nacional de Desenvolvimento Científico e Tecnológico

Publisher

Hindawi Limited

Subject

Atmospheric Science,Pollution,Geophysics

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