Synoptic and Mesoscale Analysis of a Severe Weather Event in Southern Brazil at the End of June 2020

Author:

Fortunato de Faria Leandro Fortunato de1,Reboita Michelle Simões1,Mattos Enrique Vieira1,Carvalho Vanessa Silveira Barreto1,Martins Ribeiro Joao Gabriel Martins1,Capucin Bruno César2,Drumond Anita3ORCID,Paes dos Santos Ana Paula Paes dos4

Affiliation:

1. Instituto de Recursos Naturais, Universidade Federal de Itajubá, IRN, Avenida BPS 1303, Itajubá 37500-903, MG, Brazil

2. Ampere Consultoria, Rua Alvorada 1289, Sala: 1902 a 1905, Vila Olímpia, São Paulo 04550-003, SP, Brazil

3. Universidade de São Paulo, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, São Paulo 05508-090, SP, Brazil

4. Vale Technological Institute, Belém 66055-090, PA, Brazil

Abstract

At the end of June 2020, an explosive extratropical cyclone was responsible for an environment in which a squall line developed and caused life and economic losses in Santa Catarina state, southern Brazil. The aims of this case study are the following: (a) to describe the drivers of the cyclogenesis; (b) to investigate through numerical simulations the contribution of sea–air interaction to the development of the cyclone as an explosive system; and (c) to present the physical properties of the clouds associated with the squall line. The cyclogenesis started at 1200 UTC on 30 June 2020 on the border of southern Brazil and Uruguay, having a trough at middle-upper levels as a forcing, which is a common driver of cyclogenesis in the studied region. In addition, the cyclone’s lifecycle followed Bjerknes and Solberg’s conceptual model of cyclone development. A special feature of this cyclone was its fast deepening, reaching the explosive status 12 h after its genesis. A comparison between numerical experiments with sensible and latent turbulent heat fluxes switched on and off showed that the sea–air interaction (turbulent heat fluxes) contributed to the cyclone’s deepening leading it to the explosive status. The cold front, which is a component of the cyclone, favored the development of a pre-frontal squall line, responsible for the rough weather conditions in Santa Catarina state. While satellite images do not clearly show the squall line located ahead of the cold front in the cyclone wave due to their coarse resolution, radar reflectivity data represent the propagation of the squall line over southern Brazil. On 30 June 2020, the clouds in the squall line had more than 10 km of vertical extension and a reflectivity higher than 40 dBZ in some parts of the storm; this is an indicator of hail and, consequently, is a required condition for storm electrification. In fact, electrical activity was registered on this day.

Funder

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior

Conselho Nacional de Desenvolvimento Científico e Tecnológico

PETROBRAS

MDPI

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

Reference131 articles.

1. Synoptic-dynamic climatology of the “bomb”;Sanders;Mon. Weather Rev.,1980

2. Characteristics of explosive cyclones over the Northern Pacific;Zhang;J. Appl. Meteorol. Climatol.,2017

3. NDMAIS (2022, January 14). Ventos Durante o Cyclone Bomba em Santa Catarina Chegaram a 168 km/h Aponta Epagri. Available online: https://ndmais.com.br/tempo/velocidade-durante-o-ciclone-bomba-em-santa-catarina-chegou-a-168-km-h-aponta-epagri/.

4. Eventos Meteorológicos Associados ao Ciclone Explosivo Ocorrido em Junho de 2020 e Impactos Socioambientais no Estado de Santa Catarina;Faria;Geografia,2023

5. GZH (2022, February 23). Jornal Digital Gaúcho. Available online: https://gauchazh.clicrbs.com.br/ambiente/noticia/2020/07/.

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3