Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil
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Publication Date: | 2020 |
Other Authors: | , , |
Format: | Article |
Language: | por |
Source: | Revista Ciência e Natura (Online) |
Download full: | https://periodicos.ufsm.br/cienciaenatura/article/view/55305 |
Summary: | A depletion event of 11% of the total ozone column over South Brazil was analyzed from observational data and numerical simulations. The meteorological fields resulting from the simulation did not show the presence of subtropical or polar jets over the study region. The real and simulated soundings showed the dryness at high and low tropospheric levels, pointing a stratospheric intrusion. The total ozone column values from ERA-5 reanalyses showed the maintenance of a region with low total ozone values in tropical latitudes and its advance over the study region, before and during the depletion event. The isentropic retro-trajectories of air parcels at different levels, obtained with the Hybrid Single Lagrangian Integrated Trajectory Model (HYSPLIT), confirmed the zonal transport from the tropical region over Southern Brazil. A combination of a cyclonic circulation at the 850 K stratospheric isentropic level and an intense anticyclonic circulation at the 440 K tropospheric level, over the depletion region, was identified as responsible for the tropopause lift and horizontal transport of ozone-rich air out of the column. |
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Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern BrazilEstudo numérico e observacional de um evento de diminuição da coluna total de ozônio de origem tropical no Sul do BrasilColuna total de ozônioIntrusão estratosféricaDepleção de ozônioTransporte tropicalA depletion event of 11% of the total ozone column over South Brazil was analyzed from observational data and numerical simulations. The meteorological fields resulting from the simulation did not show the presence of subtropical or polar jets over the study region. The real and simulated soundings showed the dryness at high and low tropospheric levels, pointing a stratospheric intrusion. The total ozone column values from ERA-5 reanalyses showed the maintenance of a region with low total ozone values in tropical latitudes and its advance over the study region, before and during the depletion event. The isentropic retro-trajectories of air parcels at different levels, obtained with the Hybrid Single Lagrangian Integrated Trajectory Model (HYSPLIT), confirmed the zonal transport from the tropical region over Southern Brazil. A combination of a cyclonic circulation at the 850 K stratospheric isentropic level and an intense anticyclonic circulation at the 440 K tropospheric level, over the depletion region, was identified as responsible for the tropopause lift and horizontal transport of ozone-rich air out of the column.Um evento de diminuição do 11% da coluna total de ozônio sobre o Sul do Brasil foi analisado a partir de dados observacionais e simulações numéricas. Os campos meteorológicos resultantes da simulação, não mostraram a presença dos jatos subtropical ou polar sobre a região de estudo. As sondagem reais e simuladas evidenciaram o ressecamento en altos e baixos níveis troposféricos, apontando a intrusão de ar estratosférico. As reanálises do ERA-5 mostraram a manutenção de uma região baixos valores de coluna total de ozônio em latitudes tropicais e seu avanço sobre a região de estudo, antes e durante o evento de depleção. As retro-trajetórias isentrópicas de parcelas de ar em diferentes níveis, calculada com o Modelo de Trajetória Integrada Híbrida Lagrangiana de Partícula Única (HYSPLIT), confirmaram o transporte zonal com componente da região tropical sobre o sul do Brasil. Foi identificada a combinação de uma região de circulação ciclônica no nível isentrópico estratosférico de 850 K e de uma intensa circulação anticiclônica no nível troposférico de 440 K sobre a região de depleção da coluna total de ozônio, causantes do levantamento da tropopausa e do transporte horizontal de ar rico em ozônio para fora da coluna.Universidade Federal de Santa Maria2020-09-25info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttps://periodicos.ufsm.br/cienciaenatura/article/view/5530510.5902/2179460X55305Ciência e Natura; Vol. 42 (2020): Special : II ENCONTRO DE METEOROLOGIA DO ESTADO DE SC; e5Ciência e Natura; v. 42 (2020): CIÊNCIA E NATURA: EDIÇÃO ESPECIAL: II ENCONTRO DE METEOROLOGIA DO ESTADO DE SC; e52179-460X0100-8307reponame:Revista Ciência e Natura (Online)instname:Universidade Federal de Santa Maria (UFSM)instacron:UFSMporhttps://periodicos.ufsm.br/cienciaenatura/article/view/55305/htmlCopyright (c) 2020 Ciência e Naturainfo:eu-repo/semantics/openAccessGuzmán, LissetteAnabor, VagnerSteffenel, Luiz AngeloPinheiro, Damaris Kirsch2021-01-15T17:45:01Zoai:ojs.pkp.sfu.ca:article/55305Revistahttps://periodicos.ufsm.br/cienciaenatura/indexPUBhttps://periodicos.ufsm.br/cienciaenatura/oaicienciaenatura@ufsm.br || centraldeperiodicos@ufsm.br2179-460X0100-8307opendoar:2021-01-15T17:45:01Revista Ciência e Natura (Online) - Universidade Federal de Santa Maria (UFSM)false |
dc.title.none.fl_str_mv |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil Estudo numérico e observacional de um evento de diminuição da coluna total de ozônio de origem tropical no Sul do Brasil |
title |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil |
spellingShingle |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil Guzmán, Lissette Coluna total de ozônio Intrusão estratosférica Depleção de ozônio Transporte tropical |
title_short |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil |
title_full |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil |
title_fullStr |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil |
title_full_unstemmed |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil |
title_sort |
Numerical and observational study of an event of decrease in the total ozone column of tropical origin in Southern Brazil |
author |
Guzmán, Lissette |
author_facet |
Guzmán, Lissette Anabor, Vagner Steffenel, Luiz Angelo Pinheiro, Damaris Kirsch |
author_role |
author |
author2 |
Anabor, Vagner Steffenel, Luiz Angelo Pinheiro, Damaris Kirsch |
author2_role |
author author author |
dc.contributor.author.fl_str_mv |
Guzmán, Lissette Anabor, Vagner Steffenel, Luiz Angelo Pinheiro, Damaris Kirsch |
dc.subject.por.fl_str_mv |
Coluna total de ozônio Intrusão estratosférica Depleção de ozônio Transporte tropical |
topic |
Coluna total de ozônio Intrusão estratosférica Depleção de ozônio Transporte tropical |
description |
A depletion event of 11% of the total ozone column over South Brazil was analyzed from observational data and numerical simulations. The meteorological fields resulting from the simulation did not show the presence of subtropical or polar jets over the study region. The real and simulated soundings showed the dryness at high and low tropospheric levels, pointing a stratospheric intrusion. The total ozone column values from ERA-5 reanalyses showed the maintenance of a region with low total ozone values in tropical latitudes and its advance over the study region, before and during the depletion event. The isentropic retro-trajectories of air parcels at different levels, obtained with the Hybrid Single Lagrangian Integrated Trajectory Model (HYSPLIT), confirmed the zonal transport from the tropical region over Southern Brazil. A combination of a cyclonic circulation at the 850 K stratospheric isentropic level and an intense anticyclonic circulation at the 440 K tropospheric level, over the depletion region, was identified as responsible for the tropopause lift and horizontal transport of ozone-rich air out of the column. |
publishDate |
2020 |
dc.date.none.fl_str_mv |
2020-09-25 |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://periodicos.ufsm.br/cienciaenatura/article/view/55305 10.5902/2179460X55305 |
url |
https://periodicos.ufsm.br/cienciaenatura/article/view/55305 |
identifier_str_mv |
10.5902/2179460X55305 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.none.fl_str_mv |
https://periodicos.ufsm.br/cienciaenatura/article/view/55305/html |
dc.rights.driver.fl_str_mv |
Copyright (c) 2020 Ciência e Natura info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Copyright (c) 2020 Ciência e Natura |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
text/html |
dc.publisher.none.fl_str_mv |
Universidade Federal de Santa Maria |
publisher.none.fl_str_mv |
Universidade Federal de Santa Maria |
dc.source.none.fl_str_mv |
Ciência e Natura; Vol. 42 (2020): Special : II ENCONTRO DE METEOROLOGIA DO ESTADO DE SC; e5 Ciência e Natura; v. 42 (2020): CIÊNCIA E NATURA: EDIÇÃO ESPECIAL: II ENCONTRO DE METEOROLOGIA DO ESTADO DE SC; e5 2179-460X 0100-8307 reponame:Revista Ciência e Natura (Online) instname:Universidade Federal de Santa Maria (UFSM) instacron:UFSM |
instname_str |
Universidade Federal de Santa Maria (UFSM) |
instacron_str |
UFSM |
institution |
UFSM |
reponame_str |
Revista Ciência e Natura (Online) |
collection |
Revista Ciência e Natura (Online) |
repository.name.fl_str_mv |
Revista Ciência e Natura (Online) - Universidade Federal de Santa Maria (UFSM) |
repository.mail.fl_str_mv |
cienciaenatura@ufsm.br || centraldeperiodicos@ufsm.br |
_version_ |
1839277886799872000 |