Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic

Detalhes bibliográficos
Autor(a) principal: AVILA,VILSON D. DE
Data de Publicação: 2021
Outros Autores: NUNES,ANDRÉ B., ALVES,RITA DE CÁSSIA M.
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anais da Academia Brasileira de Ciências (Online)
Texto Completo: http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652021000501102
Resumo: Abstract Six events of explosive cyclogenesis occurred in the south Atlantic were compared using reanalysis data and satellite water vapor imagery. Cases of different intensities (weak, moderate and strong) occurred during 2014 summer season and 2012 winter season were studied. Despite the similarities the tropopause anomaly was more prominent and vertical movements were stronger in the strong cyclogenesis cases. The tropopause anomalies behind the cold front and ahead of the warm front appear only in the mature stage of the weak and moderate cases while in the strong case it is already evident and more intense behind the cold front since the beginning of the cycle. In all the cases confluence of the jet streams took place at higher levels forming a jet streak with difluence occurring downstream and the cyclone beginning in the exit region. The trajectories of the cyclones were in the southeast direction but longer and more meridional in the strong cases. The results indicated the baroclinicity of the region as the main mechanism for the development of these cyclones as well as the amplitude of the upper level jet stream perturbation. Furthermore, all the explosive cyclones developed following the Shapiro & Keyser cyclone conceptual model.
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spelling Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlanticexplosive cyclonetropopause anomalyShapiro-KeyserseclusionAbstract Six events of explosive cyclogenesis occurred in the south Atlantic were compared using reanalysis data and satellite water vapor imagery. Cases of different intensities (weak, moderate and strong) occurred during 2014 summer season and 2012 winter season were studied. Despite the similarities the tropopause anomaly was more prominent and vertical movements were stronger in the strong cyclogenesis cases. The tropopause anomalies behind the cold front and ahead of the warm front appear only in the mature stage of the weak and moderate cases while in the strong case it is already evident and more intense behind the cold front since the beginning of the cycle. In all the cases confluence of the jet streams took place at higher levels forming a jet streak with difluence occurring downstream and the cyclone beginning in the exit region. The trajectories of the cyclones were in the southeast direction but longer and more meridional in the strong cases. The results indicated the baroclinicity of the region as the main mechanism for the development of these cyclones as well as the amplitude of the upper level jet stream perturbation. Furthermore, all the explosive cyclones developed following the Shapiro & Keyser cyclone conceptual model.Academia Brasileira de Ciências2021-01-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652021000501102Anais da Academia Brasileira de Ciências v.93 n.3 2021reponame:Anais da Academia Brasileira de Ciências (Online)instname:Academia Brasileira de Ciências (ABC)instacron:ABC10.1590/0001-3765202120190157info:eu-repo/semantics/openAccessAVILA,VILSON D. DENUNES,ANDRÉ B.ALVES,RITA DE CÁSSIA M.eng2021-06-11T00:00:00Zoai:scielo:S0001-37652021000501102Revistahttp://www.scielo.br/aabchttps://old.scielo.br/oai/scielo-oai.php||aabc@abc.org.br1678-26900001-3765opendoar:2021-06-11T00:00Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)false
dc.title.none.fl_str_mv Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
title Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
spellingShingle Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
AVILA,VILSON D. DE
explosive cyclone
tropopause anomaly
Shapiro-Keyser
seclusion
title_short Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
title_full Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
title_fullStr Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
title_full_unstemmed Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
title_sort Comparing explosive cyclogenesis cases of different intensities occurred in Southern Atlantic
author AVILA,VILSON D. DE
author_facet AVILA,VILSON D. DE
NUNES,ANDRÉ B.
ALVES,RITA DE CÁSSIA M.
author_role author
author2 NUNES,ANDRÉ B.
ALVES,RITA DE CÁSSIA M.
author2_role author
author
dc.contributor.author.fl_str_mv AVILA,VILSON D. DE
NUNES,ANDRÉ B.
ALVES,RITA DE CÁSSIA M.
dc.subject.por.fl_str_mv explosive cyclone
tropopause anomaly
Shapiro-Keyser
seclusion
topic explosive cyclone
tropopause anomaly
Shapiro-Keyser
seclusion
description Abstract Six events of explosive cyclogenesis occurred in the south Atlantic were compared using reanalysis data and satellite water vapor imagery. Cases of different intensities (weak, moderate and strong) occurred during 2014 summer season and 2012 winter season were studied. Despite the similarities the tropopause anomaly was more prominent and vertical movements were stronger in the strong cyclogenesis cases. The tropopause anomalies behind the cold front and ahead of the warm front appear only in the mature stage of the weak and moderate cases while in the strong case it is already evident and more intense behind the cold front since the beginning of the cycle. In all the cases confluence of the jet streams took place at higher levels forming a jet streak with difluence occurring downstream and the cyclone beginning in the exit region. The trajectories of the cyclones were in the southeast direction but longer and more meridional in the strong cases. The results indicated the baroclinicity of the region as the main mechanism for the development of these cyclones as well as the amplitude of the upper level jet stream perturbation. Furthermore, all the explosive cyclones developed following the Shapiro & Keyser cyclone conceptual model.
publishDate 2021
dc.date.none.fl_str_mv 2021-01-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652021000501102
url http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0001-37652021000501102
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv 10.1590/0001-3765202120190157
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv text/html
dc.publisher.none.fl_str_mv Academia Brasileira de Ciências
publisher.none.fl_str_mv Academia Brasileira de Ciências
dc.source.none.fl_str_mv Anais da Academia Brasileira de Ciências v.93 n.3 2021
reponame:Anais da Academia Brasileira de Ciências (Online)
instname:Academia Brasileira de Ciências (ABC)
instacron:ABC
instname_str Academia Brasileira de Ciências (ABC)
instacron_str ABC
institution ABC
reponame_str Anais da Academia Brasileira de Ciências (Online)
collection Anais da Academia Brasileira de Ciências (Online)
repository.name.fl_str_mv Anais da Academia Brasileira de Ciências (Online) - Academia Brasileira de Ciências (ABC)
repository.mail.fl_str_mv ||aabc@abc.org.br
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