Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean

Detalhes bibliográficos
Autor(a) principal: Palmeira, Ana Cristina Pinto de Almeida
Data de Publicação: 2019
Outros Autores: Camargo, Ricardo de, Palmeira, Ronaldo Maia de Jesus
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/30169
Resumo: In numerical weather prediction, the updating of the Sea Surface Temperature (SST) can influence atmospheric phenomena on different scales. Thus, a simplified model of the oceanic mixed layer (OML), was included as a subroutine in the Brazilian Regional Atmospheric System (BRAMS) in order to update the SST at each time step, with low computational cost. Comparisons between atmospheric simulations using an active OML and climatological SST mask, which is part of the BRAMS model, were made. There were significant direct variations in the latent and sensible heat fluxes as well as in cloudiness: the warmer the SST, the greater the response of these variables. On the other hand, although there was no significant increase in precipitation rates, there was higher rainfall when the SST was higher. The variations in the sea level pressure were to the order of 1-2 hPa, indicating that the variations in surface flows are related to the maintenance and persistence of systems and not to their deepening.
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spelling Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic OceanHeat fluxes; Oceanic mixed layer; Extratropical cycloneIn numerical weather prediction, the updating of the Sea Surface Temperature (SST) can influence atmospheric phenomena on different scales. Thus, a simplified model of the oceanic mixed layer (OML), was included as a subroutine in the Brazilian Regional Atmospheric System (BRAMS) in order to update the SST at each time step, with low computational cost. Comparisons between atmospheric simulations using an active OML and climatological SST mask, which is part of the BRAMS model, were made. There were significant direct variations in the latent and sensible heat fluxes as well as in cloudiness: the warmer the SST, the greater the response of these variables. On the other hand, although there was no significant increase in precipitation rates, there was higher rainfall when the SST was higher. The variations in the sea level pressure were to the order of 1-2 hPa, indicating that the variations in surface flows are related to the maintenance and persistence of systems and not to their deepening.Universidade Federal do Rio de JaneiroPalmeira, Ana Cristina Pinto de AlmeidaCamargo, Ricardo dePalmeira, Ronaldo Maia de Jesus2019-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/3016910.11137/2019_2_245_258Anuário do Instituto de Geociências; Vol 42, No 2 (2019); 245-258Anuário do Instituto de Geociências; Vol 42, No 2 (2019); 245-2581982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJenghttps://revistas.ufrj.br/index.php/aigeo/article/view/30169/17065Copyright (c) 2019 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccess2019-12-10T15:04:16Zoai:www.revistas.ufrj.br:article/30169Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2019-12-10T15:04:16Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv
Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
title Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
spellingShingle Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
Palmeira, Ana Cristina Pinto de Almeida
Heat fluxes; Oceanic mixed layer; Extratropical cyclone
title_short Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
title_full Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
title_fullStr Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
title_full_unstemmed Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
title_sort Sea Surface Temperature Optimization Evaluation in the Passage of an Explosive Cyclone in the Southwest Atlantic Ocean
author Palmeira, Ana Cristina Pinto de Almeida
author_facet Palmeira, Ana Cristina Pinto de Almeida
Camargo, Ricardo de
Palmeira, Ronaldo Maia de Jesus
author_role author
author2 Camargo, Ricardo de
Palmeira, Ronaldo Maia de Jesus
author2_role author
author
dc.contributor.none.fl_str_mv

dc.contributor.author.fl_str_mv Palmeira, Ana Cristina Pinto de Almeida
Camargo, Ricardo de
Palmeira, Ronaldo Maia de Jesus
dc.subject.none.fl_str_mv
dc.subject.por.fl_str_mv Heat fluxes; Oceanic mixed layer; Extratropical cyclone
topic Heat fluxes; Oceanic mixed layer; Extratropical cyclone
description In numerical weather prediction, the updating of the Sea Surface Temperature (SST) can influence atmospheric phenomena on different scales. Thus, a simplified model of the oceanic mixed layer (OML), was included as a subroutine in the Brazilian Regional Atmospheric System (BRAMS) in order to update the SST at each time step, with low computational cost. Comparisons between atmospheric simulations using an active OML and climatological SST mask, which is part of the BRAMS model, were made. There were significant direct variations in the latent and sensible heat fluxes as well as in cloudiness: the warmer the SST, the greater the response of these variables. On the other hand, although there was no significant increase in precipitation rates, there was higher rainfall when the SST was higher. The variations in the sea level pressure were to the order of 1-2 hPa, indicating that the variations in surface flows are related to the maintenance and persistence of systems and not to their deepening.
publishDate 2019
dc.date.none.fl_str_mv 2019-12-01
dc.type.none.fl_str_mv

dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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dc.identifier.uri.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/30169
10.11137/2019_2_245_258
url https://revistas.ufrj.br/index.php/aigeo/article/view/30169
identifier_str_mv 10.11137/2019_2_245_258
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/30169/17065
dc.rights.driver.fl_str_mv Copyright (c) 2019 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2019 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 42, No 2 (2019); 245-258
Anuário do Instituto de Geociências; Vol 42, No 2 (2019); 245-258
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
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reponame_str Anuário do Instituto de Geociências (Online)
collection Anuário do Instituto de Geociências (Online)
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