An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes
Autor(a) principal: | |
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Data de Publicação: | 2017 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Revista Brasileira de Meteorologia (Online) |
Texto Completo: | http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862017000100039 |
Resumo: | Abstract This study focuses on the quantification and evaluation of the effects of ENSO (El Niño Southern Oscillation) warm phases, using a composite of five intense El Niño episodes between 1979 – 2011 on the Energetic Lorenz Cycle for four distinct regions around the globe: 80° S – 5° N (region 1), 50° S – 5° N (region 2), 30° S – 5° N (region 3), and 30° S – 30° N (region 4), using Data from NCEP reanalysis-II. Briefly, the results showed that zonal terms of potential energy and kinetic energy were intensified, except for region 1, where zonal kinetic energy weakened. Through the analysis of the period in which higher energy production is observed, a strong communication between the available zonal potential and the zonal kinetic energy reservoirs can be identified. This communication weakened the modes linked to eddies of potential energy and kinetic energy, as well as in the other two baroclinic conversions terms. Furthermore, the results indicate that for all the regions, the system itself works to regain its stable condition. |
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An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodesatmospheric energeticsLorenz CycleENSOEl NiñoAbstract This study focuses on the quantification and evaluation of the effects of ENSO (El Niño Southern Oscillation) warm phases, using a composite of five intense El Niño episodes between 1979 – 2011 on the Energetic Lorenz Cycle for four distinct regions around the globe: 80° S – 5° N (region 1), 50° S – 5° N (region 2), 30° S – 5° N (region 3), and 30° S – 30° N (region 4), using Data from NCEP reanalysis-II. Briefly, the results showed that zonal terms of potential energy and kinetic energy were intensified, except for region 1, where zonal kinetic energy weakened. Through the analysis of the period in which higher energy production is observed, a strong communication between the available zonal potential and the zonal kinetic energy reservoirs can be identified. This communication weakened the modes linked to eddies of potential energy and kinetic energy, as well as in the other two baroclinic conversions terms. Furthermore, the results indicate that for all the regions, the system itself works to regain its stable condition.Sociedade Brasileira de Meteorologia2017-03-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862017000100039Revista Brasileira de Meteorologia v.32 n.1 2017reponame:Revista Brasileira de Meteorologia (Online)instname:Sociedade Brasileira de Meteorologia (SBMET)instacron:SBMET10.1590/0102-778632120150114info:eu-repo/semantics/openAccessSátyro,Zayra ChristineVeiga,Joséeng2019-05-23T00:00:00Zoai:scielo:S0102-77862017000100039Revistahttp://www.rbmet.org.br/port/index.phpONGhttps://old.scielo.br/oai/scielo-oai.php||rbmet@rbmet.org.br1982-43510102-7786opendoar:2019-05-23T00:00Revista Brasileira de Meteorologia (Online) - Sociedade Brasileira de Meteorologia (SBMET)false |
dc.title.none.fl_str_mv |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes |
title |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes |
spellingShingle |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes Sátyro,Zayra Christine atmospheric energetics Lorenz Cycle ENSO El Niño |
title_short |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes |
title_full |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes |
title_fullStr |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes |
title_full_unstemmed |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes |
title_sort |
An Analysis of the Energetics of Tropical and Extra-Tropical Regions for Warm ENSO Composite Episodes |
author |
Sátyro,Zayra Christine |
author_facet |
Sátyro,Zayra Christine Veiga,José |
author_role |
author |
author2 |
Veiga,José |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Sátyro,Zayra Christine Veiga,José |
dc.subject.por.fl_str_mv |
atmospheric energetics Lorenz Cycle ENSO El Niño |
topic |
atmospheric energetics Lorenz Cycle ENSO El Niño |
description |
Abstract This study focuses on the quantification and evaluation of the effects of ENSO (El Niño Southern Oscillation) warm phases, using a composite of five intense El Niño episodes between 1979 – 2011 on the Energetic Lorenz Cycle for four distinct regions around the globe: 80° S – 5° N (region 1), 50° S – 5° N (region 2), 30° S – 5° N (region 3), and 30° S – 30° N (region 4), using Data from NCEP reanalysis-II. Briefly, the results showed that zonal terms of potential energy and kinetic energy were intensified, except for region 1, where zonal kinetic energy weakened. Through the analysis of the period in which higher energy production is observed, a strong communication between the available zonal potential and the zonal kinetic energy reservoirs can be identified. This communication weakened the modes linked to eddies of potential energy and kinetic energy, as well as in the other two baroclinic conversions terms. Furthermore, the results indicate that for all the regions, the system itself works to regain its stable condition. |
publishDate |
2017 |
dc.date.none.fl_str_mv |
2017-03-01 |
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=S0102-77862017000100039 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862017000100039 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/0102-778632120150114 |
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 |
Sociedade Brasileira de Meteorologia |
publisher.none.fl_str_mv |
Sociedade Brasileira de Meteorologia |
dc.source.none.fl_str_mv |
Revista Brasileira de Meteorologia v.32 n.1 2017 reponame:Revista Brasileira de Meteorologia (Online) instname:Sociedade Brasileira de Meteorologia (SBMET) instacron:SBMET |
instname_str |
Sociedade Brasileira de Meteorologia (SBMET) |
instacron_str |
SBMET |
institution |
SBMET |
reponame_str |
Revista Brasileira de Meteorologia (Online) |
collection |
Revista Brasileira de Meteorologia (Online) |
repository.name.fl_str_mv |
Revista Brasileira de Meteorologia (Online) - Sociedade Brasileira de Meteorologia (SBMET) |
repository.mail.fl_str_mv |
||rbmet@rbmet.org.br |
_version_ |
1752122085393563648 |