On the initiation of the walker circulation during 1982/1983 enso event
Autor(a) principal: | |
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Data de Publicação: | 2009 |
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=S0102-77862009000100007 |
Resumo: | The GEOS-1 data from multiyear reanalysis are using. An altered Walker Circulation is initiated by the rising motion created over the warm ocean surface on the eastern Pacific. This occurred during the major El Niño event of 1982-1983. To compensate the rising motion, a sinking motion is generated over western Pacific completing the formation of the altered Walker Circulation. Thus, the initiation of the altered Walker Circulation is by the sea surface gradient as originally envisioned by Bjerknes. |
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On the initiation of the walker circulation during 1982/1983 enso eventWalker CirculationEl NiñoENSOThermodynamicsThe GEOS-1 data from multiyear reanalysis are using. An altered Walker Circulation is initiated by the rising motion created over the warm ocean surface on the eastern Pacific. This occurred during the major El Niño event of 1982-1983. To compensate the rising motion, a sinking motion is generated over western Pacific completing the formation of the altered Walker Circulation. Thus, the initiation of the altered Walker Circulation is by the sea surface gradient as originally envisioned by Bjerknes.Sociedade Brasileira de Meteorologia2009-03-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersiontext/htmlhttp://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862009000100007Revista Brasileira de Meteorologia v.24 n.1 2009reponame:Revista Brasileira de Meteorologia (Online)instname:Sociedade Brasileira de Meteorologia (SBMET)instacron:SBMET10.1590/S0102-77862009000100007info:eu-repo/semantics/openAccessVeiga,José Augusto PaixãoRao,Vadlamudi BrahmanandaFranchito,Sérgio Henriqueeng2009-06-17T00:00:00Zoai:scielo:S0102-77862009000100007Revistahttp://www.rbmet.org.br/port/index.phpONGhttps://old.scielo.br/oai/scielo-oai.php||rbmet@rbmet.org.br1982-43510102-7786opendoar:2009-06-17T00:00Revista Brasileira de Meteorologia (Online) - Sociedade Brasileira de Meteorologia (SBMET)false |
dc.title.none.fl_str_mv |
On the initiation of the walker circulation during 1982/1983 enso event |
title |
On the initiation of the walker circulation during 1982/1983 enso event |
spellingShingle |
On the initiation of the walker circulation during 1982/1983 enso event Veiga,José Augusto Paixão Walker Circulation El Niño ENSO Thermodynamics |
title_short |
On the initiation of the walker circulation during 1982/1983 enso event |
title_full |
On the initiation of the walker circulation during 1982/1983 enso event |
title_fullStr |
On the initiation of the walker circulation during 1982/1983 enso event |
title_full_unstemmed |
On the initiation of the walker circulation during 1982/1983 enso event |
title_sort |
On the initiation of the walker circulation during 1982/1983 enso event |
author |
Veiga,José Augusto Paixão |
author_facet |
Veiga,José Augusto Paixão Rao,Vadlamudi Brahmananda Franchito,Sérgio Henrique |
author_role |
author |
author2 |
Rao,Vadlamudi Brahmananda Franchito,Sérgio Henrique |
author2_role |
author author |
dc.contributor.author.fl_str_mv |
Veiga,José Augusto Paixão Rao,Vadlamudi Brahmananda Franchito,Sérgio Henrique |
dc.subject.por.fl_str_mv |
Walker Circulation El Niño ENSO Thermodynamics |
topic |
Walker Circulation El Niño ENSO Thermodynamics |
description |
The GEOS-1 data from multiyear reanalysis are using. An altered Walker Circulation is initiated by the rising motion created over the warm ocean surface on the eastern Pacific. This occurred during the major El Niño event of 1982-1983. To compensate the rising motion, a sinking motion is generated over western Pacific completing the formation of the altered Walker Circulation. Thus, the initiation of the altered Walker Circulation is by the sea surface gradient as originally envisioned by Bjerknes. |
publishDate |
2009 |
dc.date.none.fl_str_mv |
2009-03-01 |
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=S0102-77862009000100007 |
url |
http://old.scielo.br/scielo.php?script=sci_arttext&pid=S0102-77862009000100007 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
10.1590/S0102-77862009000100007 |
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.24 n.1 2009 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_ |
1752122083570089984 |