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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34P/3KB6J32
Repositóriosid.inpe.br/mtc-m21b/2015/09.28.17.15   (acesso restrito)
Última Atualização2015:09.28.17.16.58 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21b/2015/09.28.17.15.30
Última Atualização dos Metadados2018:06.04.02.55.42 (UTC) administrator
DOI10.1016/j.dynatmoce.2015.08.001
ISSN0377-0265
Chave de CitaçãoCintraLenSerAraMar:2015:PhPrDr
TítuloPhysical processes that drive the seasonal evolution of the Southwestern Tropical Atlantic Warm Pool
Ano2015
MêsDec.
Data de Acesso11 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho3408 KiB
2. Contextualização
Autor1 Cintra, Marcio M.
2 Lentini, Carlos Alessandre Domingos
3 Servain, Jacques
4 Araujo, Moacyr
5 Marone, Eduardo
Grupo1
2 DSR-OBT-INPE-MCTI-GOV-BR
Afiliação1 Universidade Federal do Paraná (UFPR)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Université Pierre et Marie Curie
4 Universidade Federal de Pernambuco (UFPE)
5 Universidade Federal do Paraná (UFPR)
Endereço de e-Mail do Autor1
2 carlos.lentini@inpe.br
RevistaDynamics of Atmospheres and Oceans
Volume72
Nota SecundáriaA2_GEOCIÊNCIAS
Histórico (UTC)2015-09-28 17:15:30 :: simone -> administrator ::
2018-06-04 02:55:42 :: administrator -> simone :: 2015
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-ChaveAir–sea interactions
Heat budget
Mixed layer
Net heat flux
Seasonal cycle
Tropical Atlantic
ResumoThe thermodynamics of the seasonal evolution of the Southwestern Tropical Atlantic Warm Pool (hereafter SWTAWP), which is delimited by the 28 °C isotherm, is investigated using the Regional Ocean Modeling System (ROMS). Results indicate that the net heat flux is responsible for the appearance and extinction of the SWTAWP. From March to May, the SWTAWP attains its maximum development and sometimes merges with equatorial warm waters towards the African continent, whose development follows the same period. Along the equator, the combination of oceanic terms (i.e., advection and diffusion) is important to promote the separation when it occurs of equatorial warm waters from southwestern tropical waters, which develops off the Brazilian coast. An analysis of the relative contribution of the temperature tendency terms of the mixed layer (ML) heat budget over the appearance, development and extinction of the SWTAWP is also done. The most important term for warming and cooling inside of the ML is the net heat flux at the sea surface. The ML is heated by the atmosphere between October and April, whereas the upper ocean cools down between May and September. The highest heat content values occur during the lower-temperature period (August to October), which is linked to the deepening of the ML during this time period. The horizontal advection along the equator is important, particularly at the eastern domain, which is influenced by the cold tongue. In this area, the vertical diffusive term is also significant; however, it presents values near zero outside the equator. These results contribute to a better understanding of the behavior of the heat budget within the tropical Atlantic, as previous studies over this region focused along the equator only.
ÁreaSRE
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvocintra_physical.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Repositório Espelhourlib.net/www/2011/03.29.20.55
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Lista de Itens Citando
DivulgaçãoWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Acervo Hospedeirosid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark nextedition notes number orcid pages parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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