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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentificadorJ8LNKAN8RW/36GB4NS
Repositóriodpi.inpe.br/plutao@80/2009/12.01.12.31   (acesso restrito)
Última Atualização2010:09.20.11.57.32 (UTC) marciana
Repositório de Metadadosdpi.inpe.br/plutao@80/2009/12.01.12.31.46
Última Atualização dos Metadados2018:06.05.00.12.46 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1016/j.csr.2009.07.011
ISSN0278-4343
Rótulolattes: 8150880476098677 4 LorenzzettiStecMellAssi:2009:SpVaSe
Chave de CitaçãoLorenzzettiStecMellAssi:2009:SpVaSe
TítuloSatellite observation of Brazil Current inshore thermal front in the SW South Atlantic: Space/time variability and sea surface temperatures
Ano2009
MêsSet.
Data de Acesso12 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho757 KiB
2. Contextualização
Autor1 Lorenzzetti, João Antonio
2 Stech, José Luiz
3 Mello Filho, Wilson L.
4 Assireu, Arcilan Trevenzoli
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JHHN
Grupo1 DSR-OBT-INPE-MCT-BR
2 DSR-OBT-INPE-MCT-BR
3
4 DSR-OBT-INPE-MCT-BR
Afiliação1 undefined
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3
4 undefined
Endereço de e-Mail do Autor1
2
3
4 arcilan@dsr.inpe.br
Endereço de e-Mailarcilan@dsr.inpe.br
RevistaContinental Shelf Research
Volume29
Número17
Páginas2061-2068
Nota SecundáriaA2_CIÊNCIAS_BIOLÓGICAS_I B3_CIÊNCIAS_BIOLÓGICAS_III A1_ENGENHARIAS_I A1_ENGENHARIAS_III A2_GEOCIÊNCIAS A2_INTERDISCIPLINAR A2_SAÚDE_COLETIVA
Histórico (UTC)2009-12-14 13:11:28 :: lattes -> marciana ::
2009-12-17 11:31:39 :: marciana -> administrator ::
2010-05-12 02:05:22 :: administrator -> marciana ::
2011-05-20 10:31:34 :: marciana -> administrator :: 2009
2015-10-10 10:11:52 :: administrator -> marciana :: 2009
2016-10-12 23:46:16 :: marciana -> administrator :: 2009
2018-06-05 00:12:46 :: administrator -> marciana :: 2009
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-Chaveanalytical method
bimodal association
cartography
coastal zone
data set
eddy
frontal feature
potential vorticity
probability
radiometer
satellite data
sea surface temperature
seasonal variation
shelf break front
spatial distribution
spatial variation
statistical analysis
temporal period
temporal variation
thermal regime
Atlantic Ocean
Atlantic Ocean (South)
ResumoA data set of 199 sea surface temperature maps derived from the Advanced Very High Resolution Radiometer for the period 2000-2002 was processed to derive the position of the surface inshore thermal front of the Brazil Current (BCIF) in the SE Brazilian coastal and oceanic area. After the derivation of the position of the BC front for each image. the ensemble of digital frontal vectors was processed using the algorithm of frontal density (FD) For each 5' x 5' cell in the domain the calculated FD provided an index expressing the presence and persistence of the front in the area or the probability of finding the front in the region. In the paper we present the results of the FD analysis to get a better view of the space and time variability of the BC front in the region The highest values of FD were in general observed close to or at the shelf break zone (between 200 and 1000 m isobaths) From 20 degrees S to 23 degrees S there is a tendency of BCIF to be positioned over the Outer shelf, inshore of the 200 m isobaths. SE of Cape Sao Tome and S of Cape Frio it was observed a bimodal spatial distribution of highest FD caused by the presence of two semi-permanent frontal eddies. After moving offshore near Cape Frio, the BCIF tends to return to the shelf break zone south of 24 degrees S probably due to a potential vorticity conservation mechanism The position of the highest FD values calculated for different seasons confirms previous studies in that BCIF is closer to the coast during the summer and furthest offshore in the winter Statistical analysis of the SST data gave for the BCIF an average SST gradient of 0.31 degrees C km(-1) with a standard deviation of 0.15 degrees C km(-1). A mean frontal width of 6 km was inferred from the average SST gradient and typical temperatures near the front at both sides, at outer shelf and in the BC itself. A Weibull probability density function can be fitted to describe the BCIF SST gradients with scale factor c = 0.3460 degrees C km(-1) and shape factor k = 2.1737. The BCIF SST gradient showed a seasonal variability with the smallest gradients in summer (similar to 0.24 degrees C km(-1)) and the highest in autumn (similar to 0.33 degrees C km(-1)) Using a three harmonic Fourier fit for the SST field near the BCIF, at the outer shelf and at interior of BC, it was possible to derive an analytical model for the time variability of the SST gradient of BCIF.
ÁreaSRE
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4. Condições de acesso e uso
Idiomaen
Arquivo Alvolorezentti.pdf
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Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
URL (dados não confiáveis)DOI: 10.1016/j.csr.2009.07.011
DivulgaçãoWEBSCI
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype
7. Controle da descrição
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