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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m12.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZ3r59YD6/GP3Ja
Repositóriosid.inpe.br/iris@1912/2005/07.19.23.54.51
Última Atualização2015:09.08.19.31.35 (UTC) marciana
Repositório de Metadadossid.inpe.br/iris@1912/2005/07.19.23.55
Última Atualização dos Metadados2018:06.05.00.52.28 (UTC) administrator
Chave SecundáriaINPE-6332-PRE/2420
ISSN0022-2402
Rótulo7688
Chave de CitaçãoViannaHolv:1992:PaThCo
TítuloIntegral equation approach to tropical ocean dynamics: PartI - Theory and computational methods
Ano1992
Data Secundária19970707
Data de Acesso11 maio 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho12660 KiB
2. Contextualização
Autor1 Vianna, Marcio L.
2 Holvorcem, Paulo R.
Grupo1 DSR-INPE-MCT-BR
RevistaJournal of Marine Research
Volume50
Número1
Páginas1-31
Histórico (UTC)2008-06-09 19:15:33 :: administrator -> jefferson ::
2010-07-07 18:50:28 :: jefferson -> administrator ::
2013-12-01 01:39:08 :: administrator -> marciana :: 1992
2015-09-08 19:31:35 :: marciana -> administrator :: 1992
2018-06-05 00:52:28 :: administrator -> marciana :: 1992
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
ResumoIn linear, three-dimensional, continuously stratified equatorial -plane ocean models with arbitrary and western boundaries the shallow water equations for each vertical mode must be solved numerically in the horizontal variables. This paper introduces a new numerical method of solution for the time-Fourier transformed shallow water equations with slip boundary conditions at boundaries of arbitrary geometry. The method is based on a boundary integral equation (BIE)for the pressure pertubation response to the specified wind-stress forcing field. All other dependent variables are expressed as boundary functionals of the pressure pertubation. The kernels of all functionals are constructed from the Green's function for the Laplace Tidal Equation on the -plane and its derivatives. The efficient computation of these kernels from their exact meridional mode representations may be performed by use of asymptotic methods especially developed for the numerical evaluation of functions expressed as slowly converging series of Hermite functions. The solution of the basic BIE and the computation of the boundary functionals involve the discretization of the ocean boundaries into a number of boundary segments (boundary elements). It is shown that the terms of the BIE involving the wind-stress field over the ocean may be reduced to a boundary integral, which effectively reduces the simulation problem to the solution of a one-dimensional BIE. The method incorporates the ocean physics through the relationship between the coastal pressure field and the basin-wide variables, pointing out to the possibility that the dynamic topography of the ocean may be estimated directly from the wind-stress field and coastal sea-level data.
ÁreaSRE
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4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/6qtX3pFwXQZ3r59YD6/GP3Ja
URL dos dados zipadoshttp://urlib.net/zip/6qtX3pFwXQZ3r59YD6/GP3Ja
Arquivo Alvo1992_vianna.pdf
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5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
DivulgaçãoWEBSCI
Acervo Hospedeirosid.inpe.br/banon/2001/04.06.10.52
6. Notas
Campos Vaziosaffiliation alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel doi e-mailaddress electronicmailaddress format isbn keywords language lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readpermission resumeid rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
e-Mail (login)marciana
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