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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemarte.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositóriodpi.inpe.br/lise/2001/09.19.12.32
Última Atualização2002:01.28.17.47.47 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/lise/2001/09.19.12.32.16
Última Atualização dos Metadados2018:06.06.02.47.49 (UTC) administrator
Chave SecundáriaINPE-12684-PRE/7974
ISBN85-17-00016-1
Rótulo9407
Chave de CitaçãoSatoPoliLiu:2001:ApSaDa
TítuloApplications of satellite data in estimating heat fluxes
FormatoCD-ROM, On-line.
Ano2001
Data de Acesso10 maio 2024
Tipo SecundárioPRE CN
Número de Arquivos1
Tamanho724 KiB
2. Contextualização
Autor1 Sato, Olga T.
2 Polito, Paulo S.
3 Liu, W. Timothy
Grupo1
2 DSR-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 California Institute of Technology. Jet Propulsion Laboratory (JPL).
EditorKrug, Thelma
Fonseca, Leila Maria Garcia
Endereço de e-Mailerich@sid.inpe.br
Nome do EventoSimpósio Brasileiro de Sensoriamento Remoto, 10 (SBSR).
Localização do EventoFoz do Iguaçu
Data21-26 abr. 2001
Editora (Publisher)INPE
Cidade da EditoraSão José dos Campos
Páginas849-858
Título do LivroAnais
Tipo TerciárioSessão Especial - Workshops
OrganizaçãoInstituto Nacional de Pesquisas Espaciais
Histórico (UTC)2006-05-12 21:30:57 :: administrator -> vinicius ::
2007-07-04 20:31:46 :: vinicius -> administrator ::
2009-06-03 14:22:38 :: administrator -> lise@dpi.inpe.br ::
2009-06-30 14:02:35 :: lise@dpi.inpe.br -> erich@sid.inpe.br ::
2010-05-14 02:50:03 :: erich@sid.inpe.br -> marciana ::
2011-02-16 12:57:51 :: marciana -> administrator :: 2001
2018-06-06 02:47:49 :: administrator -> :: 2001
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-ChaveOCEANOGRAFIA
fluxo do calor
temperatura do aceano
Experimento Topegráfico de Superfície do Oceano (NASA)
armazenamento de calor
heat flux
ocean temperature
Ekman layer
Nasa Ocean Surface Topography Expeiment (TOPEX)
heat storage
ResumoThe oceanic heat budget is a balance of heat storage rate, heat flux at the air-sea interface, and horizontal divergence of oceanic heat flux. The use of satellite altimeter data makes it possible to continuously monitor the oceanic heat flux components with unprecedented resolution in both space and time. Here we present how to estimate oceanic heat storage and Ekman heat flux from a remotely sensed data perspective. Oceanic heat storage and its time rate of change are correlated to the sea surface height anomaly signals from the TOPEX/Poseidon altimeter data. The height anomaly data are decomposed into basin-scale (seasonal), westward propagating (Rossby waves), eastward propagating (Kelvin waves), meso-scale eddies signals, and a small-scale residual. Since variability in sea surface height is mostly due to expansion and contraction of the water column it can be correlated with variations in the heat and salt content. Therefore, estimation of heat storage from altimeter data, when compared to in situ estimates, requires corrections for the haline effect. Correlations and rms differences are calculated to compare heat storage estimates based on altimeter and in situ data. The results show that heat storage anomaly can be estimated from altimeter data. For the studied regions, the haline corrections based on climatology provide equivalent or worse results than not applying a correction at all. A large fraction of the total oceanic heat flux is associated with Ekman dynamics. The high resolution and global coverage of satellite scatterometer wind data (1992-1998)is particularly well suited to resolve the various spectral bands of temporal and spatial variability associated with Ekiman layer fluxes. nI agreement with previous studies, the annual zonally integrated Ekman heat flux is poleward at latitudes lower that 30 degree and equatorward at high latitudes. A significant part of the difference between our results and previous studies can be attributed to the choice of the definition of the temperature of the Ekiman layer. The zonally averaged mean and amplitude of the annual cycle of the scatteromieter based estimates are smaller compared to climatology but similar to other satellite based estimates (SSMI). The relative importance of the zonal wind stress variability be divided in at least two major regimes at 15 degree latitude.
ÁreaSRE
TipoOceanografia
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSR > Applications of satellite...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/dpi.inpe.br/lise/2001/09.19.12.32
URL dos dados zipadoshttp://urlib.net/zip/dpi.inpe.br/lise/2001/09.19.12.32
Idiomaen
Arquivo Alvo0849.858.olga.pdf
Grupo de Usuáriosadministrator
erich@sid.inpe.br
Visibilidadeshown
5. Fontes relacionadas
Repositório Espelhodpi.inpe.br/marte@80/2007/10.17.19.59
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Divulgação<E>
Acervo Hospedeirodpi.inpe.br/banon/2003/12.10.19.30
6. Notas
Campos Vaziosarchivingpolicy archivist callnumber contenttype copyholder copyright creatorhistory descriptionlevel documentstage doi edition electronicmailaddress identifier issn lineage mark nextedition notes numberofvolumes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup readpermission resumeid rightsholder schedulinginformation secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark url versiontype volume


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