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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m12.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZ3r59YD6/GPbt2
Repositóriosid.inpe.br/iris@1912/2005/07.20.05.56   (acesso restrito)
Última Atualização2016:03.15.15.39.06 (UTC) marciana
Repositório de Metadadossid.inpe.br/iris@1912/2005/07.20.05.57
Última Atualização dos Metadados2018:06.05.00.52.39 (UTC) administrator
Chave SecundáriaINPE-8155-PRE/3962
Rótulo6956
Chave de CitaçãoViannaKamp:1995:HiReSt
TítuloA high resolution study of the dynamics of Atlantic SST fields
Ano1995
Data Secundária19940720
Data de Acesso11 maio 2024
Tipo SecundárioPRE CI
Número de Arquivos1
Tamanho766 KiB
2. Contextualização
Autor1 Vianna, Marcio Luiz
2 Kampel, Milton
Grupo1 DSR-INPE-MCT-BR
Nome do EventoInternational Scientific Conference on the Tropical ocean Global Atmosphere (TOGA) Programme.
Localização do EventoMelbourne, AU
Data2-7 Apr. 1995
Páginas20-24
Título do LivroProceedings
Histórico (UTC)2008-06-09 21:47:01 :: administrator -> jefferson ::
2010-07-07 18:51:51 :: jefferson -> administrator ::
2015-05-22 13:47:15 :: administrator -> marciana :: 1995
2016-03-15 15:39:06 :: marciana -> administrator :: 1995
2018-06-05 00:52:39 :: administrator -> marciana :: 1995
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveOCEANOGRAFIA
CLIMATOLOGIA
ATMOSFERA EQUATORIAL
REGIOES TROPICAIS
PROGRAMA DE PESQUISA DA TMOSFERA GLOBAL
CLIMATOLOGY
EQUATORIAL ATMOSPHERE
TROPICAL REGIONS
GLOBAL ATMOSPHERIC RESEARCH PROGRAMA
GARP
ResumoOne of the great successes of the TOGA Program consisted in establishing the central role of equatorial upper ocean motions in the determination of the time scales of ENSO variability. The role of equatorial Pacific ocean currents in the redistribution of heat content, determined by data from the Sea-Level Network, has been confirmed by other monitoring systems, prominent among these the TOGA-TAO Array. Predictability of the propagation of SST anomalies via coupled intermediate ocean-atmosphere models and statistical models has been feasible due to the good data base now available. For the western tropical Atlantic, we may cite two strong interannual variabilities of socio-economic importance which would profit from good prediction systems: the climatic drought-flood episodes, and the large fluctuations in lobster fisheries yields (Vianna, this volume), both impacting in the Brazilian Nordeste. Among the most recent efforts to relate ENSO episodeswith Atlantic Warm Events, we may cite the model study by Delecluse et al.(1994)as very relevant, due to its approach in trying to relate ENSO-driven Atlantic wind-stress perturbations to forced dynamics of the equatorial Atlantic, which to a large degree should determine the SST anomaly field several months later. The SST anomalies in the southeastern Tropical Atlantic by the end of a typical year, driven by wind-stress anomalies around May-July in the western basin, would in turn determine the nature of the rainfall season in Nordeste in the subsequent year, and the nature of the fisheries yields 6 years later. One of the main difficulties in testing present-day ideas and model results on interannual variability in Atlantic Ocean circulation is the lack of a detailed understanding of the spatial structures one might expect to find in the South Tropical Atlantic. The prior knowledge of the upper ocean currents, usually of of 50-150 m in horizontal cross-section (Molinari, 1982, and references therein), is required for the design and implementation of a TAO-Array which could provide the basic data for model testing and validation. This knowledge cannot be obtained significantly only by use of data from COADS, the Servain data set and the SEQUAL-FOCAL data due to insufficient resolution. On the other hand, advection of Indian Ocean thermocline water into the South Atlantic could in principle introduce interannual signals to the north. The present study represents an effort to obtain some answers to specific questions on the largescale dynamics of Atlantic SST fields which can only be obtained by long-term, higher resolution data sets. These questions maybe summarized by the follwing ing one: What are the specific spatial SST anomaly structures that relate with known circulation, and what are the time scales of their variabilite?.
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4. Condições de acesso e uso
Arquivo AlvoINPE 8155.pdf
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Permissão de Leituradeny from all
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ER446E
Acervo Hospedeirosid.inpe.br/banon/2001/04.06.10.52
6. Notas
Campos Vaziosaffiliation archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor electronicmailaddress format isbn issn language lineage mark mirrorrepository nextedition notes numberofvolumes orcid organization parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress resumeid rightsholder schedulinginformation secondarymark serieseditor session shorttitle sponsor subject tertiarymark tertiarytype type url versiontype volume
7. Controle da descrição
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