1. Identificação | |
Tipo de Referência | Artigo em Evento (Conference Proceedings) |
Site | mtc-m12.sid.inpe.br |
Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identificador | 6qtX3pFwXQZ3r59YD6/GPajP |
Repositório | sid.inpe.br/iris@1912/2005/07.20.05.02 |
Última Atualização | 2015:12.10.14.02.39 (UTC) marciana |
Repositório de Metadados | sid.inpe.br/iris@1912/2005/07.20.05.02.50 |
Última Atualização dos Metadados | 2018:06.05.00.52.37 (UTC) administrator |
Chave Secundária | INPE-6314-PRE/2402 |
Rótulo | 8636 |
Chave de Citação | StevensonSouz:1994:HeTrSu |
Título | Heat transport in the surface layer east of the drake passage estimated from a woce drifter-firs results |
Ano | 1994 |
Data Secundária | 20000104 |
Data de Acesso | 12 maio 2024 |
Tipo Secundário | PRE CN |
Número de Arquivos | 1 |
Tamanho | 449 KiB |
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2. Contextualização | |
Autor | 1 Stevenson, Merritt Raymond 2 Souza, Ronald Bus |
Grupo | 1 DSR-INPE-MCT-BR |
Nome do Evento | Conferencia Latinoamericana sobre Ciencias Espaciais e Atmosfericas na Antartica (CLACEAA). |
Localização do Evento | Serra Negra, BR |
Data | 20-25 nov. 1994 |
Editora (Publisher) | Transtec Editorial |
Cidade da Editora | Sao Jose dos campos |
Páginas | 117-130 |
Organização | Instituto Nacional de Pesquisas Espaciais |
Histórico (UTC) | 2008-06-09 21:46:20 :: administrator -> jefferson :: 2010-07-07 18:51:34 :: jefferson -> administrator :: 2015-02-26 11:55:18 :: administrator -> marciana :: 1994 2015-12-10 14:02:39 :: marciana -> administrator :: 1994 2016-06-04 23:29:30 :: administrator -> marciana :: 1994 2016-08-18 17:08:54 :: marciana -> administrator :: 1994 2018-06-05 00:52:37 :: administrator -> marciana :: 1994 |
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3. Conteúdo e estrutura | |
É a matriz ou uma cópia? | é a matriz |
Estágio do Conteúdo | concluido |
Transferível | 1 |
Tipo do Conteúdo | External Contribution |
Palavras-Chave | OCEANOGRAFIA ANTARTICA GELO ANTARTICO ZONA DE CONVERGENCIA ANTARTICA MEDICA TRANSFERENCIA DE CALOR EXPEDICAO BRASILEIRA ANTARTICA |
Resumo | With the objective of studying the meridional and zonal variation In the surface layer current and Its heat transport on the north side of the Polar Front In the Antarctic Convergence Zone, a WOCE (World Ocean Circulation Experiment)standard, surface layer drifter was launched at 56.1 degree S,55 degree W during the 12th Brazilian Antarctic Expedition. A southbound meridional transact of XBT vertical profiles was used to locate the "1.5 degree C thermal wall" of the Polar Front. From its 13 november. 1993 launch date, the drifter has been tracked by DCLS ARGOS aboard the operational NOAA satellites. Sea surface temperatures (SSTs)were also measured to a precision of about 0.12 degree C from the drifter. Although the drifter was still transmitting data at the end of September 1994, the first 300 days of the drifter's trajectory and SST time series are used In this report. The drifter's trajectory contained meanders and occasional loops throughout the 300 days, moving generally northeasterly until It reached 47 degree S,42 degree W, whereupon the trajectory became almost easterly. The overall mean velocity of the drifter was 11.2 cm/s toward 069 degree, the meridional component was 4.0 cm/s to the north. The mean surface temperature was 6.01 degree C. The unit heat transport at the surface of the 0-15m depth surface layer was estimated by the heat contained In this water column of uniform temperature and horizontal velocity. The temperature and displacement series were partitioned Into 6 time bins of 50 days each, to obtain the mean zonal and meridionall currents and mean surface temperature for each bin. The surface layer mean heat transport was to the north at 10.63X10 4 w/m per zonal meter, or 3.13 x10 11 w/m over the zonal distance of 2,950km. By contrast, zonal heat transport was eastward at 15.75x10 4 watts/m per meridional meter, or 2.47x10 11 w/m between 57.2 degree S and 44.2 degree S.The values of unit heat transport determined In this study are about double the heat transports noted In the literature. Differences In the methods used to determine the heat transports and the fact that the present study used data from only the surface layer, are considered to be the reasons for the larger value determined In this study. |
Área | SRE |
Arranjo | urlib.net > DIDSR > Heat transport in... |
Conteúdo da Pasta doc | acessar |
Conteúdo da Pasta source | não têm arquivos |
Conteúdo da Pasta agreement | não têm arquivos |
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4. Condições de acesso e uso | |
URL dos dados | http://urlib.net/ibi/6qtX3pFwXQZ3r59YD6/GPajP |
URL dos dados zipados | http://urlib.net/zip/6qtX3pFwXQZ3r59YD6/GPajP |
Arquivo Alvo | INPE 6314.pdf |
Grupo de Usuários | administrator marciana |
Grupo de Leitores | administrator marciana |
Visibilidade | shown |
Permissão de Leitura | allow from all |
Permissão de Atualização | não transferida |
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5. Fontes relacionadas | |
Unidades Imediatamente Superiores | 8JMKD3MGPCW/3ER446E |
Lista de Itens Citando | sid.inpe.br/bibdigital/2013/09.13.21.11 1 |
Acervo Hospedeiro | sid.inpe.br/banon/2001/04.06.10.52 |
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6. Notas | |
Campos Vazios | affiliation archivingpolicy archivist booktitle callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor electronicmailaddress format isbn issn language lineage mark mirrorrepository nextedition notes numberofvolumes orcid parameterlist parentrepositories previousedition previouslowerunit progress project resumeid rightsholder schedulinginformation secondarymark serieseditor session shorttitle sponsor subject tertiarymark tertiarytype type url versiontype volume |
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7. Controle da descrição | |
e-Mail (login) | marciana |
atualizar | |
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