1. Identificação | |
Tipo de Referência | Artigo em Revista Científica (Journal Article) |
Site | plutao.sid.inpe.br |
Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identificador | 8JMKD3MGP3W/3RAQR4H |
Repositório | sid.inpe.br/plutao/2018/06.19.04.19 (acesso restrito) |
Última Atualização | 2018:06.19.15.08.45 (UTC) lattes |
Repositório de Metadados | sid.inpe.br/plutao/2018/06.19.04.19.03 |
Última Atualização dos Metadados | 2019:01.14.17.09.18 (UTC) administrator |
DOI | 10.1016/j.dsr2.2018.02.013 |
ISSN | 0967-0645 |
Rótulo | lattes: 0537824080913130 2 SantiniSouzWainMuel:2018:TeAnWa |
Chave de Citação | SantiniSouzWainMuel:2018:TeAnWa |
Título | Temporal analysis of water masses and sea ice formation rate west of the Antarctic Peninsula in 2008 estimated from southern elephant seals' SRDL-CTD data |
Ano | 2018 |
Data de Acesso | 10 maio 2024 |
Tipo de Trabalho | journal article |
Tipo Secundário | PRE PI |
Número de Arquivos | 1 |
Tamanho | 1598 KiB |
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2. Contextualização | |
Autor | 1 Santini, Marcelo Freitas 2 Souza, Ronald Buss de 3 Wainer, Ilana 4 Muelbert, Mônica M. |
Identificador de Curriculo | 1 2 8JMKD3MGP5W/3C9JJ6U |
Grupo | 1 SER-SRE-SESPG-INPE-MCTIC-GOV-BR 2 CRCRS-COCRE-INPE-MCTIC-GOV-BR |
Afiliação | 1 Instituto Nacional de Pesquisas Espaciais (INPE) 2 Instituto Nacional de Pesquisas Espaciais (INPE) 3 Universidade de São Paulo (USP) 4 Universidade Federl do Rio Grande (FURG) |
Endereço de e-Mail do Autor | 1 marcelo.santini@inpe.br 2 ronald.buss@inpe.br |
Revista | Deep-Sea Research Part Ii-Topical Studies In Oceanography |
Volume | 149 |
Páginas | 58-69 |
Histórico (UTC) | 2018-06-19 04:19:03 :: lattes -> administrator :: 2018-06-19 15:06:39 :: administrator -> lattes :: 2018 2018-06-19 15:08:47 :: lattes -> administrator :: 2018 2019-01-14 17:09:18 :: administrator -> simone :: 2018 |
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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 |
Tipo de Versão | publisher |
Palavras-Chave | massas de agua Oceano Austral taxa de formação de gelo marinho water masses sea ice formation rate SRDL-CTD Antarctic peninsula |
Resumo | As an alternative method to collect oceanographic data in the polar oceans, especially during winter when traditional methods are very difficult to be used, sea mammals can be tagged with Satellite Relay Data Loggers with CTD capabilities (SRDLCTD). Using data from nine southern elephant seals (SES; Mirounga leonina) tagged during a field campaign of the MEOPBR project (the Brazilian Counterpart to the Marine Mammal Exploration of the Oceans Pole to Pole), this work presents a temporal analysis of the water masses and the sea ice formation rate at the western part of the Antarctic Peninsula (AP) during 2008. We found that the seasonal and local processes controlling the surface and intermediate layers of the ocean produced differences in the water mass composition and the sea ice formation rates in our study region. Sea ice formation rates ranged from less than 1 cm/day in deep sea waters off the northern part of the AP to 14 cm/day at the vicinity of ice shelves such as the Abbot and Wilkins ice shelves, further south in the AP. Maximum sea ice formation rates, as expected, occurred during autumn to winter. After the successive collapse events of the Wilkins Ice Shelf (WIS) in 2008, the sea ice formation rate endured significant reductions even when sea ice concentrations were high in the region. These reductions, observed by SES in the vicinity of WIS can be associated with freshwater input derived from shelf collapses. The presence of the Circumpolar Deep Water (CDW) over the continental shelf west of the AP affected the sea ice formation rate by both contributing to the observed low sea ice coverage and to the acceleration of the ice shelf melting. Another process that demonstrated influence on the formation of sea ice was the advection of more saline waters in the oceanic layer considered here for the application of salt balance equation. This advection resulted in unrealistic sea ice formation rates in regions where there was no sea ice cover. The data and results presented here can be used to feed and to validate climate oceanatmosphere coupled models. The data can be combined with other (more traditional) meteorological and oceanographic data in order to provide a better understanding of both oceanic and oceanatmosphere coupled processes yet not very well known in our study region. |
Área | SRE |
Arranjo 1 | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > CRCRS > Temporal analysis of... |
Arranjo 2 | urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > SER > Temporal analysis of... |
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 | |
Idioma | en |
Arquivo Alvo | santini_temporal.pdf |
Grupo de Usuários | lattes |
Grupo de Leitores | administrator lattes |
Visibilidade | shown |
Política de Arquivamento | denypublisher denyfinaldraft24 |
Permissão de Leitura | deny from all and allow from 150.163 |
Permissão de Atualização | não transferida |
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5. Fontes relacionadas | |
Unidades Imediatamente Superiores | 8JMKD3MGPCW/3EUFCFP 8JMKD3MGPCW/3F3NU5S |
Lista de Itens Citando | sid.inpe.br/bibdigital/2013/10.18.22.34 2 sid.inpe.br/mtc-m21/2012/07.13.14.59.32 1 |
Divulgação | WEBSCI; PORTALCAPES; SCOPUS. |
Acervo Hospedeiro | dpi.inpe.br/plutao@80/2008/08.19.15.01 |
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6. Notas | |
Campos Vazios | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn lineage mark mirrorrepository month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey secondarymark session shorttitle sponsor subject tertiarymark tertiarytype url |
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7. Controle da descrição | |
e-Mail (login) | simone |
atualizar | |
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