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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Siteplutao.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W/3RAQR4H
Repositóriosid.inpe.br/plutao/2018/06.19.04.19   (acesso restrito)
Última Atualização2018:06.19.15.08.45 (UTC) lattes
Repositório de Metadadossid.inpe.br/plutao/2018/06.19.04.19.03
Última Atualização dos Metadados2019:01.14.17.09.18 (UTC) administrator
DOI10.1016/j.dsr2.2018.02.013
ISSN0967-0645
Rótulolattes: 0537824080913130 2 SantiniSouzWainMuel:2018:TeAnWa
Chave de CitaçãoSantiniSouzWainMuel:2018:TeAnWa
TítuloTemporal analysis of water masses and sea ice formation rate west of the Antarctic Peninsula in 2008 estimated from southern elephant seals' SRDL-CTD data
Ano2018
Data de Acesso10 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho1598 KiB
2. Contextualização
Autor1 Santini, Marcelo Freitas
2 Souza, Ronald Buss de
3 Wainer, Ilana
4 Muelbert, Mônica M.
Identificador de Curriculo1
2 8JMKD3MGP5W/3C9JJ6U
Grupo1 SER-SRE-SESPG-INPE-MCTIC-GOV-BR
2 CRCRS-COCRE-INPE-MCTIC-GOV-BR
Afiliação1 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 Autor1 marcelo.santini@inpe.br
2 ronald.buss@inpe.br
RevistaDeep-Sea Research Part Ii-Topical Studies In Oceanography
Volume149
Páginas58-69
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
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Tipo de Versãopublisher
Palavras-Chavemassas de agua
Oceano Austral
taxa de formação de gelo marinho
water masses
sea ice formation rate
SRDL-CTD
Antarctic peninsula
ResumoAs 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.
ÁreaSRE
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Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvosantini_temporal.pdf
Grupo de Usuárioslattes
Grupo de Leitoresadministrator
lattes
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3EUFCFP
8JMKD3MGPCW/3F3NU5S
Lista de Itens Citandosid.inpe.br/bibdigital/2013/10.18.22.34 2
sid.inpe.br/mtc-m21/2012/07.13.14.59.32 1
DivulgaçãoWEBSCI; PORTALCAPES; SCOPUS.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
Campos Vaziosalternatejournal 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
7. Controle da descrição
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