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1. Identificação
Tipo de ReferênciaArtigo em Evento (Conference Proceedings)
Sitemtc-m16d.sid.inpe.br
Identificador8JMKD3MGPDW34R/3SR2AAE
Repositóriosid.inpe.br/mtc-m16d/2019/02.27.09.11
Última Atualização2019:02.27.09.11.26 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m16d/2019/02.27.09.11.26
Última Atualização dos Metadados2020:03.15.16.29.26 (UTC) administrator
Chave de CitaçãoAraujoBritMendCint:2018:SeTeSe
TítuloSensitivity test for sea ice thickness simulated by punctual model on the weddell sea
FormatoOn-line.
Ano2018
Data de Acesso19 maio 2024
Tipo SecundárioPRE CN
Número de Arquivos1
Tamanho147 KiB
2. Contextualização
Autor1 Araujo, Glicia Ruth Garcia De
2 Brito Neto, Francisco Agustinho De
3 Mendes, David
4 Cintra, Márcio Machado
Endereço de e-Mail do Autor1 glicia.garcia123@gmail.com
EditorHerdies, Dirceu Luis
Coelho, Simone Marilene Sievert da Costa
Endereço de e-Mailfrancisco.brito@inpe.br
Nome do EventoEncontro dos alunos de pós-graduação em meteorologia do CPTEC/INPE, 17 (EPGMET)
Localização do EventoCachoeira Paulista
Data22-26 out. 2018
Editora (Publisher)Instituto Nacional de Pesquisas Espaciais (INPE)
Cidade da EditoraSão José dos Campos
Título do LivroAnais
Tipo Terciárioabstract
OrganizaçãoInstituto Nacional de Pesquisas Espaciais (INPE)
Histórico (UTC)2019-02-27 09:11:26 :: francisco.brito@inpe.br -> administrator ::
2020-03-15 16:29:26 :: administrator -> francisco.brito@inpe.br :: 2018
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Palavras-ChaveWeddell Sea
Model
Balance Energy
ResumoIn a basic definition, the sea ice is resulted from the freezing of the sea water. The growth is ruled by the energy balance on the upper and lower surfaces of the sea ice. The freezing and melting dynamics occurs with heat transfering throughout the mass of ice from its center towards surface.Therefore, the numerical models standing for the Sea Ice Thickness represent the ice column divided in several layers, in order to calculate the thermal conductivity between those layers. The objective of this study is to identify the maximum number of layers required to represent the Sea Ice Thickness in the Southern Ocean. The study area is on the Weddell Sea (WS), located between latitudes 83°S/55°S and longitudes 84°W/10°E. The simulations of Sea Ice Thickness, Snow Thickness and Air Temperature were performed in 2009 to 2017 for two distinct points on the WS, being the first denominated PT1 (classified as undefined, because of the presence or absence of ice depending on the time of year in which data were acquired) and Gekstaller (classified as permanent ice layer). For each point 20 simulations were realized. Daily flows, named Latent Heat, Sensitive Heat, Long Wave Radiation, Shortwave Radiation and Albedo from the National Centers for Environmental Prediction (NCEP), were used as input data. In PT1 a greater variation in radioactive closure was observed , and larger changes in Sea Ice Thickness in relation to the point Gekstaller. In all PT1 layers, high values of Snow Thickness, mainly in layers 1, 2, 3 and 4, were obtained in the first years of. The model represented reasonably well the Air Temperature in the two selected points, being, the temperatures between 0 and -40°C in the Gekstaller station, whereas they varied between 0 and -30°C in the PT1, as this location is in higher latitudes. In addition, the model was able to represent the seasonality of temperature in the simulated points. The layer 1 in PT1 obtained lower Air Temperature values in relation to the other layers, which led to a greater Sea Ice Thickness in layer 1. As main conclusion, the punctual model showed stability, with no great variations in the Sea Ice Thickness in the five layers. At the Gekstaller point, which is characterized by a permanent ice layer, the simulations did not show great changes in the Sea Ice Thickness. This occurs because snow serves as an insulator, as indicated by the melting rate in this this region lower than the deposition rate.
ÁreaMET
TipoModelagem Geral
Arranjo 1urlib.net > BDMCI > Fonds > WETEs > XVII EPGMET > Sensitivity test for...
Arranjo 2urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > XVII EPGMET > Sensitivity test for...
Arranjo 3urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > XVII EPGMET > Sensitivity test for...
Arranjo 4urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDSA > XVII EPGMET > Sensitivity test for...
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/8JMKD3MGPDW34R/3SR2AAE
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGPDW34R/3SR2AAE
Idiomapt
Arquivo AlvoMG2-10.pdf
Grupo de Usuáriosfrancisco.brito@inpe.br
Visibilidadeshown
Licença de Direitos Autoraisurlib.net/www/2012/11.12.15.19
Detentor dos Direitosoriginalauthor yes
Permissão de Leituraallow from all
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGP3W34P/3SR8FCH
Lista de Itens Citandosid.inpe.br/mtc-m21b/2019/02.28.19.01 5
Acervo Hospedeirosid.inpe.br/mtc-m19@80/2009/08.21.17.02
6. Notas
Campos Vaziosaffiliation archivingpolicy archivist callnumber contenttype copyholder creatorhistory descriptionlevel dissemination doi edition group holdercode isbn issn label lineage mark mirrorrepository nextedition notes numberofvolumes orcid pages parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid schedulinginformation secondarydate secondarykey secondarymark serieseditor shorttitle sponsor tertiarymark url versiontype volume
7. Controle da descrição
e-Mail (login)francisco.brito@inpe.br
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