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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m21c.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador8JMKD3MGP3W34R/449MDCH
Repositóriosid.inpe.br/mtc-m21c/2021/03.04.16.46
Última Atualização2021:03.18.16.56.03 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m21c/2021/03.04.16.46.22
Última Atualização dos Metadados2022:04.03.22.28.18 (UTC) administrator
DOI10.3390/atmos12020240
ISSN2073-4433
Chave de CitaçãoCarneiroFiNeSaSaBo:2021:NoBoLa
TítuloNocturnal boundary layer erosion analysis in the amazon using large-eddy simulation during goamazon project 2014/5
Ano2021
MêsFeb.
Data de Acesso20 maio 2024
Tipo de Trabalhojournal article
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho28804 KiB
2. Contextualização
Autor1 Carneiro, Rayonil Gomes
2 Fisch, Gilberto
3 Neves, Theomar
4 Santos, Rosa
5 Santos, Carlos
6 Borges, Camilla
ORCID1 0000-0003-4403-0191
2 0000-0001-6668-9988
3
4
5 0000-0003-2414-2911
Grupo1 CST-CST-DIPGR-INPE-MCTI-GOV-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade de Taubaté (UNITAU)
3 Universidade Federal do Oeste do Pará (UFOPA)
4 Universidade do Estado do Amazonas (UEA)
5 Universidade Federal de Camina Grande (UFCG)
6 Universidade Federal de Camina Grande (UFCG)
Endereço de e-Mail do Autor1 rayonil.carneiro@inpe.br
2 gilberto.fisch@unitau.br
3 theomar.neves@ufopa.edu.br
4 rmsantos@uea.edu.br
5 carlos.santos@ufcg.edu.br
6 camillakassar@gmail.com
RevistaAtmosphere
Volume12
Número2
Páginase240
Nota SecundáriaB3_ENGENHARIAS_III B3_ENGENHARIAS_I B3_CIÊNCIAS_AMBIENTAIS B4_ENGENHARIAS_II B5_GEOCIÊNCIAS
Histórico (UTC)2021-03-04 16:46:22 :: simone -> administrator ::
2021-03-04 16:46:24 :: administrator -> simone :: 2021
2021-03-18 16:56:04 :: simone -> administrator :: 2021
2022-04-03 22:28:18 :: administrator -> simone :: 2021
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-Chaveplanetary boundary layer
kinematic heat flux
PALM model
ResumoThis study investigated the erosion of the nocturnal boundary layer (NBL) over the central Amazon using a high-resolution model of large-eddy simulation (LES) named PArallel Les Model (PALM) and observational data from Green Ocean Amazon (GoAmazon) project 2014/5. This data set was collected during four intense observation periods (IOPs) in the dry and rainy seasons in the years 2014 (considered a typical year) and 2015, during which an El Niño-Southern Oscillation (ENSO) event predominated and provoked an intense dry season. The outputs from the PALM simulations represented reasonably well the NBL erosion, and the results showed that it has different characteristics between the seasons. During the rainy season, the IOPs exhibited slow surface heating and less intense convection, which resulted in a longer erosion period, typically about 3 h after sunrise (that occurs at 06:00 local time). In contrast, dry IOPs showed more intensive surface warming with stronger convection, resulting in faster NBL erosion, about 2 h after sunrise. A conceptual model was derived to investigate the complete erosion during sunrise hours when there is a very shallow mixed layer formed close to the surface and a stable layer above. The kinematic heat flux for heating this layer during the erosion period showed that for the rainy season, the energy emitted from the surface and the entrainment was not enough to fully heat the NBL layer and erode it. Approximately 30% of additional energy was used in the system, which could come from the release of energy from biomass. The dry period of 2014 showed stronger heating, but it was also not enough, requiring approximately 6% of additional energy. However, for the 2015 dry period, which was under the influence of the ENSO event, it was shown that the released surface fluxes were sufficient to fully heat the layer. The erosion time of the NBL probably influenced the development of the convective boundary layer (CBL), wherein greater vertical development was observed in the dry season IOPs (~1500 m), while the rainy season IOPs had a shallower layer (~1200 m).
ÁreaCST
Arranjo 1urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > CST > Nocturnal boundary layer...
Arranjo 2urlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > Nocturnal boundary layer...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreement
agreement.html 04/03/2021 13:46 1.0 KiB 
4. Condições de acesso e uso
URL dos dadoshttp://urlib.net/ibi/8JMKD3MGP3W34R/449MDCH
URL dos dados zipadoshttp://urlib.net/zip/8JMKD3MGP3W34R/449MDCH
Idiomaen
Arquivo Alvoatmosphere-12-00240-v2.pdf
Grupo de Usuáriossimone
Grupo de Leitoresadministrator
simone
Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/449U4PL
8JMKD3MGPCW/46KUATE
Lista de Itens Citandosid.inpe.br/bibdigital/2022/04.03.22.23 4
sid.inpe.br/bibdigital/2021/03.06.05.18 4
DivulgaçãoWEBSCI; PORTALCAPES; SCOPUS.
Acervo Hospedeirourlib.net/www/2017/11.22.19.04
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes parameterlist parentrepositories previousedition previouslowerunit progress project readpermission resumeid rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url
7. Controle da descrição
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