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1. Identificação
Tipo de ReferênciaArtigo em Revista Científica (Journal Article)
Sitemtc-m16b.sid.inpe.br
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identificador6qtX3pFwXQZGivnK2Y/UuLha
Repositóriosid.inpe.br/mtc-m17@80/2008/06.18.12.10   (acesso restrito)
Última Atualização2008:06.18.12.10.57 (UTC) administrator
Repositório de Metadadossid.inpe.br/mtc-m17@80/2008/06.18.12.10.59
Última Atualização dos Metadados2018:06.05.03.30.52 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.1016/j.asr.2008.03.027
ISSN0273-1177
Chave de CitaçãoSimonichCeme:2008:CoDiLa
TítuloSporadic sodium layers and the average vertical distribution of atmospheric sodium: Comparison of different Nas layer strengths
Ano2008
MêsJuly
Data de Acesso29 abr. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho149 KiB
2. Contextualização
Autor1 Simonich, Dale Martin
2 Cemesha, Barclay Robert
Identificador de Curriculo1 8JMKD3MGP5W/3C9JGT2
Grupo1 DAE-CEA-INPE-MCT-BR
2 DAE-CEA-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
RevistaAdvances in Space Research
Volume42
Número1
Páginas229-233
Histórico (UTC)2008-06-18 12:10:59 :: simone -> administrator ::
2012-07-13 22:33:06 :: administrator -> simone :: 2008
2013-02-20 15:20:20 :: simone -> administrator :: 2008
2018-06-05 03:30:52 :: administrator -> marciana :: 2008
3. Conteúdo e estrutura
É a matriz ou uma cópia?é a matriz
Estágio do Conteúdoconcluido
Transferível1
Tipo do ConteúdoExternal Contribution
Palavras-ChaveSporadic sodium
Mesospheric sodium
LIDAR
ResumoIn an earlier study of sporadic sodium layers (Nas) [Simonich, D.M., Clemesha B.R., Batista, P.P. Sporadic layers and the vertical distribution of atmospheric sodium. Adv. Space Res. 35, 19761980, 2005], observed by lidar at São José do Campos (23°S, 46°W) we found that, although individual profiles give the impression that Nas layers involve sodium additional to the normal background layer, there is very little difference between the long-term averages of profiles with and without the presence of Nas. This led us to conclude that Nas layers result from the redistribution of an omnipresent source, rather than an additional source mechanism. We have now extended this study to investigate whether or not the relative magnitude of Nas layers influences this conclusion. To this end we manually characterized all the profiles obtained in the time interval from 1900 to 2200 LT for the years 19932004. This involved registering the upper and lower limits to each Nas layer observed, the height of the peak and the sodium concentration at each of these three points. We then computed average profiles for Nas layers of differing strengths, with strength defined as the concentration at the peak divided by the mean of the concentrations at the upper and lower boundaries. For strengths up to 4 the results confirmed our earlier conclusion but for Nas layer strengths greater than 4 we found a significant difference between the average profiles with and without Nas. For the strong Nas layers both the average abundance and the average peak sodium concentration were about 10% greater than for layers without Nas. This leads to the possibility that a different mechanism might be responsible for very stronger sporadic layers although we do not think this very likely.
ÁreaCEA
ArranjoSporadic sodium layers...
Conteúdo da Pasta docacessar
Conteúdo da Pasta sourcenão têm arquivos
Conteúdo da Pasta agreementnão têm arquivos
4. Condições de acesso e uso
Idiomaen
Arquivo Alvosporadic sodium.pdf
Grupo de Usuáriosadministrator
simone
Visibilidadeshown
Política de Arquivamentodenypublisher denyfinaldraft24
Permissão de Leituradeny from all and allow from 150.163
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ETL868
DivulgaçãoWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Acervo Hospedeirolcp.inpe.br/ignes/2004/02.12.18.39
cptec.inpe.br/walmeida/2003/04.25.17.12
6. Notas
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel documentstage e-mailaddress electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Controle da descrição
e-Mail (login)marciana
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