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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
IdentificadorJ8LNKAN8RW/39RQDNR
Repositóriodpi.inpe.br/plutao/2011/06.11.03.26.29
Última Atualização2011:12.06.17.02.26 (UTC) administrator
Repositório de Metadadosdpi.inpe.br/plutao/2011/06.11.03.26.30
Última Atualização dos Metadados2018:06.05.00.01.19 (UTC) administrator
Chave SecundáriaINPE--PRE/
DOI10.5194/acp-11-12137-2011
ISSN1680-7316
Rótulolattes: 2306964700488382 3 BagestonWrBaEFrGoAn:2011:ObMeFr
Chave de CitaçãoBagestonWrBaEFrGoAn:2011:ObMeFr
TítuloObservation of a mesospheric front in a dual duct over King George Island, Antarctica
Ano2011
Data de Acesso26 jun. 2024
Tipo SecundárioPRE PI
Número de Arquivos1
Tamanho780 KiB
2. Contextualização
Autor1 Bageston, José Valentin
2 Wrasse, Cristiano Max
3 Batista, Paulo Prado
4 E, Hibbins R
5 Fritts, David C.
6 Gobbi, Delano
7 Andrioli, Vânia Fátima
Identificador de Curriculo1
2
3 8JMKD3MGP5W/3C9JJ3H
4
5
6 8JMKD3MGP5W/3C9JGTE
Grupo1
2
3 DAE-CEA-INPE-MCT-BR
4
5
6 DAE-CEA-INPE-MCT-BR
Afiliação1
2 VSE, Sao Jose Dos Campos, Brazil
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Norwegian Univ Sci & Technol, N-7034 Trondheim, Norway
5 Colorado Res Associates CoRA, Boulder, CO USA
6 Instituto Nacional de Pesquisas Espaciais (INPE)
Endereço de e-Mail do Autor1
2
3 ppbatista@laser.inpe.br
Endereço de e-Mailppbatista@laser.inpe.br
RevistaAtmospheric Chemistry and Physics
Volume11
Número23
Páginas12137-12147
Nota SecundáriaA2_ASTRONOMIA_/_FÍSICA A1_ENGENHARIAS_II A1_ENGENHARIAS_III A1_GEOCIÊNCIAS A1_INTERDISCIPLINAR
Histórico (UTC)2011-06-11 17:43:44 :: lattes -> administrator :: 2011
2011-07-26 13:05:10 :: administrator -> marciana :: 2011
2011-11-01 11:21:21 :: marciana -> tereza@sid.inpe.br :: 2011
2011-12-06 17:02:27 :: tereza@sid.inpe.br -> administrator :: 2011
2012-07-25 15:50:44 :: administrator -> banon :: 2011
2012-09-21 14:41:37 :: banon -> administrator :: 2011
2012-10-19 20:25:35 :: administrator -> tereza@sid.inpe.br :: 2011
2013-02-04 12:37:55 :: tereza@sid.inpe.br -> administrator :: 2011
2018-06-05 00:01:19 :: administrator -> tereza@sid.inpe.br :: 2011
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-Chavegravity-wave event
airglow emissions
62-degrees s
bore event
OH
climatology
atmosphere
campaign
station
region
ResumoA mesospheric front was observed with an all-sky airglow imager on the night of 9-10 July 2007 at Ferraz Station (62 degrees S, 58 degrees W), located on King George island on the Antarctic Peninsula. The observed wave propagated from southwest to northeast with a well defined wave front and a series of crests behind the main front. The wave parameters were obtained via a 2-D Fourier transform of the imager data providing a horizontal wavelength of 33 km, an observed period of 6 min, and a horizontal phase speed of 92ms(-1). Simultaneous mesospheric winds were measured with a medium frequency (MF) radar at Rothera Station (68 degrees S, 68 degrees W) and temperature profiles were obtained from the SABER instrument on the TIMED satellite. These wind and temperature profiles were used to estimate the propagation environment of the wave event. A wavelet technique was applied to the wind in the plane of wave propagation at the OH emission height spanning three days centered on the front event to define the dominant periodicities. Results revealed a dominance of near-inertial periods, and semi-diurnal and terdiurnal tides suggesting that the ducting structure enabling mesospheric front propagation occurred on large spatial scales. The observed tidal motions were used to reconstruct the winds employing a least-squares method, which were then compared to the observed ducting environment. Results suggest an important contribution of large-scale winds to the ducting structure, but with buoyancy frequency variations in the vertical also expected to be important. These results allow us to conclude that the wave front event was supported by a duct including contributions from both winds and temperature.
ÁreaCEA
Arranjourlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Observation of a...
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/J8LNKAN8RW/39RQDNR
URL dos dados zipadoshttp://urlib.net/zip/J8LNKAN8RW/39RQDNR
Idiomaen
Arquivo AlvoBageston-acpd-11-16185-206-2011[1].pdf
Grupo de Usuáriosadministrator
banon
lattes
marciana
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Grupo de Leitoresadministrator
tereza@sid.inpe.br
Visibilidadeshown
Política de Arquivamentoallowpublisher allowfinaldraft
Permissão de Atualizaçãonão transferida
5. Fontes relacionadas
Unidades Imediatamente Superiores8JMKD3MGPCW/3ETL868
Lista de Itens Citandosid.inpe.br/bibdigital/2013/09.29.20.43 4
sid.inpe.br/mtc-m21/2012/07.13.14.58 2
sid.inpe.br/mtc-m21/2012/07.13.14.44.27 1
DivulgaçãoWEBSCI; PORTALCAPES; AGU.
Acervo Hospedeirodpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notas
NotasSetores de Atividade: Pesquisa e desenvolvimento científico.
Campos Vaziosalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn lineage mark mirrorrepository month nextedition orcid parameterlist parentrepositories previousedition previouslowerunit progress project readpermission rightsholder schedulinginformation secondarydate session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Controle da descrição
e-Mail (login)tereza@sid.inpe.br
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