1. Identificação | |
Tipo de Referência | Artigo em Revista Científica (Journal Article) |
Site | mtc-m16.sid.inpe.br |
Código do Detentor | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S |
Identificador | 6qtX3pFwXQZGivnJVY/LsoHL |
Repositório | sid.inpe.br/mtc-m16@80/2006/06.14.18.16 (acesso restrito) |
Última Atualização | 2006:06.14.18.16.19 (UTC) administrator |
Repositório de Metadados | sid.inpe.br/mtc-m16@80/2006/06.14.18.16.20 |
Última Atualização dos Metadados | 2021:07.18.04.01.22 (UTC) administrator |
Chave Secundária | INPE--13780-PRE/8966 |
ISSN | 1364-6826 |
Chave de Citação | WrasseSAANTTMTGS:2006:ReRaTr |
Título | Reverse ray tracing of the mesospheric gravity waves observed at 23°S (Brazil) and 7°S (Indonesia) in airglow imagers |
Ano | 2006 |
Mês | Jan. |
Data de Acesso | 29 abr. 2024 |
Tipo Secundário | PRE PI |
Número de Arquivos | 1 |
Tamanho | 1140 KiB |
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2. Contextualização | |
Autor | 1 Wrasse, Cristiano Max 2 Suratno, E. 3 Admiranto, A. G. 4 Achmad, E. 5 Nakamura, T. 6 Tsuda, T. 7 Takahashi, Hisao 8 Medeiros, A. F. 9 Taylor, M. J. 10 Gobbi, Delano 11 Salatum, A. |
Identificador de Curriculo | 1 2 3 4 5 6 7 8JMKD3MGP5W/3C9JHCM 8 9 10 8JMKD3MGP5W/3C9JGTE |
Grupo | 1 DAE-INPE-MCT-BR 2 DAE-INPE-MCT-BR 3 DAE-INPE-MCT-BR |
Afiliação | 1 Instituto Nacional de Pesquisas Espaciais, Divisão de Aeronomia (INPE/DAE) 2 Space Science Center, National Institute of Aeronautics and Space 3 Space Science Center, National Institute of Aeronautics and Space 4 Space Science Center, National Institute of Aeronautics and Space 5 Research Institute for Sustainable Humanosphere (RISH) 6 Research Institute for Sustainable Humanosphere (RISH) 7 Instituto Nacional de Pesquisas Espaciais, Divisão de Aeronomia (INPE/DAE) 8 Universidade Federal de Campina Grande (UFCG) 9 Space Dynamics Laboratory and Physics Department, Utah State University 10 Instituto Nacional de Pesquisas Espaciais, Divisão de Aeronomia (INPE/DAE) 11 Space Science Center, National Institute of Aeronautics and Space |
Revista | Journal of Atmospheric and Solar-Terrestrial Physics |
Volume | 68 |
Número | 2 |
Páginas | 163-181 |
Histórico (UTC) | 2006-06-14 18:16:20 :: simone -> administrator :: 2021-07-18 04:01:22 :: administrator -> marciana :: 2006 |
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3. Conteúdo e estrutura | |
É a matriz ou uma cópia? | é a matriz |
Estágio do Conteúdo | concluido |
Transferível | 1 |
Tipo do Conteúdo | External Contribution |
Palavras-Chave | Gravity waves Ray tracing Mesosphere Sources Troposphere Airglow MIDDLE ATMOSPHERE RADAR OBSERVATIONS MESOSCALE VARIABILITY NIGHTGLOW EMISSIONS CACHOEIRA-PAULISTA JET-STREAM OH AIRGLOW WIND PROPAGATION TIDES |
Resumo | Gravity wave observations using all-sky CCD imager to measure the airglow OH, 02, and 01 emissions were made at Cachoeira Paulista (22.7 degrees S, 45 degrees W) (CP), at the low-middle latitude in Brazil, from October 1998 to September 1999. Near the equator, at Tanjungsari observatory (6.9 degrees S, 107.9 degrees E) (TJS), Indonesia, another wide angle CCD imager measuring the OH airglow emission layer has been operated from September 2000 to September 2001. With these data sets, a reverse ray tracing method was used to study propagation of gravity waves through the middle atmosphere and to estimate the source region. The CIRA-86 reference zonal wind and temperature models and the GSWM-02 tidal wind model were used in the present analysis. Both observation sites showed apparently similar wave characteristics, except for the horizontal phase speed.. which was much faster in the equatorial region. From the inverse ray tracing calculations, it was found that at CP, only about 15% of the wave events originated in the troposphere. Most of the events were located over the continent within an area of less than 400 km from the observation site. The identified source region in the troposphere showed a seasonal anisotropy, being mainly to the northwest of CP during summer and to the southeast and northwest in winter. This corresponds to the region of high tropospheric convection activity in the South American continent during summer and high meteorological front activity on the southwestern side during winter. At CP more than 70% of the waves showed that the ray tracing paths stopped in the mesosphere. At TJS the ray tracing indicates that 60% of the gravity wave sources might be located in the troposphere with an area of less than 200 km from the observation site, much closer than the case of CP. This corresponds to convective cloud activities on the north and northwest side of TJS. However, during southern hemisphere summer at both observation sites, most of the ray tracing paths stopped at the mesosphere owing to a condition of m(2) < 0 or critical level interactions. (c) 2005 Elsevier Ltd. All rights reserved. |
Área | CEA |
Arranjo | urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Reverse ray tracing... |
Conteúdo da Pasta doc | acessar |
Conteúdo da Pasta source | não têm arquivos |
Conteúdo da Pasta agreement | não têm arquivos |
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4. Condições de acesso e uso | |
Idioma | en |
Arquivo Alvo | Reverse ray tracing of the mesospheric gravity waves.pdf |
Grupo de Usuários | administrator simone |
Visibilidade | shown |
Detentor da Cópia | SID/SCD |
Política de Arquivamento | denypublisher denyfinaldraft24 |
Permissão de Leitura | deny from all and allow from 150.163 |
Permissão de Atualização | transferida para simone |
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5. Fontes relacionadas | |
Unidades Imediatamente Superiores | 8JMKD3MGPCW/3ETL868 |
Divulgação | WEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX. |
Acervo Hospedeiro | sid.inpe.br/banon/2003/08.15.17.40 |
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6. Notas | |
Campos Vazios | alternatejournal archivist callnumber copyright creatorhistory descriptionlevel doi 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 |
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7. Controle da descrição | |
e-Mail (login) | marciana |
atualizar | |
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