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Tipo da ReferênciaConference Proceedings
Identificador6qtX3pFwXQZGivnJVY/Ng2z3
Repositóriosid.inpe.br/mtc-m16@80/2006/11.24.18.27
Metadadossid.inpe.br/mtc-m16@80/2006/11.24.18.27.35
Sitemtc-m16.sid.inpe.br
Rótuloself-archiving-INPE-MCTIC-GOV-BR
Chave SecundáriaINPE--PRE/
Código do Detentorisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Chave de CitaçãoTakahashiWFMWGNS:2006:AtGrWa
Autor1 Takahashi, Hisao
2 Wrasse, Cristiano Max
3 Fechine, Joaquim
4 Medeiros, A. F.
5 Wickert, J.
6 Gobbi, Delano
7 Nakamura, T.
8 Shiokawa, K.
Grupo1 DAE-INPE-MCT-BR
2 DAE-INPE-MCT-BR
3 DAE-INPE-MCT-BR
4
5
6 DAE-INPE-MCT-BR
Afiliação1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal de Campina Grande
5 The German Research Center for Earth Sciences
6 Instituto Nacional de Pesquisas Espaciais (INPE)
7 Research Institute for sustainable humanosphere, Kyoto University
8 Solar-Terrestrial Environment Laboratory, Nagoya University
TítuloAtmospheric gravity wave activity in the equatorial region observed by optical and radio-wave techniques (solicited)
Nome do EventoCommitte on Space Research, 36 (COSPAR).
Ano2006
Título do LivroProceedings
Data2006-07-16
Localização do EventoBeijing, China
ResumoGravity wave signatures in the upper mesosphere to lower thermosphere (MLT) in the equatorial and low latitude regions have been investigated by airglow imaging technique from the south American sector at Cariri (7 S, 36 W). The wave characteristics, direction of propagation and frequency of occurrence, were analyzed in order to understand the wave generation and propagation schemes. Temperature variability in the stratosphere observed by CHAMP satellite GPS radio-occultation measurement was also used to find out a region of high gravity wave activity in the upper troposphere to stratosphere. It was found that at Cariri a major part of the observed waves (75 %) has characteristics of ducting and/or evanescent forms. Only 25 % of them showed the vertical propagation form from troposphere to mesosphere, and most of them came from an area of 250 km from the observation site. These results will be compared with the data from the western pacific region and presented.
Idiomaen
Tipo SecundárioPRE CI
Tipo TerciárioPoster Session
AreaCEA
Tamanho62 KiB
Número de Arquivos1
Arquivo Alvotakahashi_atmospheric.pdf
Última Atualização2020:10.08.14.05.13 sid.inpe.br/banon/2003/08.15.17.40 marciana
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Tipo do ConteudoExternal Contribution
Estágio do Documentonot transferred
Tipo de Versãopublisher
Permissão de Leituraallow from all
Unidades Imediatamente Superiores8JMKD3MGPCW/3ETL868
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Histórico2006-11-24 18:27:35 :: simone -> administrator ::
2018-06-05 01:17:08 :: administrator -> marciana :: 2006
2020-10-08 14:05:14 :: marciana -> simone :: 2006
Campos Vaziosaccessionnumber archivingpolicy archivist callnumber copyholder copyright creatorhistory descriptionlevel dissemination doi e-mailaddress edition editor electronicmailaddress format isbn issn keywords lineage mark mirrorrepository nextedition notes numberofvolumes orcid organization pages parameterlist parentrepositories previousedition previouslowerunit progress project publisher publisheraddress readergroup resumeid rightsholder secondarydate secondarymark serieseditor session shorttitle sponsor subject tertiarymark type url volume
Data de Acesso31 out. 2020
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