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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3K3BKUB
Repositorysid.inpe.br/mtc-m21b/2015/08.11.16.00
Last Update2015:08.11.16.01.18 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2015/08.11.16.00.20
Metadata Last Update2018:06.04.02.55.37 (UTC) administrator
Secondary KeyINPE--PRE/
Citation KeyEgitoBatiClemBuri:2015:VeWi34
TitleVertical winds and 3-4 day momentum flux in the MLT inferred from meteor radar measurements
Year2015
Access Date2024, May 17
Secondary TypePRE CI
Number of Files1
Size596 KiB
2. Context
Author1 Egito, Fábio
2 Batista, Paulo Prado
3 Clemesha, Barclay Robert
4 Buriti, Ricardo A.
Resume Identifier1
2 8JMKD3MGP5W/3C9JJ3H
3 8JMKD3MGP5W/3C9JGKH
Group1
2 DAE-CEA-INPE-MCTI-GOV-BR
3 DAE-CEA-INPE-MCTI-GOV-BR
Affiliation1 Universidade Federal do Oeste da Bahia (UFOB)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal de Campina Grande (UFCG)
Author e-Mail Address1
2 paulo.batista@inpe.br
3 brc@laser.inpe.br
Conference NameInternational Congress of the Brazilian Geophysical Society, 14
Conference LocationRio de Janeiro, RJ
Date3-6 Aug.
History (UTC)2015-08-11 16:00:20 :: simone -> administrator ::
2018-06-04 02:55:37 :: administrator -> simone :: 2015
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
AbstractPlanetary scale waves in equatorial region transport a significant amount of energy and momentum through atmosphere. Quantifying the momentum transported by these waves and its effects toward the mean flow is rather important. Direct estimative of the momentum flux transported by these waves requires horizontal and vertical wind measurements. Ground-based meteor radars have provided continuous and reliable measurements of the horizontal wind components in the MLT region. On the other hand, vertical wind component does not present the same reliability. However, an approach presented by Babu et al. (2012), made possible to calculate tridimensional daily winds by using only near zenith echoes detected around their maximum counting rate, i.e., during early morning hours. From daily tridimensional winds, momentum fluxes due to planetary scale waves can be estimated. Following this approach, we have used measurements performed by a meteor radar installed at São João do Cariri (7.4ºS; 36.5ºW) in order to measure vertical winds and after determine the momentum flux transported by these waves. Vertical wind presents magnitudes of a few meters per second and occasionally reaches magnitudes higher than 10 m/s. Below 92 km vertical wind is upward during the whole year and above exhibits a semi-annual oscillation with downward phase during the equinoxes. Variations associated to planetary scale waves in the vertical wind are also observed and some of them appear simultaneously in the zonal and meridional wind. Vertical transport of zonal momentum fluxes of 3-4 day component is found to be maximum near autumn equinox, when its value reaches almost 20 m2s -2, while minimum momentum fluxes were observed before winter solstice.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Vertical winds and...
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4. Conditions of access and use
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zipped data URLhttp://mtc-m21b.sid.inpe.br/zip/8JMKD3MGP3W34P/3K3BKUB
User Groupself-uploading-INPE-MCTI-GOV-BR
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Reader Groupadministrator
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Visibilityshown
Read Permissionallow from all
Update Permissionnot transferred
5. Allied materials
LinkingTrabalho não Vinculado à Tese/Dissertação
Mirror Repositoryurlib.net/www/2011/03.29.20.55
Next Higher Units8JMKD3MGPCW/3ETL868
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.40.54 1
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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