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Reference TypeJournal Article
Sitemtc-m16d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP7W/37SMQF8
Repositorysid.inpe.br/mtc-m19@80/2010/07.19.13.13   (restricted access)
Last Update2010:08.09.16.56.39 (UTC) administrator
Metadatasid.inpe.br/mtc-m19@80/2010/07.19.13.13.04
Metadata Last Update2021:07.18.04.02.30 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.1016/j.jastp.2010.03.017
ISSN1364-6826
Citation KeyClemeshaSimoBati:2010:MeReTe
TitleMesopause region temperature structure observed by sodium resonance lidar
ProjectFundacao de Apoio a Pesquisa do Estado de Sao Paulo - FAPESP ; Conselho Nacional de Desenvolvimento Cientifico e Tecnico - CNPq
Year2010
MonthJunho
Access Date2021, July 25
Number of Files1
Size563 KiB
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Author1 Clemesha, Barclay Robert
2 Simonich, Dale
3 Batista, Paulo Prado
Resume Identifier1
2
3 8JMKD3MGP5W/3C9JJ3H
Group1 DAS-CEA-INPE-MCT-BR
2 DAS-CEA-INPE-MCT-BR
3 DAE-CEA-INPE-MCT-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
JournalJournal of Atmospheric and Solar-Terrestrial Physics
Volume72
Number9-10
Pages740 - 744
Secondary TypePRE PI
Secondary MarkB2_ASTRONOMIA_/_FÍSICA B1_CIÊNCIAS_BIOLÓGICAS_I B1_ECOLOGIA_E_MEIO_AMBIENTE B1_ENGENHARIAS_IV B1_GEOCIÊNCIAS A2_INTERDISCIPLINAR
History (UTC)2011-05-24 23:41:22 :: marciana -> administrator :: 2010
2012-07-15 03:42:05 :: administrator -> marciana :: 2010
2013-02-26 19:24:50 :: marciana -> administrator :: 2010
2021-07-18 04:02:30 :: administrator -> marciana :: 2010
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Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordsgravity-wave perturbations, density response, wind shears, na layer.
AbstractMesopause region temperature measurements made with a sodium resonance lidar show two unexpected features: (1) Strong positive temperature gradients are often associated with strong gradients in the sodium concentration and (2) positive temperature gradients are generally much stronger than negative ones. Although the structures we see frequently appear to be associated with gravity waves or tides, the asymmetrical temperature oscillations cannot be explained as the result of simple wave propagation. We suggest that strong positive temperature gradients correspond to regions of high atmospheric stability, where eddy diffusion is inhibited, permitting the build-up of strong gradients in temperature and minor constituent mixing ratio.
AreaCEA
Arrangement 1urlib.net > BDMCI > Fonds > Produção > DIDAE > Mesopause region temperature...
Arrangement 2urlib.net > BDMCI > Fonds > Produção > DIDAS > Mesopause region temperature...
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Languageen
Target Fileclemesha.pdf
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Visibilityshown
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Update Permissionnot transferred
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Mirror Repositorysid.inpe.br/mtc-m19@80/2009/08.21.17.02.53
Next Higher Units8JMKD3MGPCW/3ETL868
8JMKD3MGPCW/3ETR8EH
DisseminationWEBSCI; PORTALCAPES; AGU.
Host Collectionsid.inpe.br/mtc-m19@80/2009/08.21.17.02
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