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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Repositorysid.inpe.br/iris@1916/2005/11.24.15.26   (restricted access)
Last Update2005:11.24.15.26.00 (UTC) administrator
Metadata Repositorysid.inpe.br/iris@1916/2005/11.24.15.26.42
Metadata Last Update2018:06.05.01.16.14 (UTC) administrator
Secondary KeyINPE-13199PRE/8455
ISSN0273-1177
Citation KeyClemeshaSimoBatiTaka:2005:SeVaSo
TitleSeasonal variation in the solar diurnal tide and its possible influence on the atmospheric sodium layer
Year2005
Access Date2024, May 08
Secondary TypePRE PI
Number of Files1
Size260 KiB
2. Context
Author1 Clemesha, Barclay Robert
2 Simonich, Dale Martin
3 Batista, Paulo Prado
4 Takahashi, Hisao
Resume Identifier1 8JMKD3MGP5W/3C9JGKH
2 8JMKD3MGP5W/3C9JGT2
3 8JMKD3MGP5W/3C9JJ3H
4 8JMKD3MGP5W/3C9JHCM
Group1 DAE-INPE-MCT-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais, Divisão de Aeronomia (INPE, DAE)
JournalAdvances in Space Research
Volume35
Number11
Pages1951-1956
History (UTC)2005-11-24 15:26:43 :: sergio -> administrator ::
2006-09-28 22:30:35 :: administrator -> sergio ::
2008-01-07 12:53:12 :: sergio -> administrator ::
2012-07-17 12:40:45 :: administrator -> marciana ::
2012-10-03 14:40:51 :: marciana -> administrator :: 2005
2018-06-05 01:16:14 :: administrator -> marciana :: 2005
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsUpper atmosphere
Atmospheric tides
Sodium layer
AbstractIn a paper published 12 years ago, we showed that the height of the atmospheric sodium layer at our location is about 1 km lower in November than at any other time of the year. We also showed that the decrease in height of the sodium layer was accompanied by an increase in the intensity of the OI 557.7 nm and OH(9,4) band airglow emissions. At that time we suggested that this behavior could be the result of large scale convective transport in the MLT region. We have now had the opportunity to compare the diurnal variations of the sodium layer and airglow emissions with the tidal winds measured by meteor radar over the past 5 years. We find that the amplitude of the diurnal tide is much smaller in November than at other times of the year. Since most of the sodium measurements and all of the airglow observations are for night-time conditions only, a change in the amplitude of the 24-h tide could strongly influence the average measured sodium and airglow parameters. It is shown that the observed changes in the tidal winds are qualitatively consistent with the sodium measurements, but the amplitude of the observed height change is much greater than would be expected from the tidal winds.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Seasonal variation in...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Fileseasonal variation.pdf
User Groupadministrator
marciana
sergio
Reader Groupadministrator
marciana
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.40.54 2
sid.inpe.br/mtc-m21/2012/07.13.14.44.15 2
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Host Collectionsid.inpe.br/banon/2003/08.15.17.40
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyright creatorhistory descriptionlevel doi e-mailaddress electronicmailaddress format identifier isbn label lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Description control
e-Mail (login)marciana
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