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1. Identity statement
Reference TypeJournal Article
Sitemarte3.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3r59YCT/GUgsq
Repositorysid.inpe.br/iris@1905/2005/07.29.00.36   (restricted access)
Last Update2013:04.02.11.55.57 (UTC) jefferson
Metadata Repositorysid.inpe.br/iris@1905/2005/07.29.00.36.30
Metadata Last Update2018:06.06.04.14.09 (UTC) administrator
Secondary KeyINPE-5691-PRE/1851
DOI10.1016/0273-1177(90)90012-O
ISSN0273-1177
Label7086
Citation KeyTakahashiSahaTeix:1990:AiInTe
TitleAirglow intensity and temperature response to atmospheric wave propagation in the mesopause region
Year1990
Secondary Date19960311
Access Date2024, May 02
Secondary TypePRE PI
Number of Files1
Size313 KiB
2. Context
Author1 Takahashi, Hisao
2 Sahai, Yogeshwar
3 Teixeira, Nelson Rodrigues
Group1 DAE-INPE-BR
2 DGE-INPE-BR
3 DAE-INPE-BR
JournalAdvances in Space Research
Volume10
Number10
Pages77-81
History (UTC)2012-10-14 00:12:20 :: administrator -> jefferson ::
2013-02-19 14:56:04 :: jefferson -> administrator :: 1990
2013-04-02 11:55:29 :: administrator -> jefferson :: 1990
2013-04-02 11:55:57 :: jefferson -> administrator :: 1990
2018-06-06 04:14:09 :: administrator -> marciana :: 1990
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsAtmospheric Composition
Atmospherics
Airglow Intensity
Atmospheric Wave Propagation
Mesopause Region
AbstractSimultaneous measurements of the 02(0,1) atmospheric band (864.5 nm) and OH(9,4) band (774,6 nm) emissions in the night airglow, using a tilting filter photometer, have been carried out at Cachoeira Paulista (22.7 deg. S, 45.0 deg W), Brazil, since 1983. The band intensities of the 02(0,1) band, I(02) and OH(9,4) band, I(OH), and their rotational temperatures, T(02) and T(OH) have been obtained. In the nocturnal variations time-lagged wave-like co-variations between the intensities and rotational temperatures were frequently observed. Correlation studies reveal that, in general, the rotational temperature variations, T(02) and T(OH), lead the intensity variations, I(02) and I(OH), respectively. It is found that the time lag between T(02) and T(OH) is less, by about 0.5 hour, than that between I(02) and I(OH), which is about 1.5 hours, indicating that the airglow intensity response to atmospheric wave propagation is different from the temperature response.
AreaCEA
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4. Conditions of access and use
Languageen
Target File1-s2.0-027311779090012O-main.pdf
User Groupadministrator
jefferson
Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
8JMKD3MGPCW/3EU29DP
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Host Collectionsid.inpe.br/banon/2001/04.03.15.36
6. Notes
Empty Fieldsaffiliation alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress electronicmailaddress format isbn lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup resumeid rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Description control
e-Mail (login)marciana
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