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1. Identity statement
Reference TypeJournal Article
Sitemarte3.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3r59YCT/GUgqa
Repositorysid.inpe.br/iris@1905/2005/07.29.00.33.59   (restricted access)
Last Update2013:05.15.14.20.42 (UTC) jefferson
Metadata Repositorysid.inpe.br/iris@1905/2005/07.29.00.34
Metadata Last Update2021:07.18.04.00.40 (UTC) administrator
Secondary KeyINPE-5687-PRE/1844
ISSN1364-6826
Label7082
Citation KeyClemeshaSimo:1990:CoPaEn
TitleComments on a paper entitled "Gravity wave generation of simultaneous auroral sporadic-E layers and sudden neutral sodium layers" by S. Kirkwood and P.N. Collis
ProjectFNDCT (FINEP 537/CT).
Year1990
Secondary Date19960311
Access Date2024, May 01
Secondary TypePRE PI
Number of Files1
Size182 KiB
2. Context
Author1 Clemesha, Barclay Robert
2 Simonich, Dale Martin
Group1 DAE-INPE-BR
2 DAE-INPE-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1 brc@laser.inpe.br
2 simonich@laser.inpe.br
JournalJournal of Atmospheric and Solar-Terrestrial Physics
Volume52
Number1
Pages85-86
History (UTC)2008-06-09 16:14:53 :: administrator -> banon ::
2010-05-11 15:18:24 :: banon -> administrator ::
2013-03-08 14:47:27 :: administrator -> jefferson :: 1990
2013-03-08 14:58:18 :: jefferson -> administrator :: 1990
2013-03-14 05:00:49 :: administrator -> jefferson :: 1990
2013-05-15 14:20:43 :: jefferson -> administrator :: 1990
2021-07-18 04:00:40 :: administrator -> marciana :: 1990
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordsgravity waves
auroral sporadic-E layers
neutral sodium layers
AbstractKIRKWOOD and COLLIS (1989) have suggested that the sudden sodium layers (SSLs) which have been observed at high latitudes (von ZAHN et al., 1987; von ZAHN and HANSEN, 1988; GARDNER et al., 1986) might be produced by strong downward neutral winds, probably produced by gravity waves resulting from Joule heating caused by auroral precipitation. They show that the presence of such a wind could produce enhanced concentrations of minor atmospheric constituents provided two conditions were met: (1) the vertical wind would have to decrease rapidly with decreasing height (in Kirkwood and Collis's model it was reduced to zero just below the height at which the layer was to be formed), and (2) the mixing ratio of the minor constituent would have to increase with height above this point. The suggestion of Kirkwood and Collis is an interesting one, especially in view of the fact that the alternative mechanisms which have been suggested in the literature (CLEMESHA et al., 1978, 1980; von ZAHN et al., 1987; CLEMESHA et al., 1988) have not been shown to explain all the observed characteristics of enhanced sodium layers. Unfortunately, however, there appear to be two fatal flaws in the proposed mechanism.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Comments on a...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target File1-s2.0-0021916990901187-main.pdf
User Groupadministrator
banon
jefferson
Visibilityshown
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3ETL868
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
Host Collectionsid.inpe.br/banon/2001/04.03.15.36
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel doi e-mailaddress format isbn lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress readergroup resumeid rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Description control
e-Mail (login)marciana
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