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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/432C6HS
Repositorysid.inpe.br/mtc-m21c/2020/08.05.11.01   (restricted access)
Last Update2020:08.05.11.01.53 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2020/08.05.11.01.54
Metadata Last Update2022:01.04.01.35.18 (UTC) administrator
DOI10.1016/j.jastp.2020.105397
ISSN1364-6826
Citation KeyEgitoBatTakBatBur:2020:VaEqIo
TitleVariability of the equatorial ionosphere induced by nonlinear interaction between an ultrafast Kelvin wave and the diurnal tide
Year2020
MonthOct.
Access Date2024, May 08
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size2378 KiB
2. Context
Author1 Egito, Fábio
2 Batista, Inez Staciarini
3 Takahashi, Hisao
4 Batista, Paulo Prado
5 Buriti, R. A.
Resume Identifier1
2 8JMKD3MGP5W/3C9JHDA
3 8JMKD3MGP5W/3C9JHCM
4 8JMKD3MGP5W/3C9JJ3H
Group1
2 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
3 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
4 DIDAE-CGCEA-INPE-MCTIC-GOV-BR
Affiliation1 Universidade Federal do Recôncavo da Bahia (UFRB)
2 Instituto Nacional de Pesquisas Espaciais (INPE)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Instituto Nacional de Pesquisas Espaciais (INPE)
5 Universidade Federal de Campina Grande (UFCG)
Author e-Mail Address1 fabioegito@yahoo.com.br
2 inez.batista@inpe.br
3
4 paulo.batista@inpe.br
JournalJournal of Atmospheric and Solar-Terrestrial Physics
Volume208
Pagese105397
Secondary MarkA1_ENGENHARIAS_I A2_GEOCIÊNCIAS A2_ENGENHARIAS_III B1_INTERDISCIPLINAR B1_ENGENHARIAS_IV B1_BIODIVERSIDADE B2_ASTRONOMIA_/_FÍSICA C_CIÊNCIAS_BIOLÓGICAS_I
History (UTC)2020-08-05 11:01:54 :: simone -> administrator ::
2020-08-05 11:01:55 :: administrator -> simone :: 2020
2020-08-05 11:04:43 :: simone -> administrator :: 2020
2022-01-04 01:35:18 :: administrator -> simone :: 2020
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
KeywordsUltrafast Kelvin wave and tides
Nonlinear interaction
Secondary waves
Ionosphere
AbstractThe wave forcing from below allows the neutral atmosphere to drive short-term variability in the ionosphere. Recent modeling studies have shown that secondary waves originated from the nonlinear interaction of the atmospheric tides with planetary scale waves can contribute significantly to day-to-day variability of the ionosphere. In this study we used MLT neutral wind measured at S~ ao Jo~ ao do Cariri (7.4�S, 36.5�W) and ionospheric soundings performed by a digisonde installed at Fortaleza (3.9�S, 38.4�W) to investigate the presence and the induced variability by a secondary wave in the mesosphere-ionosphere system over the Brazilian equatorial region. We found evidences of the nonlinear interaction between a 3.5-day ultrafast Kelvin wave and the diurnal tide. The interaction produced a 1.3-day secondary wave that was found to propagate upward with maximum amplitude of 15 m/s and relatively long vertical wavelength (~44 km) in the MLT, which may allow it to penetrate into the ionosphere. In the ionosphere, we observed a common 1.3-day periodic variation in the virtual height (hF) and critical frequency (foF2), which may be connected to the secondary wave observed in the MLT via modulation of the wind system in the E region dynamo. These findings suggest that secondary waves may impose additional variability to ionosphere.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDAE > Variability of the...
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4. Conditions of access and use
Languageen
Target Fileegito_variability.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
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/bibdigital/2013/09.29.20.43 2
sid.inpe.br/mtc-m21/2012/07.13.14.50.14 1
DisseminationWEBSCI; PORTALCAPES; AGU; COMPENDEX; SCOPUS.
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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