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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/44D54JL
Repositorysid.inpe.br/mtc-m21c/2021/03.25.14.00
Metadata Repositorysid.inpe.br/mtc-m21c/2021/03.25.14.00.38
Metadata Last Update2022:04.03.19.25.14 (UTC) administrator
Secondary KeyINPE--PRE/
Citation KeyEgitoBuriBatiPanc:2021:LoVaNo
TitleLongitudinal variability of the nonlinear interaction between ultrafast Kelvin waves and diurnal tides
Year2021
Access Date2024, May 23
Secondary TypePRE CN
2. Context
Author1 Egito, F.
2 Buriti, R. A.
3 Batista, Paulo Prado
4 Pancheva, D.
Resume Identifier1
2
3 8JMKD3MGP5W/3C9JJ3H
Group1
2
3 DIHPA-CGCE-INPE-MCTI-GOV-BR
Affiliation1 Universidade Federal do Recôncavo da Bahia
2 Universidade Federal de Campina Grande (UFCG)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Bulgarian Academy of Sciences
Author e-Mail Address1
2
3 paulopradobatista@yahoo.com
Conference NameSimpósio Brasileiro de Geofísica Espacial e Aeronomia, 8 (SBGEA)
Conference LocationOnline
Date22-26 mar.
History (UTC)2021-03-25 14:00:38 :: simone -> administrator ::
2022-04-03 19:25:14 :: administrator -> simone :: 2021
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
AbstractThe nonlinear interaction between tides and planetary scale waves contributes to the short-term variability of the MLT dynamics and is a pathway for the coupling between the neutral atmosphere and the ionosphere-thermosphere (I-T) system. By using MLT wind measurements carried out at Cariri (7.4oS, 36.5oW) and at Ascension Island (7.9oS, 14.4oW) we have investigated the nonlinear interaction between an ultrafast Kelvin wave (UFKW) and the diurnal tide. Along with the signature of an UFKW (∼0.25 cycle/day), we observed periodic oscillations in the zonal wind, at both Cariri and Ascension Island, consistent with the secondary waves generated via the nonlinear interaction between the UFKW and the diurnal tide (1 cycle/day). In addition, we observed the modulation of the diurnal tide amplitude in the zonal wind at the period of the UFKW. At Cariri only the 0.75 cycle/day secondary wave related to the difference between the frequencies of the diurnal tide (1 cycle/day) and the UFKW was observed. On the other hand, at Ascension, both secondary waves related to the sum (1.25 cycle/day) and difference (0.75 cycle/day) between the diurnal tide and UFKW frequencies were observed. The vertical structure of these periodic oscillations also exhibited distinct behavior. At Cariri, the 0.75 cycle/day secondary wave exhibited a well-defined vertical structure with downward phase progression, indicating upward propagation with vertical wavelength of 44 km. On the other hand, at Ascension, while the 0.75 cycle/day secondary wave did not exhibit clear phase progression, either downward or upward, the 1.25 cycle/day secondary wave exhibited downward phase progression, and then upward propagation, with vertical wavelength of approximately 20 km. In this paper we will present and discuss in more details the characteristics and possible impacts of the nonlinear interaction in the mesosphere-thermosphere-ionosphere system.
AreaCEA
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Visibilityshown
Update Permissionnot transferred
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Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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