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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemtc-m21d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34T/46L4378
Repositorysid.inpe.br/mtc-m21d/2022/04.04.13.13
Last Update2022:04.04.13.13.37 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21d/2022/04.04.13.13.37
Metadata Last Update2023:01.03.16.46.03 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.5194/egusphere-egu22-11510
Citation KeyMitraGuhaBatiBuri:2022:ReTrPl
TitleResponse of the traveling planetary waves at low latitude middle atmosphere during September 2019 minor sudden stratospheric warming
FormatOn-line
Year2022
Access Date2024, May 13
Secondary TypePRE CI
Number of Files1
Size290 KiB
2. Context
Author1 Mitra, Gourav
2 Guharay, Amitava
3 Batista, Paulo Prado
4 Buriti, Ricardo
Resume Identifier1
2
3 8JMKD3MGP5W/3C9JJ3H
Group1
2
3 DIHPA-CGCE-INPE-MCTI-GOV-BR
Affiliation1 Physical Research Laboratory, Ahmedabad, India
2 Physical Research Laboratory, Ahmedabad, India
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal de Campina Grande (UFCG)
Author e-Mail Address1 gourav@prl.res.in
2 guharay@prl.res.in
3 paulo.batista@inpe.br
4 rburiti.ufcg@gmail.com
Conference NameEGU General Assembly
Conference LocationOnline
Date23-27 May 2022
PublisherEGU
Book TitleProceedings
History (UTC)2022-04-04 13:13:37 :: simone -> administrator ::
2023-01-03 16:46:03 :: administrator -> simone :: 2022
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractPlanetary wave (PW) associated dynamical variability in the equatorial and extratropical middle atmosphere during the September 2019 Southern hemisphere minor sudden stratospheric warming (SSW) is investigated utilizing meteor radar wind observations from São João do Cariri (7.4°S, 36.5°W) and Cachoeira Paulista (22.7°S, 45°W) and reanalysis data. Signature of the mesospheric warming in conjunction with the stratospheric cooling is found at low latitudes. The strong westerly wind at low latitudes decelerates notably near 65 km at the onset of the warming episode, although no wind reversal is observed. The wind spectra reveal a prevalent quasi-16-day wave (Q16DW) prior to the SSW and existence of a quasi-6-day wave (Q6DW) after the warming event. Possible existence of barotropic/baroclinic instability in the low and mid latitude middle atmosphere may be responsible for exciting the Q6DW. The traveling PW is primarily found to travel westward corresponding to zonal wavenumber 1 and 2. Furthermore, significant latitudinal mixing of airmass between the tropics and high latitudes is evident in the potential vorticity map. The Eliassen-Palm flux diagnosis shows the propagation of the Q6DW and Q16DW from mid to low latitudes during the warming event.
AreaCEA
Arrangementurlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCE > Response of the...
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4. Conditions of access and use
data URLhttp://mtc-m21d.sid.inpe.br/ibi/8JMKD3MGP3W34T/46L4378
zipped data URLhttp://mtc-m21d.sid.inpe.br/zip/8JMKD3MGP3W34T/46L4378
Languageen
Target FileEGU22-11510-print.pdf
User Groupsimone
Visibilityshown
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/46KTFK8
Host Collectionurlib.net/www/2021/06.04.03.40
6. Notes
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