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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3LFC7F8
Repositorysid.inpe.br/mtc-m21b/2016/04.07.16.13   (restricted access)
Last Update2016:04.07.16.14.39 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2016/04.07.16.13.54
Metadata Last Update2021:01.02.03.53.50 (UTC) administrator
DOI10.1002/joc.4373
ISSN0899-8418
Citation KeyRibeiroSeluChou:2016:SyClWa
TitleSynoptic climatology of warm fronts in southeastern South America
Year2016
MonthFeb.
Access Date2024, May 18
Secondary TypePRE PI
Number of Files1
Size9801 KiB
2. Context
Author1 Ribeiro, Bruno Zanetti
2 Seluchi, Marcelo Enrique
3 Chou, Sin Chan
Resume Identifier1
2 8JMKD3MGP5W/3C9JHP2
Group1 MET-MET-SPG-INPE-MCTI-GOV-BR
2
3 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 National Center for Monitoring and Early Warning of Natural Disasters (Cemaden)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1 bruno.ribeiro@cptec.inpe.br
2
3 chou.sinchan@cptec.inpe.br
JournalInternational Journal of Climatology
Volume36
Number2
Pages644-655
Secondary MarkA1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
History (UTC)2016-04-07 16:13:54 :: simone -> administrator ::
2021-01-02 03:53:50 :: administrator -> simone :: 2016
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordswarm front
synoptic climatology
Southeastern South America
composites
AbstractThis study shows a synoptic climatology of warm fronts in Southeastern South America (SESA). Data from Climate Forecast System Reanalysis (CFSR) was used to identify warm fronts from 1979 to 2010. The identification method was based on the magnitude of meridional gradient of 850-hPa equivalent potential temperature (e) and 850-hPa wind fields. Composites of the most important atmospheric variables were constructed from 1 day before until 1 day after the formation of the warm front. An average frequency of two warm fronts per month is observed, with higher frequencies in austral winter. Most warm fronts precede the formation of extratropical cyclones over Uruguay and form because of the southward movement of previous cold/stationary fronts. Warm fronts form on average around southern Paraguay, northeastern Argentina and western part of southern Brazil and Uruguay, coupled to the eastern edge of the Chaco Low (CL) and the Northwestern Argentinean Low (NAL) where north/northwesterly flow predominates. An upper-level wave of wavenumber eight supports warm frontogenesis. Location and intensity of synoptic systems associated with a warm front event differ from winter to summer. Elevated instability is commonly present near warm fronts, and the average warm-front slope is 1:110, agreeing with other studies. Instability indices increase after the warm-front passage, leading to greater rainfall 1 day after the warm front forms.
AreaMET
Arrangement 1urlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Synoptic climatology of...
Arrangement 2urlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Synoptic climatology of...
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4. Conditions of access and use
Languageen
Target FileRibeiro_synoptic.pdf
User Groupsimone
Reader Groupadministrator
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Visibilityshown
Archiving Policydenypublisher denyfinaldraft
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Mirror Repositoryurlib.net/www/2011/03.29.20.55
Next Higher Units8JMKD3MGPCW/3F35TRS
8JMKD3MGPCW/43SKC35
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.14.54.36 1
sid.inpe.br/bibdigital/2021/01.01.17.20 1
DisseminationWEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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