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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34P/3JCESAP
Repositorysid.inpe.br/mtc-m21b/2015/04.23.16.29   (restricted access)
Last Update2015:04.23.16.29.55 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m21b/2015/04.23.16.29.55
Metadata Last Update2021:01.02.22.17.09 (UTC) administrator
DOI10.1007/s00382-015-2532-2
ISSN0930-7575
Citation KeyMüllerGanPivaSilv:2015:EnWaPr
TitleEnergetics of wave propagation leading to cold event in tropical latitudes of South America
Year2015
Access Date2024, May 20
Secondary TypePRE PI
Number of Files1
Size8103 KiB
2. Context
Author1 Müller, Gabriela Viviana
2 Gan, Manoel Alonso
3 Piva, Everson Dal
4 Silveira, Virginia Piccinini
Resume Identifier1
2 8JMKD3MGP5W/3C9JHNM
Group1
2 DOP-CPT-INPE-MCTI-GOV-BR
Affiliation1
2 Instituto Nacional de Pesquisas Espaciais (INPE)
JournalClimate Dynamics
Volumex
Secondary MarkA1_CIÊNCIAS_BIOLÓGICAS_I A1_INTERDISCIPLINAR A1_CIÊNCIAS_AMBIENTAIS A1_BIODIVERSIDADE A1_GEOCIÊNCIAS A2_ASTRONOMIA_/_FÍSICA A2_ENGENHARIAS_I B1_CIÊNCIA_DA_COMPUTAÇÃO
History (UTC)2015-04-23 16:29:55 :: valdirene -> administrator ::
2021-01-02 22:17:09 :: administrator -> simone :: 2015
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordsenergetics
wave propagation
frost events
South America
AbstractThis paper presents a new vision on the cold and cool events that affect the tropical region of South America, considering the dynamics and the energetics of wave train propagation associated with these systems. Through a composite analysis of meridional winds at 300 hPa for cold (T < 0 °C) and cool (0 °C ≤ T ≤ 2.5 °C) air incursions affecting tropical latitudes and causing frost are studied. The cold events observed in tropical latitudes are associated with a single Rossby wave pattern propagating over the Pacific Ocean which drives the low level anticyclone from the southwest of the continent to low latitudes. This propagation involves a southern circulation due to the meridional wind penetration and consequently cold air advection causing temperatures to drop below 0 °C. During cool events a subtropical wave train propagating through the Pacific Ocean is observed, which merges before the event with a wave coming from the subpolar latitudes of the South Atlantic Ocean. The zonal propagation leads to the entrance of the anticyclone from the west of the continent, and it is strengthened together with the meridionaly extended cyclone located upstream. This configuration causes southerly wind advection over central-southeastern Brazil and consequently causes the temperature decrease. The energetics shows that the cold events kinetic energy maxima are more intense than those of cool events. For the cold events three maxima are observed, the first (K1) and the third (K3) maxima are developed by baroclinic conversion and ageostrophic flux convergence and the second one (K2) by ageostrophic flux convergence. For the cool events two maxima are found, the first maximum (K4) developed by baroclinic conversion and the second one by ageostrophic flux convergence.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDOP > Energetics of wave...
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4. Conditions of access and use
Target FileMuller_Energetics.pdf
User Groupvaldirene
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Visibilityshown
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5. Allied materials
Mirror Repositoryurlib.net/www/2011/03.29.20.55
Next Higher Units8JMKD3MGPCW/43SQKNE
Citing Item Listsid.inpe.br/bibdigital/2021/01.02.22.14 2
DisseminationWEBSCI; PORTALCAPES; AGU; COMPENDEX; SCOPUS.
Host Collectionsid.inpe.br/mtc-m21b/2013/09.26.14.25.20
6. Notes
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