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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/yyuUD
Repositorycptec.inpe.br/walmeida/2003/06.25.09.38   (restricted access)
Last Update2005:05.20.03.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2003/06.25.09.38.56
Metadata Last Update2021:02.10.18.59.14 (UTC) administrator
Secondary KeyINPE--PRE/
ISSN0177-798X
Citation KeyMarengoAmbrKilaLieb:2002:UpWaTr
TitleUpper-air wave trains over the Pacific Ocean and wintertime cold surges in tropical-subtropical South America leading to Freezes in Southern and Southeastern Brazil.
Year2002
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size763 KiB
2. Context
Author1 Marengo, José Antônio
2 Ambrizzi, Tercio
3 Kiladis, G.
4 Liebmann, B.
Group1 DMD-INPE-MCT-BR
Affiliation1 CPTEC-INPE- Cachoeira Paulista -12630-000- SP-Brazil
e-Mail Addressdeicy@cptec.inpe.br
JournalTheoretical and Applied Climatology
Volume73
Number3-4
Pages223-242
History (UTC)2005-05-20 12:15:45 :: marciana -> administrator ::
2021-02-10 18:59:14 :: administrator -> marciana :: 2002
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsBaroclinic atmosphere
northern winter
rossby waves
Amazon basin
convection
anomalies
propagation
seasonality
incursions
dynamic
AbstractAn examination is made of the relationships between circulation and convection over South America as related to strong cooling in southern and southeastern Brazil during austral wintertime. Correlations between sub monthly (230 days) near-surface air temperature in southeastern Brazil reveal the preferred path of a quasi-stationary Rossby wave impinging on to the region from mid-latitudes and emanating from the tropical western Pacific. The large amplitude upper-level trough in middle latitudes, which extends into the tropics, has been pointed out as one of the major features of the cold situation. These waves embedded in westerly flow are an example of wintertime tropical-extratropical interactions leading to cooling in southeastern South America. This is suggested by the results from the observational and baroclinic-modeling studies presented here. However, in addition to the right synoptic situation associated with this intermediate modulation, local controls are important on determining the degree of cooling and the occurrence of freezes.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Upper-air wave trains...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target FileMarengo_Upper-air wave.pdf.pdf
User Groupadministrator
Visibilityshown
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/43SKC35
DisseminationWEBSCI; PORTALCAPES; MGA.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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7. Description control
e-Mail (login)marciana
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