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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/EfEhg
Repositorycptec.inpe.br/walmeida/2004/11.23.15.19   (restricted access)
Last Update2007:03.26.12.10.26 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/11.23.15.19.27
Metadata Last Update2021:02.10.19.00.24 (UTC) administrator
Secondary KeyINPE-14502-PRE/9533
ISSN0899-8418
Citation KeyKayanoAndr:2007:ReSoAm
TitleRelations of South American summer rainfall interannual variations with the Pacific decadal oscillation
Projectclimatologia dinâmica, modelagem climática
Year2007
Secondary Date20070330
MonthMar.
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size785 KiB
2. Context
Author1 Kayano, Mary Toshie
2 Andreoli, Rita Valéria
Resume Identifier1 8JMKD3MGP5W/3C9JHST
Group1 DMD-INPE-MCT-BR
2 DMD-INPE-MCT-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)
2 Instituto Nacional de Pesquisas Espaciais (INPE/CPTEC)
Author e-Mail Address1 mkayano@cptec.inpe.br
2 rita@cptec.inpe.b
e-Mail Addressatus@cptec.inpe.br
JournalInternational Journal of Climatology
Volume27
Number4
Pages531-540
History (UTC)2006-07-26 14:28:22 :: fabia -> administrator ::
2006-11-17 23:18:36 :: administrator -> estagiario ::
2006-11-20 13:27:41 :: estagiario -> fabia ::
2007-09-03 13:03:32 :: fabia -> administrator ::
2012-11-20 03:12:50 :: administrator -> fabia :: 2007
2013-02-20 14:45:30 :: fabia -> administrator :: 2007
2021-02-10 19:00:24 :: administrator -> marciana :: 2007
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsEl Niñ
o
southern oscillation
pacific decadal oscillation
rainfall
climate variability
AbstractThe anomaly patterns of rainfall in South America for El Nino/Southern Oscillation (ENSO) extreme conditions stratified according to the high, low, and normal Pacific (inter-) Decadal Oscillation (PDO) phases (HPDO, LPDO and NPDO) are examined for the three bi-months of the season from November to April. El Nino (EN) and La Nina (LN) composites as well as the linear (EN − LN) and nonlinear (EN LN) components of the precipitation anomaly patterns relative to ENSO show substantial differences among the three PDO phases. The differences in the strength of ENSO teleconnections for the South American rainfall might be related to the PDO, which creates a background for these teleconnections acting constructively (destructively) when ENSO and PDO are in the same (opposite) phase. An interesting aspect is the occurrence of robust structures of the nonlinear component, which are due to the same sign rainfall anomalies for EN and LN composites. This is particularly conspicuous for the HPDO over eastern Brazil in the South Atlantic Convergence Zone (SACZ) region during Nov/Dec and Jan/Feb, for the HPDO over northern/northwestern South America during Mar/Apr, and for the NPDO over northeastern Brazil during Mar/Apr. The results presented here might have relevant implications for climate monitoring purposes. Copyright ÆÉ 2006 Royal Meteorological Society.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Relations of South...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target FileKayano_relations.pdf
User Groupadministrator
fabia
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft
Read Permissiondeny from all and allow from 150.163
Update Permissiontransferred to fabia
5. Allied materials
Next Higher Units8JMKD3MGPCW/43SKC35
URL (untrusted data)http://www.rmets.org/
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
NotesDOI: 10.1002/joc.1417 25/09/2006 in www.interscience.wiley.com
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7. Description control
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