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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKAN8RW/3E7UC6T
Repositorydpi.inpe.br/plutao/2013/05.31.16.49.19   (restricted access)
Last Update2013:07.12.18.00.07 (UTC) administrator
Metadata Repositorydpi.inpe.br/plutao/2013/05.31.16.49.20
Metadata Last Update2021:01.02.03.52.43 (UTC) administrator
DOI10.1002/joc.3569
ISSN0899-8418
Labellattes: 9331105406437396 1 KayanoAndrSouz:2013:ReENSo
Citation KeyKayanoAndrSouz:2013:ReENSo
TitleRelations between ENSO and the South Atlantic SST modes and their effects on the South American rainfall
ProjectCNPq (569749/2008-5)
Year2013
Access Date2024, June 17
Secondary TypePRE PI
Number of Files1
Size1342 KiB
2. Context
Author1 Kayano, Mary Toshie
2 Andreoli, Rita Valeria
3 Souza, Rodrigo Augusto Ferreira de
Resume Identifier1 8JMKD3MGP5W/3C9JHST
Group1 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Universidade do Estado do Amazonas, Escola Superior de Tecnologia, Manaus, AM, Brazil
3 Universidade do Estado do Amazonas, Escola Superior de Tecnologia, Manaus, AM, Brazil
Author e-Mail Address1 mary.kayano@cptec.inpe.br
e-Mail Addressmary.kayano@cptec.inpe.br
JournalInternational Journal of Climatology
Volume33
Pages2008 – 2023
Secondary MarkA1 A1 A1 A1 A2 A2 B1
History (UTC)2013-05-31 16:49:20 :: lattes -> administrator ::
2021-01-02 03:52:43 :: administrator -> marcelo.pazos@inpe.br :: 2013
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
Keywordsclimatology
climate variability
El Niņo-Southern Oscillation
AbstractThis paper analyses the relations between the El Niņo/Southern Oscillation (ENSO) mode in the tropical Pacific and the sea surface temperature (SST) modes in the South Atlantic for the 1900 2006 period. In the South Atlantic, two modes are analysed in more detail: the South Atlantic dipole (SAD) mode, with centres at (15°S, Greenwich longitude) and at (37.5°S, 25°W) and the southwestern South Atlantic (SWSA) mode, with centres at (30°S, 40°W) and at the southern midlatitudes. The ENSO and SAD modes are lagged or lead connected depending on the period of analysis. An El Niņo (a La Niņa) precedes by up to 6 months the establishment of a positive (negative) SAD mode during the 1920 1930 and 1940 1980 periods. Otherwise, a positive (negative) SAD mode precedes by up to 1 year the establishment of a La Niņa (El Niņo) during the 1975 2000 period. On the other hand, the SWSA is strongly driven by the ENSO. The effects of both the SAD and SWSA modes on the South American rainfall are also discussed on a seasonal basis. In general, the SAD (ENSO) mode has a weak influence on the ENSO-related (SAD-related) rainfall anomalies over South America. On the other hand, in general, the SWSA and ENSO modes have a combined effect on rainfall of the southern and southeastern regions of South America. A particularly important result of the present analysis for climate monitoring and forecasting purposes seems to be the changing relations between the SAD and ENSO modes.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produįão anterior ā 2021 > DIDMD > Relations between ENSO...
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4. Conditions of access and use
Languageen
Target FileKayano_Relations.PDF
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5. Allied materials
Mirror Repositoryiconet.com.br/banon/2006/11.26.21.31
Next Higher Units8JMKD3MGPCW/43SKC35
Citing Item Listsid.inpe.br/bibdigital/2021/01.01.17.20 3
sid.inpe.br/mtc-m21/2012/07.13.14.56.22 2
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX; SCOPUS.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
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