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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/ArcPU
Repositorycptec.inpe.br/walmeida/2003/12.12.10.25   (restricted access)
Last Update2005:03.29.03.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2003/12.12.10.25.50
Metadata Last Update2021:02.10.18.59.22 (UTC) administrator
Secondary KeyINPE-10148-PRE/5676
ISSN0177-7971
Citation KeyKayanoAndr:2003:PrSeTe
TitlePropagation of the sea-surface temperature anomalies in the Tropical Atlantic.
Year2003
Secondary Date20030508
MonthOct.
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size1179 KiB
2. Context
Author1 Kayano, Mary Toshie
2 Andreoli, Rita Valeria
Resume Identifier1 8JMKD3MGP5W/3C9JHST
Group1 DMD-INPE-MCT-BR
Affiliation1 INPE/ Centro de Previsao de Tempo e Estudos Climaticos, BR-12227010 Sao Jose Dos Campos, SP, Brazil
e-Mail Addressdeicy@cptec.inpe.br
JournalMeteorology and Atmospheric Physics
Volume84
Number3-4
Pages275-284
History (UTC)2005-03-29 13:22:44 :: marciana -> administrator ::
2021-02-10 18:59:22 :: administrator -> marciana :: 2003
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsClimatic Variability
meridional modes
ocean
equatorial
AbstractThe evolving modes of the sea-surface temperature (SST) in the Tropical Atlantic on the short interannual (IA) timescale were obtained by performing the extended empirical orthogonal function (EEOF) analyses on this variable separately for the 106-year (1871-1976) and 20-year (1881-1900; 1901-1920; 1921-1940; 1941-1960) periods. The equatorial and inter-hemispheric patterns manifest in the first EEOF mode of each analysis as part of the short IA evolution of the SST anomalies in the Tropical Atlantic. Another outstanding feature of the first EEOF mode of each analysis concerns the propagations of the SST anomalies in the meridional direction within the 20degrees N-20degreesS band and in the zonal direction in the sector 40degreesW-20degrees W. For all analyses, the SST anomalies propagate northward from the equator to 15degreesN and southward from 20degreesN to 15degreesN, with the same sign anomalies merging approximately at 15degreesN. On the other hand, the SST anomalies propagate westward in the sector 40degreesW-20degrees W with a propagation rate close to that of the phase speed of the fastest baroclinic Rossby wave in the ocean. So, the observed propagations of the SST anomalies in the 20degreesN-20degreesS band might result from the combined effect of the surface oceanic currents in this band and the baroclinic Rossby waves in the ocean.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Propagation of the...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target FileKayano_Propagation of the sea-surface temperature
User Groupadministrator
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/43SKC35
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn label lineage mark mirrorrepository nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Description control
e-Mail (login)marciana
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