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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZGivnJUY/Mc3kL
Repositorysid.inpe.br/mtc-m15@80/2006/08.18.13.49   (restricted access)
Last Update2006:08.18.13.49.54 (UTC) administrator
Metadata Repositorysid.inpe.br/mtc-m15@80/2006/08.18.13.49.56
Metadata Last Update2021:02.10.19.00.52 (UTC) administrator
Secondary KeyINPE-14160-PRE/9293
ISSN0143-1161
Citation KeyPezziCataChal:2006:SaObPa
TitleSatellite observations of the Pacific tropical instability waves characteristics and their interannual variability
Year2006
Secondary Date20060818
MonthApr.
Access Date2024, Apr. 25
Secondary TypePRE PI
Number of Files1
Size1049 KiB
2. Context
Author1 Pezzi, Luciano Ponzi
2 Catalbiano, A. C.
3 Chalenor, P.
Resume Identifier1 8JMKD3MGP5W/3C9JHM8
Group1 DMD-INPE-MCT-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE), Centro de Previsão de Tempo e Estudos Climáticos (CPTEC)
e-Mail Addressatus@cptec.inpe.br
JournalInternational Journal of Remote Sensing
Volume27
Number08
Pages1581-1599
History (UTC)2006-09-20 13:51:46 :: deicy -> administrator ::
2006-11-17 23:06:44 :: administrator -> deicy ::
2007-03-27 17:27:29 :: deicy -> administrator ::
2013-03-12 03:31:43 :: administrator -> deicy :: 2006
2013-04-05 15:05:11 :: deicy -> administrator :: 2006
2021-02-10 19:00:52 :: administrator -> marciana :: 2006
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordstropical Instability waves
satellite
tropical Pacific
sea surface temperature
AbstractDescriptions of tropical instability wave (TIW) characteristics in the tropical Pacific Ocean as a function of the large-scale climate conditions and interannual variability, such as the El Niño southern oscillation, are made based on satellite data. As others have found, the TIW ocean atmosphere coupling is caused by atmospheric boundary layer instability and mixing. Our observational investigation extends some of these previous findings and suggests that this mechanism of coupled variability of the wind and sea surface temperature may occur not only during La Nina years, when TIWs are more active, but whenever the TIWs are active. The sea surface temperature and height anomaly covariability phase shift might occur also independent of the TIW season activity. There is evidence that TIW activity increases when under strengthened wind stress conditions either in La Nina years or, by analogy, when oceanic numerical simulations are carried out with stronger wind stress. Observational results show larger TIW wavelengths and shorter periods when the ocean is under the action of strengthened wind stress. On this observational study this occurs when La Nina conditions prevail on the equatorial Pacific.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Satellite observations of...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target FilePezzi. satellite.pdf
User Groupadministrator
deicy
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Previous Editionsid.inpe.br/iris@1915/2005/12.13.19.32
Next Higher Units8JMKD3MGPCW/43SKC35
DisseminationWEBSCI; PORTALCAPES; MGA; COMPENDEX.
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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