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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3r59YD9/G4d8x
Repositorysid.inpe.br/iris@1915/2005/05.05.11.36
Last Update2005:05.05.03.00.00 (UTC) administrator
Metadata Repositorysid.inpe.br/iris@1915/2005/05.05.11.36.36
Metadata Last Update2021:02.10.19.00.32 (UTC) administrator
Secondary KeyINPE-9104-PRE/4779
ISSN0894-8755
Citation KeyRaoChapFernFran:2002:RoWaVa
TitleA diagnosis of rainfall over South America during the 1997/98 El Nino event. Part II: Roles of water vapor transport and stationary waves
Year2002
Secondary Date20020612
MonthMar.
Access Date2024, May 18
Secondary TypePRE PI
Number of Files1
Size998 KiB
2. Context
Author1 Rao, Vadlamudi Brahmananda
2 Chapa, Srinivasa R.
3 Fernandez, Julio Pablo Reyes
4 Franchito, Sergio Henrique
Resume Identifier1 8JMKD3MGP5W/3C9JJAJ
2
3 8JMKD3MGP5W/3C9JHKJ
4 8JMKD3MGP5W/3C9JJ82
Group1 DMD-INPE-MCT-BR
2 DMD-INPE-MCT-BR
3
4 DMD-INPE-MCT-BR
Affiliation1 INPE- Sao Jose dos Campos-12227-010-SP-Brasil
2 Instituto Nacional de Pesquisas Espaciais(INPE/CPTEC)
3
4 Instituto Nacional de Pesquisas Espaciais(INPE/CPTEC)
e-Mail Addressatus@cptec.inpe.br
JournalJournal of Climate
Volume15
Number5
Pages512-521
History (UTC)2005-05-05 11:36:37 :: fabia -> administrator ::
2006-11-17 23:12:36 :: administrator -> estagiario ::
2007-09-05 19:02:43 :: estagiario -> administrator ::
2008-06-10 19:51:47 :: administrator -> estagiario ::
2010-05-11 16:55:56 :: estagiario -> administrator ::
2021-02-10 19:00:32 :: administrator -> marciana :: 2002
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsSoutheast PacificBrasil
oscillation
propagation
blocking
variability
climate
summer
GCM
El Nino
AbstractA diagnosis of rainfall over South America (SA)during the 1997/ 98 El Nino year is made examining the roles of water vapor transport and stationary waves. It is found that the low-level jet (LLJ)on the eastern side of the central Andes is stronger during the El Nino event and transports more moisture. This seems to be the source for higher rainfall over southeast SA noted during the El Nino years. A calculation of three-dimensional stationary wave activity (F-s)for 1997 and 1998 showed that in the summer of 1996/97 stationary waves propagate poleward and eastward from midlatitudes into the higher latitudes to the west of south SA and then propagate equatorward to the east of SA. During the autumn of 1997, the vertical component of F-s is consistent with a blocking high over the southeast Pacific. To the east of this high cold air advection from Antarctica occurs, and to the west warm air advection occurs. This is consistent with negative and positive centers seen in the vertical component of F-s to the east and west of south SA. The rainfall anomalies during a particular season seem to be due to multiple causes and this complicates a direct connection between them. Although over the southeast of SA, the higher rainfall during 1997 and 1998 can be attributed to some specific causes such as higher water vapor transport by LLJ in summer of 1997/ 98, in other parts such an association was not possible.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > A diagnosis of...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
data URLhttp://mtc-m16b.sid.inpe.br/ibi/6qtX3pFwXQZ3r59YD9/G4d8x
zipped data URLhttp://mtc-m16b.sid.inpe.br/zip/6qtX3pFwXQZ3r59YD9/G4d8x
Languageen
Target FileVadlamudi_A diagnosis of rainfall_Parte II.pdf
User Groupadministrator
estagiario
fabia
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher6 allowfinaldraft
Read Permissionallow from all
5. Allied materials
Next Higher Units8JMKD3MGPCW/43SKC35
Citing Item Listsid.inpe.br/mtc-m21/2012/07.13.15.00 2
DisseminationWEBSCI; PORTALCAPES; AGU; MGA; COMPENDEX.
Host Collectioncptec.inpe.br/walmeida/2003/04.25.17.12
6. Notes
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