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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16b.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifierx6e6X3pFwXQZ3DUS8rS5/C7KAA
Repositorycptec.inpe.br/walmeida/2004/05.11.09.03   (restricted access)
Last Update2005:04.25.03.00.00 (UTC) administrator
Metadata Repositorycptec.inpe.br/walmeida/2004/05.11.09.03.36
Metadata Last Update2021:02.10.18.59.45 (UTC) administrator
Secondary KeyINPE-11387-PRE/6824
ISSN0899-8418
Citation KeyMarengo:1992:InVaSu
TitleInterannual variability of surface climate in the Amazon basin
Year1992
Monthdec.
Access Date2024, May 02
Secondary TypePRE PI
Number of Files1
Size290 KiB
2. Context
AuthorMarengo, Jose Antonio
GroupDMD-INPE-MCT-BR
AffiliationCPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brazil
e-Mail Addressfabia@cptec.inpe.br
JournalInternational Journal of Climatology
Volume12
Number8
Pages853-863
History (UTC)2005-04-25 17:48:40 :: Fabia -> administrator ::
2008-06-10 19:46:07 :: administrator -> estagiario ::
2010-05-11 16:53:09 :: estagiario -> administrator ::
2021-02-10 18:59:45 :: administrator -> marciana :: 1992
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordsinterannual climate variability
Amazon basin
rainfall anomalies
AbstractThis empirical study examines the circulation mechanisms of anomalously wet and dry years in the Amazon basin. Data sources include surface ship observations in the tropical Atlantic, eastern Pacific, and Indian Oceans, as well as various hydrometeorological indices in Amazonia during 1951 1983. Rainfall and river water level anomalies in northern Amazonia are associated with distinct circulation patterns in the tropical Atlantic, particularly at the March April peak of the rainy season. Thus, abundant rainfall in northern Amazonia and high Rio Negro water levels are accompanied by a strong North Atlantic high, steep meridional pressure gradient on its equatorward side, accelerated North-east trades, and cool surface waters in the tropical North Atlantic. The intensified North-east trades may entail enhanced boundary-layer moisture transport from the tropical North Atlantic into the Amazon basin. This ensemble of atmospheric and oceanic anomalies is characteristic of, but not limited to, the high phase of the Southern Oscillation (defined by anomalously high/low pressure at Tahiti/Darwin).
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Interannual variability of...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target Filemarengo_interannualvariability.pdf
User Groupadministrator
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft
Read Permissiondeny from all and allow from 150.163
5. Allied materials
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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