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1. Identity statement
Reference TypeJournal Article
Sitemarte3.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3r59YCT/GTgAD
Repositorysid.inpe.br/iris@1905/2005/07.27.07.22   (restricted access)
Last Update2010:03.03.16.36.28 (UTC) administrator
Metadata Repositorysid.inpe.br/iris@1905/2005/07.27.07.22.37
Metadata Last Update2021:02.10.18.35.44 (UTC) administrator
Secondary KeyINPE-9072-PRE/4748
ISSN0259-8477
Label6224
Citation KeyBuchmannSilvMour:1986:TrCoOv
TitleTransient convection over the amazon Bolivia region and the dynamics of droughts over northeast Brazil
ProjectModelagem atmosférica e oceanos
Year1986
Secondary Date20060109
Access Date2024, Apr. 28
Secondary TypePRE PI
Number of Files1
Size1651 KiB
2. Context
Author1 Buchmann, J.
2 Silva Dias, Pedro Leite da
3 Moura, A. D.
Group1
2
3 CPT-INPE-BR
Affiliation1 Departamento de meteorologia
2 Instituto Astronômico e Geofísico
3 Instituto Nacional de Pesquisas Espaciais (INPE)
e-Mail Addressatus@cptec.inpe.br
JournalArchives for Meteorology Geophysics, and Bioclimatology. Series A - Meteorology and atmospheric physics
Volume34
Number3-4
Pages367-384
History (UTC)2005-07-27 07:22:38 :: administrator -> jefferson ::
2006-01-09 09:51:35 :: jefferson -> administrator ::
2008-06-09 16:09:12 :: administrator -> jefferson ::
2010-07-08 11:25:57 :: jefferson -> administrator :: 1986
2021-02-10 18:35:44 :: administrator -> marciana :: 1986
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
KeywordsNortheast Brazil
region Bolivia
Drought
Amazon
convections
AbstractA two-layer, nonlinear, equatoria, B-plane model, in p-coordinates is used to study the atmospheric response to a large-scale heat source varying in time. The heat source is meant to represent a convective burst whith total duration of approximately 48 hours over the Amazon/Bolívia region. The boundary conditions used are meridional velocity zero at 60ºN and 60ºS, w=0 at the top and zero geometric velocity at the lower boundary. Sensitivity study was done which includes initial state at rest, compared with realistic initial flow. The scale of the heat source is 1500km in latitude and longitude and it is centered at 10ºS. Special attention is paid to the distribution and intensity of the induced vertical motion. The model is integrated for two days and the preliminary resilts show agreement with the observed 200 mb flow. Of interest is the establishment of a trough and descending motion to the northeast of the heat source.A conjecture is thus made that the Amazon heat source and its fluctuations bear nome realtionship with the drought problem over Northeast Brazil.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > CGCPT > Transient convection over...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target FileTRANSIENT CONVECTION....pdf
User Groupadministrator
jefferson
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EUPEJL
DisseminationPORTALCAPES
Host Collectionsid.inpe.br/banon/2001/04.03.15.36
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyright creatorhistory descriptionlevel documentstage doi electronicmailaddress format isbn lineage mark mirrorrepository month nextedition notes orcid parameterlist parentrepositories previousedition previouslowerunit progress readergroup resumeid rightsholder schedulinginformation secondarymark session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url versiontype
7. Description control
e-Mail (login)marciana
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