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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
IdentifierJ8LNKAN8RW/3C643G8
Repositorydpi.inpe.br/plutao/2012/06.21.20.36.42   (restricted access)
Last Update2012:08.29.16.55.18 (UTC) administrator
Metadata Repositorydpi.inpe.br/plutao/2012/06.21.20.36.43
Metadata Last Update2021:01.02.03.52.39 (UTC) administrator
DOI10.1007/s00704-011-0571-0
ISSN0177-798X
Labellattes: 9873289111461387 2 SilvaFreiGiel:2012:RoCoTr
Citation KeySilvaFreiGiel:2012:RoCoTr
TitleNumerical simulation of the diurnal cycle of rainfall in SW Amazon basin during the 1999 rainy season: the role of convective trigger function
Year2012
Access Date2024, Mar. 28
Secondary TypePRE PI
Number of Files1
Size739 KiB
2. Context
Author1 Silva, Cláudio Moisés Santos e
2 Freitas, Saulo Ribeiro de
3 Gielow, Ralf
Resume Identifier1
2 8JMKD3MGP5W/3C9JJ7M
3 8JMKD3MGP5W/3C9JJ53
Group1
2 DMD-CPT-INPE-MCTI-GOV-BR
Affiliation1 Universidade Federal do Rio Grande do Norte
2 Instituto Nacional de Pesquisas Espaciais (INPE)
Author e-Mail Address1 claudio@dfte.ufrn.br
2 saulo.freitas@cptec.inpe.br
e-Mail Addresssaulo.freitas@cptec.inpe.br
JournalTheoretical and Applied Climatology
Volume109
Pages473–483
Secondary MarkB2_ASTRONOMIA_/_FÍSICA A2_CIÊNCIAS_AGRÁRIAS_I B1_GEOCIÊNCIAS A2_GEOGRAFIA A2_INTERDISCIPLINAR
History (UTC)2012-06-22 00:11:01 :: lattes -> administrator :: 2012
2012-07-25 08:17:16 :: administrator -> secretaria.cpa@dir.inpe.br :: 2012
2012-08-29 16:55:18 :: secretaria.cpa@dir.inpe.br -> administrator :: 2012
2021-01-02 03:52:39 :: administrator -> marciana :: 2012
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractIn continental areas, the maximum rainfall simulated with the Brazilian developments on the Regional Atmospheric Modeling System (BRAMS) occurs around 4 h earlier than the one observed with rain gauges. This work presents the successful implementation of a new convective trigger function (CTF) in the convective parameterization scheme used in BRAMS that corrects this misfit between model and observations. The importance of the CTF formulation on the diurnal cycle of rainfall over the Amazon Basin is reflected by the following numbers: Over Rondonia (SWAmazonia), the original version of BRAMS simulates the maximum rainfall at 1400 UTC (1000 LST), with the new CTF maximum shifting to 1800 UTC (1400 LST), while the S-band radar rainfall maximum is at 1900 UTC (1500 LST). This is attributed to two factors: (1) the new CTF is now coupled to the sensible and latent heat fluxes at surface; (2) during the early morning, the convective available potential energy is reduced.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção anterior à 2021 > DIDMD > Numerical simulation of...
doc Directory Contentaccess
source Directory Contentthere are no files
agreement Directory Contentthere are no files
4. Conditions of access and use
Languageen
Target FileSantoseSilva_et_al_2012.pdf
User Groupadministrator
lattes
secretaria.cpa@dir.inpe.br
Visibilityshown
Archiving Policydenypublisher denyfinaldraft12
Read Permissiondeny from all and allow from 150.163
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/43SKC35
DisseminationWEBSCI; PORTALCAPES; MGA.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
Empty Fieldsalternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel format isbn keywords lineage mark mirrorrepository month nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project readergroup rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype typeofwork url
7. Description control
e-Mail (login)marciana
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