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1. Identity statement
Reference TypeJournal Article
Siteplutao.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W/45U8BC8
Repositorysid.inpe.br/plutao/2021/12.09.15.55
Last Update2021:12.15.10.55.37 (UTC) lattes
Metadata Repositorysid.inpe.br/plutao/2021/12.09.15.55.31
Metadata Last Update2022:04.03.22.27.20 (UTC) administrator
DOI10.5194/gmd-14-5393-2021
ISSN1991-959X
Labellattes: 9873289111461387 1 FreitasGrelLi:2021:ReDeEx
Citation KeyFreitasGrelLi:2021:ReDeEx
TitleThe Grell-Freitas (GF) convection parameterization: recent developments, extensions, and applications
Year2021
Access Date2024, May 19
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size16813 KiB
2. Context
Author1 Freitas, Saulo Ribeiro de
2 Grell, Georg A.
3 Li, Haiqin
Resume Identifier1 8JMKD3MGP5W/3C9JJ7M
Group1 DIMNT-CGCT-INPE-MCTI-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 National Oceanic and Atmospheric Administration (NOAA)
3 National Oceanic and Atmospheric Administration (NOAA)
Author e-Mail Address1 saulo.r.de.freitas@gmail.com
JournalGeoscientific Model Development
Volume14
Number9
Pages5393-5411
History (UTC)2021-12-09 15:55:31 :: lattes -> administrator ::
2021-12-15 10:54:16 :: administrator -> lattes :: 2021
2021-12-15 10:55:38 :: lattes -> administrator :: 2021
2022-04-03 22:27:20 :: administrator -> simone :: 2021
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractRecent developments and options in the GF (Grell and Freitas, 2014; Freitas et al., 2018) convection parameterization are presented. The parameterization has been expanded to a trimodal spectral size to simulate three convection modes: shallow, congestus, and deep. In contrast to usual entrainment and detrainment assumptions, we assume that beta functions (BFs), commonly applied to represent probability density functions (PDFs), can be used to characterize the vertical mass flux profiles for the three modes and use the BFs to derive entrainment and detrainment rates. We also added a new closure for nonequilibrium convection that improved the simulation of the diurnal cycle of convection, with a better representation of the transition from shallow to deep convection regimes over land. The transport of chemical constituents (including wet deposition) can be treated inside the GF scheme. The tracer transport is handled in flux form and is mass-conserving. Finally, the cloud microphysics have been extended to include the ice phase to simulate the conversion from liquid water to ice in updrafts with resulting additional heat release and the melting from snow to rain.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > The Grell-Freitas (GF)...
doc Directory Contentaccess
source Directory Contentthere are no files
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/8JMKD3MGP3W/45U8BC8
zipped data URLhttp://urlib.net/zip/8JMKD3MGP3W/45U8BC8
Languageen
Target Filefreitas_greel.pdf
User Grouplattes
Reader Groupadministrator
lattes
Visibilityshown
Archiving Policyallowpublisher allowfinaldraft
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/46KUATE
Citing Item Listsid.inpe.br/bibdigital/2022/04.03.22.23 2
sid.inpe.br/mtc-m21/2012/07.13.14.59.52 1
DisseminationWEBSCI; PORTALCAPES.
Host Collectiondpi.inpe.br/plutao@80/2008/08.19.15.01
6. Notes
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