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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/3S4RNNE
Repositorysid.inpe.br/mtc-m21c/2018/10.26.13.23
Last Update2018:10.26.13.23.22 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2018/10.26.13.23.22
Metadata Last Update2019:01.14.17.06.37 (UTC) administrator
DOI10.3390/atmos9100399
ISSN2073-4433
Citation KeyNevesFiscRaas:2018:LoCoTu
TitleLocal convection and turbulence in the Amazonia using Large Eddy Simulation model
Year2018
MonthOct.
Access Date2024, Apr. 25
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size4662 KiB
2. Context
Author1 Neves, Theomar
2 Fisch, Gilberto
3 Raasch, Siegfried
ORCID1 0000-0002-5908-7660
2 0000-0001-6668-9988
Group1 MET-MET-SESPG-INPE-MCTIC-GOV-BR
Affiliation1 Instituto Nacional de Pesquisas Espaciais (INPE)
2 Centro Técnico Aeroespacial (CTA/IAE)
3 Leibniz University Hannover
Author e-Mail Address1 neves.theomar@gmail.com
2 fisch.gilberto@gmail.com
3 raasch@muk.uni-hannover.de
JournalAtmosphere
Volume9
Number10
Pagese399
Secondary MarkB3_ENGENHARIAS_III B3_ENGENHARIAS_I B3_CIÊNCIAS_AMBIENTAIS B4_ENGENHARIAS_II B5_GEOCIÊNCIAS
History (UTC)2018-10-26 13:23:22 :: simone -> administrator ::
2018-10-26 13:23:22 :: administrator -> simone :: 2018
2018-10-26 13:24:00 :: simone -> administrator :: 2018
2019-01-14 17:06:37 :: administrator -> simone :: 2018
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Version Typepublisher
AbstractUsing a high resolution model of Large Eddies Simulation (LES), named PALM from PArallel LES Model, a set of simulations were performed to understand how turbulence and convection behave in a pasture and forest sites in Amazonia during the dry and rainy seasons. Related to seasonality, dry period presented higher differences of values (40Wm-2) and patterns over the sites, while in the wet period have more similar characteristics (difference of -10 W m-2). The pasture site had more convection than the forest, with effective mixing and a deeper boundary layer (2600 m). The vertical decrease of sensible heat flux with altitude fed convection and also influenced the convective boundary layer (CBL) height. Regarding the components of turbulent kinetic energy equation, the thermal production was the most important component and the dissipation rate responded with higher growth, especially in cases of greatest mechanical production at the forest surface reaching values up to -20.0.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção pgr ATUAIS > MET > Local convection and...
doc Directory Contentaccess
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4. Conditions of access and use
data URLhttp://urlib.net/ibi/8JMKD3MGP3W34R/3S4RNNE
zipped data URLhttp://urlib.net/zip/8JMKD3MGP3W34R/3S4RNNE
Languageen
Target Fileneves_local.pdf
User Groupsimone
Reader Groupadministrator
simone
Visibilityshown
Archiving Policyallowpublisher allowfinaldraft
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/3F35TRS
Citing Item Listsid.inpe.br/bibdigital/2013/10.15.01.34 1
DisseminationWEBSCI; PORTALCAPES; SCOPUS.
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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