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1. Identity statement
Reference TypeConference Paper (Conference Proceedings)
Sitemtc-m21c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34R/44JUSDP
Repositorysid.inpe.br/mtc-m21c/2021/04.30.18.17
Last Update2021:04.30.18.17.11 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21c/2021/04.30.18.17.11
Metadata Last Update2022:04.03.22.29.11 (UTC) administrator
Secondary KeyINPE--PRE/
DOI10.5194/egusphere-egu21-12971
Citation KeyMortariniDAOBGSTAMC:2021:InAtSt
TitleInfluence of Atmospheric Stability on the flow dynamics within and above a dense Amazonian forest
Year2021
Access Date2024, May 19
Secondary TypePRE CI
Number of Files1
Size279 KiB
2. Context
Author 1 Mortarini, Luca
 2 Dias Júnior, Cléo Quaresma
 3 Acevedo, Otavio
 4 Oliveira, Pablo
 5 Brondani, Daiane
 6 Giostra, Umberto
 7 Sörgel, Matthias
 8 Tsokankunku, Anywhere
 9 Araújo, Alessandro
10 Machado, Luiz Augusto Toledo
11 Cava, Daniela
Resume Identifier 1
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10 8JMKD3MGP5W/3C9JHMS
ORCID 1 0000-0002-0543-2975
 2 0000-0003-4783-4689
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 4 0000-0003-1172-6870
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 6 0000-0001-8399-8715
 7 0000-0003-1745-8221
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 9 0000-0002-7361-5087
Group 1
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10 DISSM-CGCT-INPE-MCTI-GOV-BR
Affiliation 1 Institute of Atmospheric Sciences and Climate
 2 Instituto Nacional de Pesquisas da Amazônia (INPA)
 3 Universidade Federal de Santa Maria (UFSM)
 4 Universidade Federal do Rio Grande do Norte (UFRN)
 5 Instituto Nacional de Pesquisas da Amazônia (INPA)
 6 Università degli Studi di Urbino “Carlo Bo”
 7 Max Planck Institute for Chemistry
 8 Max Planck Institute for Chemistry
 9 Empresa Brasileira de Pesquisa Agropecuária (EMBRAPA)
10 Instituto Nacional de Pesquisas Espaciais (INPE)
11 Institute of Atmospheric Sciences and Climate
Author e-Mail Address 1
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10 Luiz.at.machado@gmail.com
Conference NameEGU General Assembly
Conference LocationOnline
Date19-30 apr.
PublisherEGU
History (UTC)2021-04-30 18:17:12 :: simone -> administrator ::
2022-04-03 22:29:11 :: administrator -> simone :: 2021
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
AbstractThis study provides a detailed analysis of the influence of atmospheric stratification on the flow dynamics above and within a dense forest for a 19-days campaign at the Amazon Tall Tower Observatory (ATTO) site. Observations taken at seven levels within and above the forest along an 81-meter and a 325-meter towers allow a unique investigation of the vertical evolution of the turbulent field in the roughness sublayer and in the surface layer above it. Five different stability classes were defined on the basis of the behavior of turbulent heat, momentum and CO2 fluxes and variance ratio as a function of h/L stability parameter (where h is the canopy height and L is the Obukhov length). The novelty is the identification of a super-stable (SS) regime (h/L>3) characterized by extremely low wind speeds, the almost completely suppression of turbulence and a clear dominance of submeso motions both above and within the forest. The obtained data classification was used to study the influence of atmospheric stratification on the vertical profiles of turbulent statistics. The spectral characteristics of coherent structures and of submeso motions (that may influence the energy and mass exchange above the Amazon forest) have been analyzed by wavelet analyses. The role of the main structures in momentum, heat and CO2 transport at the different levels inside and above the forest and in different diabatic conditions was thoroughly investigated through multiresolution and quadrant analyses. In unstable and neutral stability, the flow above the canopy appears modulated by ejections, whereas downward and intermittent sweeps dominate the transport inside the canopy. In the roughness sublayer (z £ 2h) the coherent structures dominating the transport within and above the canopy have a characteristic temporal scale of about 100 sec, whereas above this layer the transport is mainly driven by larger scale convection (temporal scale of about 15 min). In stable conditions the height of roughness sublayer progressively decreases with increasing stability reaching the minimum value (z<1.35h) in the SS regime. Above the canopy the flow is clearly dominated by ejections but characterized by a higher intermittency mainly in SS conditions. On the other hand, the rapid shear stress absorption in the highest part of the vegetation produces a less clear dominance of sweeps and a less defined role of odd and even quadrants inside the canopy in the transport of momentum, heat and CO2. In the weakly stable regime (0.15<h/L<1) transport is dominated in the roughness sublayer by canopy coherent structures with a characteristic temporal scale of about 60 sec. As stability increases the influence of low-frequency (submeso) processes, with a temporal scale of 20-30 min, on flow dynamics progressively increases and becomes dominant in the SS regime where the buoyancy strongly dampens or completely inhibits turbulent structures whereas the large-scale oscillations propagate in the interior of the canopy modulating the heat and CO2 transport.
AreaMET
Arrangementurlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > Influence of Atmospheric...
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4. Conditions of access and use
data URLhttp://mtc-m21c.sid.inpe.br/ibi/8JMKD3MGP3W34R/44JUSDP
zipped data URLhttp://mtc-m21c.sid.inpe.br/zip/8JMKD3MGP3W34R/44JUSDP
Languageen
Target FileEGU21-12971-print.pdf
User Groupsimone
Visibilityshown
Update Permissionnot transferred
5. Allied materials
Next Higher Units8JMKD3MGPCW/46KUATE
Citing Item List
Host Collectionurlib.net/www/2017/11.22.19.04
6. Notes
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