| 1. Identity statement | ||||
| Reference Type | Journal Article | |||
| Site | mtc-m21d.sid.inpe.br | |||
| Holder Code | isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S | |||
| Identifier | 8JMKD3MGP3W34T/44UH33P | |||
| Repository | sid.inpe.br/mtc-m21d/2021/06.28.13.38 (restricted access) | |||
| Last Update | 2021:06.28.13.38.25 (UTC) simone | |||
| Metadata Repository | sid.inpe.br/mtc-m21d/2021/06.28.13.38.25 | |||
| Metadata Last Update | 2022:04.03.22.27.24 (UTC) administrator | |||
| DOI | 10.1016/j.agrformet.2021.108457 | |||
| ISSN | 0168-1923 | |||
| Citation Key | CorreaDCSBAOMMMTALWM:2021:CaStGr | |||
| Title | A case study of a gravity wave induced by Amazon forest orography and low level jet generation  | |||
| Year | 2021 | |||
| Month | Sept. | |||
| Access Date | 2024, May 19 | |||
| Type of Work | journal article | |||
| Secondary Type | PRE PI | |||
| Number of Files | 1 | |||
| Size | 10200 KiB | |||
| 2. Context | ||||
| Author | 1 Correa, Polari B. 2 Dias Júnior, Cléo Quaresma 3 Cava, Daniela 4 Sorgel, Matthias 5 Botia, Santiago 6 Acevedo, Otávio 7 Oliveira, Pablo E. S. 8 Manzi, Antonio Ocimar 9 Machado, Luiz Augusto Toledo 10 Martins, Hardiney dos Santos 11 Tsokankunku, Anywhere 12 Araújo, Alessandro C. de 13 Lavric, Jost V. 14 Walter, David 15 Mortarini, Luca | |||
| Resume Identifier | 1 2 3 4 5 6 7 8 9 8JMKD3MGP5W/3C9JHMS | |||
| Group | 1 2 3 4 5 6 7 8 DIMNT-CGCT-INPE-MCTI-GOV-BR 9 DISSM-CGCT-INPE-MCTI-GOV-BR | |||
| Affiliation | 1 Instituto Nacional de Pesquisas da Amazônia (INPA) 2 Instituto Nacional de Pesquisas da Amazônia (INPA) 3 Consiglio Nazionale delle Ricerche (ISAC-CNR) 4 Max Planck Institute for Chemistry 5 Max Planck Institute for Biogeochemistry 6 Universidade Federal de Santa Maria (UFSM) 7 Universidade Federal do Rio Grande do Norte (UFRN) 8 Instituto Nacional de Pesquisas Espaciais (INPE) 9 Instituto Nacional de Pesquisas Espaciais (INPE) 10 Instituto Federal do Pará (IFPA) 11 Max Planck Institute for Chemistry 12 Embrapa Amazônia Oriental 13 Max Planck Institute for Biogeochemistry 14 Max Planck Institute for Chemistry 15 Consiglio Nazionale delle Ricerche (ISAC-CNR) | |||
| Author e-Mail Address | 1 2 cleo.quaresma@ifpa.edu.br 3 4 5 6 7 8 aomanzi@gmail.com 9 Luiz.at.machado@gmail.com | |||
| Journal | Agricultural and Forest Meteorology | |||
| Volume | 307 | |||
| Pages | e108457 | |||
| Secondary Mark | A1_INTERDISCIPLINAR A1_GEOCIÊNCIAS A1_ENGENHARIAS_III A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A1_BIODIVERSIDADE A2_CIÊNCIAS_BIOLÓGICAS_I B2_ASTRONOMIA_/_FÍSICA | |||
| History (UTC) | 2021-06-28 13:38:25 :: simone -> administrator :: 2021-06-28 13:38:26 :: administrator -> simone :: 2021 2021-06-28 13:41:00 :: simone -> administrator :: 2021 2022-04-03 22:27:24 :: administrator -> simone :: 2021 | |||
| 3. Content and structure | ||||
| Is the master or a copy? | is the master | |||
| Content Stage | completed | |||
| Transferable | 1 | |||
| Content Type | External Contribution | |||
| Version Type | publisher | |||
| Keywords | Coherent structures Gravity waves Low-level jet Stable boundary layer wave-turbulence interaction | |||
| Abstract | We investigated the role of turbulent coherent structures (CS), gravity waves (GW) and low-level jet (LLJ) propagation in the flow dynamics of the Nocturnal Boundary Layer (NBL) within and above a forest canopy at the Amazon Tall Tower Observatory (ATTO), in Central Amazon. Seven levels of wind velocity and temperature measurements allowed the study of the flow structure below and above the surface layer. We analyzed one dynamically rich night in 2015, which includes three distinct periods. In the first one, the NBL is characterized by CS generated at the canopy top. In the second period, the change in wind direction triggers the onset of a orographic GW above the roughness sublayer. The wave, suppressing the propagation of CS, strongly influences the boundary layer structure, both above and below the canopy. In the third period, low turbulence intensity at the canopy top enables the development of a LLJ. As the jet shear layer propagates upward, it disrupts the wave oscillations, while LLJ dominates the flow dynamics. The wavelet analyses identified i) turbulent and non-turbulent structures with different length and time-scales; ii) coupling of the flow at different levels and the vertical propagation of turbulent and wave motions; and iii) the ability of turbulent and low frequency processes associated with the orographic GW to penetrate within the canopy. Further, scalar measurements of methane, carbon monoxide and carbon dioxide identified the LLJ nose as upward limit for how far scalars can be transported. | |||
| Area | MET | |||
| Arrangement | urlib.net > BDMCI > Fonds > Produção a partir de 2021 > CGCT > A case study... | |||
| doc Directory Content | access | |||
| source Directory Content | there are no files | |||
| agreement Directory Content |
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| 4. Conditions of access and use | ||||
| Language | en | |||
| Target File | correa_case.pdf | |||
| User Group | simone | |||
| Reader Group | administrator simone | |||
| Visibility | shown | |||
| Archiving Policy | denypublisher denyfinaldraft24 | |||
| Read Permission | deny from all and allow from 150.163 | |||
| Update Permission | not transferred | |||
| 5. Allied materials | ||||
| Next Higher Units | 8JMKD3MGPCW/46KUATE | |||
| Citing Item List | sid.inpe.br/bibdigital/2022/04.03.22.23 2 | |||
| Dissemination | WEBSCI; PORTALCAPES. | |||
| Host Collection | urlib.net/www/2021/06.04.03.40 | |||
| 6. Notes | ||||
| Empty Fields | alternatejournal archivist callnumber copyholder copyright creatorhistory descriptionlevel e-mailaddress format isbn label lineage mark mirrorrepository nextedition notes number orcid parameterlist parentrepositories previousedition previouslowerunit progress project rightsholder schedulinginformation secondarydate secondarykey session shorttitle sponsor subject tertiarymark tertiarytype url | |||
| 7. Description control | ||||
| e-Mail (login) | simone | |||
| update | ||||