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Registros recuperados : 7 | |
1. | | CAVA, D.; MORTARINI, L.; DIAS JÚNIOR, C. Q.; BRONDANI, D.; ACEVEDO, O.; OLIVEIRA, P.; GIOSTRA, U.; MANZI, A. O.; ARAUJO, A. C. de; TSOKANKUNKU, A.; SÖRGEL, M. Impact of Atmospheric Stability on Vertical Propagation of Submeso and Coherent Structure in a Dense Amazon Forest. In: EGU GENERAL ASSEMBLY, 2022, Viena. Programme. [S.l.]: EGU, 2022. Biblioteca(s): Embrapa Amazônia Oriental. |
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2. | | OLVEIRA, P. E. S.; ACEVEDO, O. C.; SÖRGEL, M.; TSOKANKUNKU, A.; WOLFF, S.; ARAUJO, A. C. de; SOUZA, R. A. F.; SÁ, M. O.; MANZI, A. O.; ANDREAE, M. O. Nighttime wind and scalar variability within and above an Amazonian canopy. Atmospheric Chemistry and Physics, v. 18, n. 5, p. 3083-3099, 2018. Biblioteca(s): Embrapa Amazônia Oriental. |
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3. | | RINGSDORF, A.; EDTBAUER, A.; ARELLANO, J. V.-G. de; PFANNERSTILL, E. Y.; GROMOV, S.; KUMAR, V.; POZZER, A.; WOLFF, S.; TSOKANKUNKU, A.; SOERGEL, M.; SÁ, M. O.; ARAUJO, A. C. de; DITAS, F.; POEHLKER, C.; LELIEVELD, J.; WILLIAMS, J. Inferring the diurnal variability of OH radical concentrations over the Amazon from BVOC measurements. Scientific Reports, v. 13, Article number: 14900, 2023. Biblioteca(s): Embrapa Amazônia Oriental. |
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4. | | PFANNERSTILL, E. Y.; REIJRINK, N. G.; EDTBAUER, A.; RINGSDORF, A.; ZANNONI, N.; ARAUJO, A. C. de; DITAS, F.; HOLANDA, B. A.; SÁ, M. O.; TSOKANKUNKU, A.; WALTER, D.; WOLFF, S.; LAVRIC, J. V.; PÖHLKER, C.; SÖRGEL, M.; WILLIAMS, J. Total OH reactivity over the Amazon rainforest: variability with temperature, wind, rain, altitude, time of day, season, and an overall budget closure. Atmospheric Chemistry and Physics, v. 21, n. 8, p. 6231-6256, 2021. Biblioteca(s): Embrapa Amazônia Oriental. |
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5. | | MORTARINI, L.; DIAS-JÚNIOR, C. Q.; ACEVEDO, O.; OLIVEIRA, P. E. S.; TSOKANKUNKU, A.; SÖRGEL. M.; MANZI, A. O.; ARAUJO, A. C. de; BRONDANI, D. V.; TORO, I. M. C.; GIOSTRA, U.; CAVA, D. Vertical propagation of submeso and coherent structure in a tall and dense amazon forest in different stability conditions. PART II: Coherent structures analysis. Agricultural and Forest Meteorology, v. 322, 108993, July 2022. Biblioteca(s): Embrapa Amazônia Oriental. |
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6. | | CORRÊA, P. B.; DIAS-JÚNIOR, C. Q.; CAVA, D.; SÖRGEL, M.; BOTÍA, S.; ACEVEDO, O.; OLIVEIRA, P. E. S.; MANZI, A. O.; MACHADO, L. A. T.; MARTINS, H. dos S.; TSOKANKUNKU, A.; ARAUJO, A. C. de; LAVRIC, J. V.; WALTER, D.; MORTARINI, L. A case study of a gravity wave induced by Amazon forest orography and low level jet generation. Agricultural and Forest Meteorology, v. 307, Article 108457, 2021. Biblioteca(s): Embrapa Amazônia Oriental. |
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7. | | PFANNERSTILL, E. Y.; NÖLSCHER, A. C.; YÁÑEZ-SERRANO, A. M.; BOURTSOUKIDIS, E.; KEBEL, S.; JANSSEN, R. H. H.; TSOKANKUNKU, A.; WOLFF, S.; SÖRGEL, M.; SÁ, M. O.; ARAUJO, A. C. de; WALTER, D.; LAVRIC, J.; DIAS-JUNIOR, C. Q.; KESSELMEIER, J.; WILLIAMS, J. Total OH reactivity changes over the Amazon rainforest during an El Niño event. Frontiers in Forests and Global Change, v. 1, Article 12, Dec. 2018. Biblioteca(s): Embrapa Amazônia Oriental. |
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Registros recuperados : 7 | |
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Registro Completo
Biblioteca(s): |
Embrapa Amazônia Oriental. |
Data corrente: |
18/05/2018 |
Data da última atualização: |
20/05/2022 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
OLVEIRA, P. E. S.; ACEVEDO, O. C.; SÖRGEL, M.; TSOKANKUNKU, A.; WOLFF, S.; ARAUJO, A. C. de; SOUZA, R. A. F.; SÁ, M. O.; MANZI, A. O.; ANDREAE, M. O. |
Afiliação: |
Pablo E. S. Oliveira, UFSM; Otávio C. Acevedo, UFSM; Matthias Sörgel, Max Planck Institute for Chemistry; Anywhere Tsokankunku, Max Planck Institute for Chemistry; Stefan Wolff, Max Planck Institute for Chemistry; ALESSANDRO CARIOCA DE ARAUJO, CPATU; Rodrigo A. F. Souza, UEA; Marta O. Sá, INPA; Antônio O. Manzi, INPA; Meinrat O. Andreae, Max Planck Institute for Chemistry. |
Título: |
Nighttime wind and scalar variability within and above an Amazonian canopy. |
Ano de publicação: |
2018 |
Fonte/Imprenta: |
Atmospheric Chemistry and Physics, v. 18, n. 5, p. 3083-3099, 2018. |
DOI: |
10.5194/acp-18-3083-2018 |
Idioma: |
Inglês |
Conteúdo: |
Nocturnal turbulent kinetic energy (TKE) and fluxes of energy, CO2 and O3 between the Amazon forest and the atmosphere are evaluated for a 20-day campaign at the Amazon Tall Tower Observatory (ATTO) site. The distinction of these quantities between fully turbulent (weakly stable) and intermittent (very stable) nights is discussed. Spectral analysis indicates that low-frequency, nonturbulent fluctuations are responsible for a large portion of the variability observed on intermittent nights. In these conditions, the low-frequency exchange may dominate over the turbulent transfer. In particular, we show that within the canopy most of the exchange of CO2 and H2O happens on temporal scales longer than 100 s. At 80 m, on the other hand, the turbulent fluxes are almost absent in such very stable conditions, suggesting a boundary layer shallower than 80 m. The relationship between TKE and mean winds shows that the stable boundary layer switches from the very stable to the weakly stable regime during intermittent bursts of turbulence. In general, fluxes estimated with long temporal windows that account for low-frequency effects are more dependent on the stability over a deeper layer above the forest than they are on the stability between the top of the canopy and its interior, suggesting that low-frequency processes are controlled over a deeper layer above the forest. |
Palavras-Chave: |
Energia cinética turbulenta; TKE. |
Thesagro: |
Dióxido de Carbono; Vento. |
Thesaurus NAL: |
Amazonia. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/177153/1/Oliveira-ACP-2018.pdf
|
Marc: |
LEADER 02255naa a2200301 a 4500 001 2091667 005 2022-05-20 008 2018 bl uuuu u00u1 u #d 024 7 $a10.5194/acp-18-3083-2018$2DOI 100 1 $aOLVEIRA, P. E. S. 245 $aNighttime wind and scalar variability within and above an Amazonian canopy.$h[electronic resource] 260 $c2018 520 $aNocturnal turbulent kinetic energy (TKE) and fluxes of energy, CO2 and O3 between the Amazon forest and the atmosphere are evaluated for a 20-day campaign at the Amazon Tall Tower Observatory (ATTO) site. The distinction of these quantities between fully turbulent (weakly stable) and intermittent (very stable) nights is discussed. Spectral analysis indicates that low-frequency, nonturbulent fluctuations are responsible for a large portion of the variability observed on intermittent nights. In these conditions, the low-frequency exchange may dominate over the turbulent transfer. In particular, we show that within the canopy most of the exchange of CO2 and H2O happens on temporal scales longer than 100 s. At 80 m, on the other hand, the turbulent fluxes are almost absent in such very stable conditions, suggesting a boundary layer shallower than 80 m. The relationship between TKE and mean winds shows that the stable boundary layer switches from the very stable to the weakly stable regime during intermittent bursts of turbulence. In general, fluxes estimated with long temporal windows that account for low-frequency effects are more dependent on the stability over a deeper layer above the forest than they are on the stability between the top of the canopy and its interior, suggesting that low-frequency processes are controlled over a deeper layer above the forest. 650 $aAmazonia 650 $aDióxido de Carbono 650 $aVento 653 $aEnergia cinética turbulenta 653 $aTKE 700 1 $aACEVEDO, O. C. 700 1 $aSÖRGEL, M. 700 1 $aTSOKANKUNKU, A. 700 1 $aWOLFF, S. 700 1 $aARAUJO, A. C. de 700 1 $aSOUZA, R. A. F. 700 1 $aSÁ, M. O. 700 1 $aMANZI, A. O. 700 1 $aANDREAE, M. O. 773 $tAtmospheric Chemistry and Physics$gv. 18, n. 5, p. 3083-3099, 2018.
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Embrapa Amazônia Oriental (CPATU) |
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