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Registros recuperados : 5 | |
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. | | MORAES, E. T. I.; DIAS-JÚNIOR, C. Q.; COHEN, J. C. P.; CORRÊA, P. B.; MARTINS, H. S.; D'OLIVEIRA, F. A. F.; KUHN, P. A.; CATTANIO, J. H.; SOUZA, E. B.; ARAUJO, A. C. de; TEIXEIRA, P. R.; MORTARINI, L. Simulation of an orographic gravity wave above the Amazon rainforest and its influence on gases transport near the surface. Atmospheric Research, v. 278, 106349, Nov. 2022. Biblioteca(s): Embrapa Amazônia Oriental. |
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3. | | SERRA-NETO, E. M.; MARTINS, H. S.; DIAS-JUNIOR, C. Q.; SANTANA, R. A.; BRONDANI, D. V.; MANZI, A. O.; ARAUJO, A. C. de; TEIXEIRA, P. R.; SÖRGEL, M.; MORTARINI, L. Simulation of the scalar transport above and within the Amazon Forest Canopy. Atmosphere, v. 12, n. 12, Article 1631, 2021. Biblioteca(s): Embrapa Amazônia Oriental. |
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4. | | 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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5. | | 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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Registros recuperados : 5 | |
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| Acesso ao texto completo restrito à biblioteca da Embrapa Amazônia Oriental. Para informações adicionais entre em contato com cpatu.biblioteca@embrapa.br. |
Registro Completo
Biblioteca(s): |
Embrapa Amazônia Oriental. |
Data corrente: |
04/12/2023 |
Data da última atualização: |
04/12/2023 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Circulação/Nível: |
A - 1 |
Autoria: |
MORAES, E. T. I.; DIAS-JÚNIOR, C. Q.; COHEN, J. C. P.; CORRÊA, P. B.; MARTINS, H. S.; D'OLIVEIRA, F. A. F.; KUHN, P. A.; CATTANIO, J. H.; SOUZA, E. B.; ARAUJO, A. C. de; TEIXEIRA, P. R.; MORTARINI, L. |
Afiliação: |
EIKY T. I. MORAES, UNIVERSIDADE FEDERAL DO PARÁ; CLÉO Q. DIAS-JÚNIOR, UNIVERSIDADE FEDERAL DO PARÁ; JÚLIA C. P. COHEN, UNIVERSIDADE FEDERAL DO PARÁ; POLARI B. CORRÊA, INSTITUTO NACIONAL DE PESQUISAS DA AMAZÔNIA; HARDINEY S. MARTINS, INSTITUTO FEDERAL DO PARÁ; FLÁVIO A. F. D'OLIVEIRA, UNIVERSIDADE FEDERAL DO PARÁ; PAULO A. KUHN, UNIVERSIDADE FEDERAL DO PARÁ; JOSÉ H. CATTANIO, UNIVERSIDADE FEDERAL DO PARÁ; EVERALDO B. SOUZA, UNIVERSIDADE FEDERAL DO PARÁ; ALESSANDRO CARIOCA DE ARAUJO, CPATU; PAULO R. TEIXEIRA, INSTITUTO NACIONAL DE PESQUISAS DA AMAZÔNIA; LUCA MORTARINI, ISTITUTO DI SCIENZE DELL'ATMOSFERA E DEL CLIMA. |
Título: |
Simulation of an orographic gravity wave above the Amazon rainforest and its influence on gases transport near the surface. |
Ano de publicação: |
2022 |
Fonte/Imprenta: |
Atmospheric Research, v. 278, 106349, Nov. 2022. |
DOI: |
https://doi.org/10.1016/j.atmosres.2022.106349 |
Idioma: |
Inglês |
Conteúdo: |
The influence of the topography at the ATTO site (Amazon Tall Tower Observatory) in the formation of Gravity Waves (GW) was investigated in this work. The role of these waves in gas transport on different heights in the nocturnal boundary layer, was also investigated. For this, were analyzed: experimental data of wind speed, temperature, humidity and CO2 to identify the GW. Furthermore satellite images, ECMWF ERA5 (European Center for Medium-Range Weather Forecasts) reanalysis, and numerical simulations from the mesoscale JULES-CCATT-BRAMS model (Brazilian Regional Atmospheric Modeling System) version 5.3 were used to perform GW simulations. The simulations involved two configurations (Control-With Topography and No Topography). The sattelite images made it clear that the GW was not associated with convective activities. The simulations showed clear ondulatory signs in air temperature, vertical component of the wind, and gases like CO and O3. Moreover, they also reveal that the wave originated by the presence of the local topography and this orograph gravity wave had and important role in the transport of gases above the ATTO site. |
Palavras-Chave: |
BRAMS simulation; Gases transport; Orographic gravity wave; Wavelet analyses. |
Thesagro: |
Floresta Tropical. |
Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
Marc: |
LEADER 02161naa a2200325 a 4500 001 2159084 005 2023-12-04 008 2022 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1016/j.atmosres.2022.106349$2DOI 100 1 $aMORAES, E. T. I. 245 $aSimulation of an orographic gravity wave above the Amazon rainforest and its influence on gases transport near the surface.$h[electronic resource] 260 $c2022 520 $aThe influence of the topography at the ATTO site (Amazon Tall Tower Observatory) in the formation of Gravity Waves (GW) was investigated in this work. The role of these waves in gas transport on different heights in the nocturnal boundary layer, was also investigated. For this, were analyzed: experimental data of wind speed, temperature, humidity and CO2 to identify the GW. Furthermore satellite images, ECMWF ERA5 (European Center for Medium-Range Weather Forecasts) reanalysis, and numerical simulations from the mesoscale JULES-CCATT-BRAMS model (Brazilian Regional Atmospheric Modeling System) version 5.3 were used to perform GW simulations. The simulations involved two configurations (Control-With Topography and No Topography). The sattelite images made it clear that the GW was not associated with convective activities. The simulations showed clear ondulatory signs in air temperature, vertical component of the wind, and gases like CO and O3. Moreover, they also reveal that the wave originated by the presence of the local topography and this orograph gravity wave had and important role in the transport of gases above the ATTO site. 650 $aFloresta Tropical 653 $aBRAMS simulation 653 $aGases transport 653 $aOrographic gravity wave 653 $aWavelet analyses 700 1 $aDIAS-JÚNIOR, C. Q. 700 1 $aCOHEN, J. C. P. 700 1 $aCORRÊA, P. B. 700 1 $aMARTINS, H. S. 700 1 $aD'OLIVEIRA, F. A. F. 700 1 $aKUHN, P. A. 700 1 $aCATTANIO, J. H. 700 1 $aSOUZA, E. B. 700 1 $aARAUJO, A. C. de 700 1 $aTEIXEIRA, P. R. 700 1 $aMORTARINI, L. 773 $tAtmospheric Research$gv. 278, 106349, Nov. 2022.
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