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Registro Completo |
Biblioteca(s): |
Embrapa Uva e Vinho. |
Data corrente: |
22/05/2014 |
Data da última atualização: |
02/04/2019 |
Tipo da produção científica: |
Artigo em Periódico Indexado |
Autoria: |
TONIETTO, J.; SOTES RUIZ, V.; ZANUS, M. C.; MONTES, C.; ULIARTE, E. M.; BRUNO, L. A.; CLIMACO, P.; PENA, A.; GUERRA, C. C.; CATANIA, C. D.; KOHLBERG, E. K.; PEREIRA, G. E.; RICARDO-DA-SILVA, J.-M.; RAGOUT, J. V.; NAVARRO, L. V.; LAUREANO, O.; DE CASTRO, R.; DEL MONTE, R. F.; DEL MONTE, S. A.; GOMEZ-MIGUEL, V.; CARBONNEAU, A. |
Afiliação: |
JORGE TONIETTO, CNPUV; UPM - Universidad Politécnica, Madrid, Spain; MAURO CELSO ZANUS, CNPUV; CEAZA - Centro de Estudios Avanzados en Zonas Áridas, La Serena, Chile; INTA EEA, Mendoza, Argentina; PFCUVS-FAUTAPO, Tarija, Bolivia; INIA/INRB, Estação Vitivinícola Nacional, Dois Portos, Portugal; Faculdad de Ciencias Agronomicas, Universidad de Chile, Santiago, Chile; CELITO CRIVELLARO GUERRA, CNPUV; INTA – EEA, Mendoza, Argentina; Kohlberg Estate, Tarija, Bolivia; GIULIANO ELIAS PEREIRA, CNPUV; ISA-UTL - Instituto Superior de Agronomia, Lisboa, Portugal; ISA-UTL - Instituto Superior de Agronomia, Lisboa, Portugal; ISA-UTL - Instituto Superior de Agronomia, Lisboa, Portugal; INTA EEA, Mendoza, Argentina; INTA EEA, Mendoza, Argentina; UPM - Universidad Politécnica, Madrid, Spain; Supagro, Montpellier, France. |
Título: |
The Effect of Viticultural Climate on Red and White Wine Typicity - Characterization in Ibero-American grape-growing regions |
Ano de publicação: |
2014 |
Fonte/Imprenta: |
Spécial Laccave, J. Int. Sci. Vigne Vin, p. 19 - 23, 2014. |
Idioma: |
Inglês |
Conteúdo: |
Aim: This study is part of a CYTED (Ibero-American Program for Science, Technology and Development) project on vitivinicultural zoning. The objective was to characterize the effect of viticultural climate on red and white wine typicity in the macro Ibero-American viticultural region. Methods and results: The climate of 46 grape-growing regions in 6 Ibero-American countries (Argentina, Bolivia, Brazil, Chile, Spain and Portugal) was characterized using the three viticultural climate index of the Geoviticulture MCC System: the Heliothermal index HI, the Cool Night index CI and the Dryness index DI. The main sensory characteristics frequently observed in representative red and white wines of each of these regions were described by enology experts in the respective countries: intensity of colour, aroma, aroma-ripe fruit, body-palate concentration, alcohol, tannins (for red wines) and acidity as well as persistence on the palate. The data were submitted to a correlation analysis of the variables and Principal Component Analysis (PCA). Conclusion: The typicity of red and white wines was correlated with the HI, CI and DI viticultural climate indexes from the MCC System. The main wine sensory variables affected by viticultural climate were identified. Significance and impact of the study : The results can be used to project the potential impacts of climate change on wine sensory characteristics. |
Palavras-Chave: |
Ibero-America; Ibero-American countries. |
Thesagro: |
Clima; Regiao fisiografica; Uva; Viticultura. |
Thesaurus Nal: |
Climate change; Principal component analysis; Sensory properties; Viticulture. |
Categoria do assunto: |
-- |
URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/102462/1/Tonietto-Pereira-et-al-JISVV-2014.pdf
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Marc: |
LEADER 02769naa a2200481 a 4500 001 1986819 005 2019-04-02 008 2014 bl uuuu u00u1 u #d 100 1 $aTONIETTO, J. 245 $aThe Effect of Viticultural Climate on Red and White Wine Typicity - Characterization in Ibero-American grape-growing regions$h[electronic resource] 260 $c2014 520 $aAim: This study is part of a CYTED (Ibero-American Program for Science, Technology and Development) project on vitivinicultural zoning. The objective was to characterize the effect of viticultural climate on red and white wine typicity in the macro Ibero-American viticultural region. Methods and results: The climate of 46 grape-growing regions in 6 Ibero-American countries (Argentina, Bolivia, Brazil, Chile, Spain and Portugal) was characterized using the three viticultural climate index of the Geoviticulture MCC System: the Heliothermal index HI, the Cool Night index CI and the Dryness index DI. The main sensory characteristics frequently observed in representative red and white wines of each of these regions were described by enology experts in the respective countries: intensity of colour, aroma, aroma-ripe fruit, body-palate concentration, alcohol, tannins (for red wines) and acidity as well as persistence on the palate. The data were submitted to a correlation analysis of the variables and Principal Component Analysis (PCA). Conclusion: The typicity of red and white wines was correlated with the HI, CI and DI viticultural climate indexes from the MCC System. The main wine sensory variables affected by viticultural climate were identified. Significance and impact of the study : The results can be used to project the potential impacts of climate change on wine sensory characteristics. 650 $aClimate change 650 $aPrincipal component analysis 650 $aSensory properties 650 $aViticulture 650 $aClima 650 $aRegiao fisiografica 650 $aUva 650 $aViticultura 653 $aIbero-America 653 $aIbero-American countries 700 1 $aSOTES RUIZ, V. 700 1 $aZANUS, M. C. 700 1 $aMONTES, C. 700 1 $aULIARTE, E. M. 700 1 $aBRUNO, L. A. 700 1 $aCLIMACO, P. 700 1 $aPENA, A. 700 1 $aGUERRA, C. C. 700 1 $aCATANIA, C. D. 700 1 $aKOHLBERG, E. K. 700 1 $aPEREIRA, G. E. 700 1 $aRICARDO-DA-SILVA, J.-M. 700 1 $aRAGOUT, J. V. 700 1 $aNAVARRO, L. V. 700 1 $aLAUREANO, O. 700 1 $aDE CASTRO, R. 700 1 $aDEL MONTE, R. F. 700 1 $aDEL MONTE, S. A. 700 1 $aGOMEZ-MIGUEL, V. 700 1 $aCARBONNEAU, A. 773 $tSpécial Laccave, J. Int. Sci. Vigne Vin, p. 19 - 23, 2014.
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Embrapa Uva e Vinho (CNPUV) |
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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: |
RESTREPO-COUPE, N.; ALBERT, L. P.; LONGO, M.; BAKER, I.; LEVINE, N. M.; MERCADO, L. M.; ARAUJO, A. C. de; CHRISTOFFERSEN, B. O.; COSTA, M. H.; FITZJARRALD, D. R.; GALBRAITH, D.; IMBUZEIRO, H.; MALHI, Y.; RANDOW, C. von; ZENG, X.; MOORCROFT, P.; SALESKA, S. R. |
Afiliação: |
NATALIA RESTREPO-COUPE, University of Arizona / University of Technology Sydney; LOREN P. ALBERT, University of Arizona / West Virginia University; MARCOS LONGO, Harvard University/California Institute of Technology; IAN BAKER, Colorado State University; NAOMI M. LEVINE, Harvard University / University of Southern California; LINA M. MERCADO, University of Exeter / Centre for Ecology and Hydrology; ALESSANDRO CARIOCA DE ARAUJO, CPATU; BRADLEY O'DONNELL CHRISTOFFERSEN, University of Texas Rio Grande Valley / Earth and Environmental Sciences Division, Los Alamos National Laboratory; MARCOS H. COSTA, UFV; DAVID R. FITZJARRALD, University at Albany SUNY; DAVID GALBRAITH, University of Leeds; HEWLLEY IMBUZEIRO, UFV; YADVINDER MALHI, University of Oxford; CELSO VON RANDOW, INPE; XUBIN ZENG, University of Arizona; PAUL MOORCROFT, California Institute of Technology; SCOTT R. SALESKA, University of Arizona. |
Título: |
Understanding water and energy fluxes in the Amazonia: Lessons from an observation-model intercomparison. |
Ano de publicação: |
2021 |
Fonte/Imprenta: |
Global Change Biology, v. 27, n. 9, p. 1802-1819, 2021. |
DOI: |
https://doi.org/10.1111/gcb.15555 |
Idioma: |
Inglês |
Conteúdo: |
Tropical forests are an important part of global water and energy cycles, but the mechanisms that drive seasonality of their land-atmosphere exchanges have proven challenging to capture in models. Here, we (1) report the seasonality of fluxes of latent heat (LE), sensible heat (H), and outgoing short and longwave radiation at four diverse tropical forest sites across Amazonia-along the equator from the Caxiuanã and Tapajós National Forests in the eastern Amazon to a forest near Manaus, and from the equatorial zone to the southern forest in Reserva Jaru; (2) investigate how vegetation and climate influence these fluxes; and (3) evaluate land surface model performance by comparing simulations to observations. We found that previously identified failure of models to capture observed dry-season increases in evapotranspiration (ET) was associated with model overestimations of (1) magnitude and seasonality of Bowen ratios (relative to aseasonal observations in which sensible was only 20%-30% of the latent heat flux) indicating model exaggerated water limitation, (2) canopy emissivity and reflectance (albedo was only 10%-15% of incoming solar radiation, compared to 0.15%-0.22% simulated), and (3) vegetation temperatures (due to underestimation of dry-season ET and associated cooling). These partially compensating model-observation discrepancies (e.g., higher temperatures expected from excess Bowen ratios were partially ameliorated by brighter leaves and more interception/evaporation) significantly biased seasonal model estimates of net radiation (Rn), the key driver of water and energy fluxes (LE ~ 0.6 Rn and H ~ 0.15 Rn), though these biases varied among sites and models. A better representation of energy-related parameters associated with dynamic phenology (e.g., leaf optical properties, canopy interception, and skin temperature) could improve simulations and benchmarking of current vegetation-atmosphere exchange and reduce uncertainty of regional and global biogeochemical models. MenosTropical forests are an important part of global water and energy cycles, but the mechanisms that drive seasonality of their land-atmosphere exchanges have proven challenging to capture in models. Here, we (1) report the seasonality of fluxes of latent heat (LE), sensible heat (H), and outgoing short and longwave radiation at four diverse tropical forest sites across Amazonia-along the equator from the Caxiuanã and Tapajós National Forests in the eastern Amazon to a forest near Manaus, and from the equatorial zone to the southern forest in Reserva Jaru; (2) investigate how vegetation and climate influence these fluxes; and (3) evaluate land surface model performance by comparing simulations to observations. We found that previously identified failure of models to capture observed dry-season increases in evapotranspiration (ET) was associated with model overestimations of (1) magnitude and seasonality of Bowen ratios (relative to aseasonal observations in which sensible was only 20%-30% of the latent heat flux) indicating model exaggerated water limitation, (2) canopy emissivity and reflectance (albedo was only 10%-15% of incoming solar radiation, compared to 0.15%-0.22% simulated), and (3) vegetation temperatures (due to underestimation of dry-season ET and associated cooling). These partially compensating model-observation discrepancies (e.g., higher temperatures expected from excess Bowen ratios were partially ameliorated by brighter leaves and more interception/evaporatio... Mostrar Tudo |
Thesagro: |
Balanço de Energia; Ecossistema; Floresta Tropical. |
Thesaurus NAL: |
Amazonia; Ecosystems; Eddy covariance; Energy balance; Evapotranspiration; Tropical forests. |
Categoria do assunto: |
K Ciência Florestal e Produtos de Origem Vegetal |
Marc: |
LEADER 03241naa a2200433 a 4500 001 2159142 005 2023-12-04 008 2021 bl uuuu u00u1 u #d 024 7 $ahttps://doi.org/10.1111/gcb.15555$2DOI 100 1 $aRESTREPO-COUPE, N. 245 $aUnderstanding water and energy fluxes in the Amazonia$bLessons from an observation-model intercomparison.$h[electronic resource] 260 $c2021 520 $aTropical forests are an important part of global water and energy cycles, but the mechanisms that drive seasonality of their land-atmosphere exchanges have proven challenging to capture in models. Here, we (1) report the seasonality of fluxes of latent heat (LE), sensible heat (H), and outgoing short and longwave radiation at four diverse tropical forest sites across Amazonia-along the equator from the Caxiuanã and Tapajós National Forests in the eastern Amazon to a forest near Manaus, and from the equatorial zone to the southern forest in Reserva Jaru; (2) investigate how vegetation and climate influence these fluxes; and (3) evaluate land surface model performance by comparing simulations to observations. We found that previously identified failure of models to capture observed dry-season increases in evapotranspiration (ET) was associated with model overestimations of (1) magnitude and seasonality of Bowen ratios (relative to aseasonal observations in which sensible was only 20%-30% of the latent heat flux) indicating model exaggerated water limitation, (2) canopy emissivity and reflectance (albedo was only 10%-15% of incoming solar radiation, compared to 0.15%-0.22% simulated), and (3) vegetation temperatures (due to underestimation of dry-season ET and associated cooling). These partially compensating model-observation discrepancies (e.g., higher temperatures expected from excess Bowen ratios were partially ameliorated by brighter leaves and more interception/evaporation) significantly biased seasonal model estimates of net radiation (Rn), the key driver of water and energy fluxes (LE ~ 0.6 Rn and H ~ 0.15 Rn), though these biases varied among sites and models. A better representation of energy-related parameters associated with dynamic phenology (e.g., leaf optical properties, canopy interception, and skin temperature) could improve simulations and benchmarking of current vegetation-atmosphere exchange and reduce uncertainty of regional and global biogeochemical models. 650 $aAmazonia 650 $aEcosystems 650 $aEddy covariance 650 $aEnergy balance 650 $aEvapotranspiration 650 $aTropical forests 650 $aBalanço de Energia 650 $aEcossistema 650 $aFloresta Tropical 700 1 $aALBERT, L. P. 700 1 $aLONGO, M. 700 1 $aBAKER, I. 700 1 $aLEVINE, N. M. 700 1 $aMERCADO, L. M. 700 1 $aARAUJO, A. C. de 700 1 $aCHRISTOFFERSEN, B. O. 700 1 $aCOSTA, M. H. 700 1 $aFITZJARRALD, D. R. 700 1 $aGALBRAITH, D. 700 1 $aIMBUZEIRO, H. 700 1 $aMALHI, Y. 700 1 $aRANDOW, C. von 700 1 $aZENG, X. 700 1 $aMOORCROFT, P. 700 1 $aSALESKA, S. R. 773 $tGlobal Change Biology$gv. 27, n. 9, p. 1802-1819, 2021.
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