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| Registros recuperados : 37 | |
| 21. |  | ROCHA, H. R. da; GOULDEN, M.; MILLER, S.; MANZI, A. O.; CABRAL, O. M. R.; FREITAS, H. C. de; NOBRE, A.; SALESKA, S.; WOFSY, S.; KRUIJT, B.; RANDOW, C. VON. Patterns of CO2 and water fluxes measured by flux towers across tropical forest, ecotone and savanna ecosystems in Brazil. In: INTEGRATED LAND ECOSYSTEM - ATMOSPHERE PROCESSES STUDY, 1., 2006, Colorado, USA. Proceedings... Colorado, USA: Finnish Association for Aerosol Research, 2006. p. 215. (Report Series in Aerosol Science, n. 76). Editors: Anni Reissell, Asbjorn Aarflot.| Biblioteca(s): Embrapa Meio Ambiente. |
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| 22. | | QUERINO, C. A. S.; SMEETS, C. J. P. P.; VIGANO, I.; HOLZINGER, R.; MOURA, V.; GATTI, L. V.; MARTINEWSKI, A.; MANZI, A. O.; ARAUJO, A. C. de; RÖCKMANN, T. Methane flux, vertical gradient and mixing ratio measurements in a tropical forest. Atmospheric Chemistry and Physics Discussions, v. 11, p. 5313-5350, Feb. 2011.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 23. | | 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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| 24. | | 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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| 25. | | 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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| 26. | | 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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| 27. | | MOLION, L. C. B.; MANZI, A. O.; NOBRE, C. A.; SÁ, L. D. de A.; SILVA FILHO, V. de P.; MARQUES FILHO, A. de O.; FISCH, G.; RIBEIRO, M. N. G.; JANUÁRIO, M.; CABRAL, O. M. R.; PATEL, S. R.; MORAES, J. C. de; AGUIAR, L. F. de. Resultados preliminares de um experimento micrometeorológico na Floresta Amazônica. In: SIMPÓSIO DO TRÓPICO ÚMIDO, 1., 1984, Belém, PA. Anais... Belém: EMBRAPA-CPATU, 1986. v. 1. p. 79-86. (EMBRAPA-CPATU. Documentos, 36).| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 28. | | ALVALA, R. C. S.; MANZI, A. O.; SA, L. D. A; MURTY, P. R. V. K.; GIELOW, R.; ARLINO, P. R. A.; ALVALA, P. C.; LIMA, I. D. T.; MARQUES FILHO, E. P. M.; SAMBATTI, S. B. M.; RANDOW, C. von; SOUZA, A. de S; KASSAR, E.; MALHI, Y. S.; KRUIJT, B.; MEIRELLES, M. L. Projeto interdisciplinar do Pantanal - fase umida (IPE - 1). In: CONGRESSO BRASILEIRO DE METEOROLOGIA, 10.; CONGRESSO DA FLISMET, 8., 1998, Brasilia, DF. [Anais]. [S.l.: s.n., 1998?]. n.p.| Biblioteca(s): Embrapa Cerrados. |
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| 29. | | MARENGO, J. A.; CAVALCANTI, I. F. de A.; SATYAMURTY, P.; NOBRE, C. A.; BONATTI, J. P.; TROSNIKOV, I.; MANZI, A. O.; SAMPAIO, G.; CAMARGO JUNIOR, H.; SANCHES, M. B.; CUNNINGHAM, C. A. C.; D'ALMEIDA, C.; PEZZI, L. P.; CALBETE, N. O. Ensemble simulation of interanual climate variability using the CPTEC/COLA atmospheria model. São José dos Campos: INPE, 2001. 77 p. (INPE. 8135-RPQ-717).| Biblioteca(s): Embrapa Agropecuária Oeste. |
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| 30. | | SÁ, M. de O.; LEAL, L. do S. M.; CAMPOS, J. G.; ARAUJO, A. C. de; SILVA, P. R. T. da; SILVA, M. M. da; PAULETTO, D.; OLIVEIRA, M. B. L. de; FERNANDES, M. R. P. S.; DINIZ, M. M.; MANZI, A. O. Estudo do clima e interações entre a floresta e a atmosfera, no Parque Nacional do Pico da Neblina, São Gabriel da Cachoeira, AM. In: OLIVEIRA, L. A. G. de; GUILLERMO CASTELLÓN, E. (Ed.). Desvendando as fronteiras do conhecimento na região amazônica do alto rio Negro. Manaus: INPA, 2012. p. 23-36.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 31. | | BAKER, I. T.; HARPER, A. B.; ROCHA, H. R. da; DENNING, A. S.; ARAUJO, A. C.; BORMA, L. S.; FREITAS, H. C.; GOULDE, M. L.; MANZI, A. O.; MILLER, S. D.; NOBRE, A. D.; RESTREPO-COUPE, N.; SALESKA, S. R.; STÖCKLI, R.; RANDOW, C. von; WOFSY, S. C. Surface ecophysiological behavior across vegetation and moisture gradients in tropical South America. Agricultural and Forest Meteorology, v. 182-183, p. 177-188, Dec. 2013.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 32. | | RESTREPO-COUPE, N.; ROCHA, H. R. da; HUTYRA, L. R.; ARAUJO, A. C. da; BORMA, L. S.; CHRISTOFFERSEN, B.; CABRAL, O. M. R.; CAMARGO, P. B. de; CARDOSO, F. L.; COSTA, A. C. L. da; FITZJARRALD, D. R.; GOULDEN, M. L.; KRUIJT, B.; MAIA, J. M. F.; MALHI, Y. S.; MANZI, A. O.; MILLER, S. D.; NOBRE, A. D.; RANDOW, C. von; SÁ, L. D. ABREU; SAKAI, R. K.; TOTA, J.; WOFSY, S. C.; ZANCHI, F. B.; SALESKA, S. R. What drives the seasonality of photosynthesis across the Amazon basin: a cross-site analysis of eddy flux tower measurements from the Brasil flux network. Agricultural and Forest Meteorology, v. 182-183, p. 128-144, Dec. 2013.| Biblioteca(s): Embrapa Amazônia Oriental; Embrapa Meio Ambiente. |
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| 33. | | RANDOW, C. von; ZERI, M.; RESTREPO-COUPE, N.; MUZA, M. N.; GONÇALVES, L. G. G. de; COSTA, M. H.; ARAUJO, A. C.; MANZI, A. O.; ROCHA, H. R. da; SALESKA, S. R.; ARAIN, M. A.; BAKER, I. T.; CESTARO, B. P.; CHRISTOFFERSEN, B.; CIAIS, P.; FISHER, J. B.; GALBRAITH, D.; GUAN, X.; HURK, B. van den; ICHII, K.; IMBUZEIRO, H.; JAIN, A.; LEVINE, N.; MIGUEZ-MACHO, G.; POULTER, B.; ROBERTI, D. R.; SAHOO, A.; SCHAEFER, K.; SHI, M.; TIAN, H.; VERBEECK, H.; YANG, Z.-L. Inter-annual variability of carbon and water fluxes in Amazonian forest, Cerrado and pasture sites, as simulated by terrestrial biosphere models. Agricultural and Forest Meteorology, v. 182-183, p. 144-155, Dec. 2013.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 34. | | CHRISTOFFERSEN, B. O.; RESTREPO-COUPE, N.; ARAIN, M. A.; BAKER, I. T.; CESTARO, B. P.; CIAIS, P.; FISHER, J. B.; GALBRAITH, D.; GUAN, X.; GULDEN, L.; HURK, B. van den; ICHII, K.; IMBUZEIRO, H.; JAIN, A.; LEVINE, N.; MIGUEZ-MACHO, G.; POULTER, B.; ROBERTI, D. R.; SAKAGUCHI, K.; SAHOO, A.; SCHAEFER, K.; SHI, M.; VERBEECK, H.; YANG, Z.-L.; ARAUJO, A. C.; KRUIJT, B.; MANZI, A. O.; ROCHA, H. R. da; RANDOW, C. von; MUZA, M. N.; BORAK, J.; COSTA, M. H.; GONÇALVES, L. G. G. de; ZENG, X.; SALESKA, S. R. Mechanisms of water supply and vegetation demand govern the seasonality and magnitude of evapotranspiration in Amazonia and Cerrado. Agricultural and Forest Meteorology, v. 191, p. 33-50, June 2014.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 35. | | ANDREAE, M. O.; ACEVEDO, O. C.; ARAUJO, A.; ARTAXO, P.; BARBOSA, C. G. G.; BARBOSA, H. M. J.; BRITO, J.; CARBONE, S.; CHI, X.; CINTRA, B. B. L.; SILVA, N. F. da; DIAS, N. L.; DIAS-JÚNIOR, C. Q.; DITAS, F.; DITZ, R.; GODOI, A. F. L.; GODOI, R. H. M.; HEIMANN, M.; HOFFMANN, T.; KESSELMEIER, J.; KÖNEMANN, T.; KRÜGER, M. L.; LAVRIC, J. V.; MANZI, A. O.; MORAN-ZULOAGA, D.; NÖLSCHER, A. C.; NOGUEIRA, D. S.; PIEDADE, M. T. F.; PÖHLKER, C.; PÖSCHL, U.; RIZZO, L. V.; RO, C.-U.; RUCKTESCHLER, N.; SÁ, L. D. A.; SÁ, M. D. O.; SALES, C. B.; SANTOS, R. M. N. dos; SATURNO, J.; SCHÖNGART, J.; SÖRGEL, M.; SOUZA, C. M. de; SOUZA, R. A. F. de; SU, H.; TARGHETTA, N.; TÓTA, J.; TREBS, I.; TRUMBORE, S.; EIJCK, A. van; WALTER, D.; WANG, Z.; WEBER, B.; WILLIAMS, J.; WINDERLICH, J.; WITTMANN, F.; WOLFF, S.; YÁÑEZ-SERRANO, A. M. The Amazon Tall Tower Observatory (ATTO) in the remote Amazon basin: overview of first results from ecosystem ecology, meteorology, trace gas, and aerosol measurements. Atmospheric Chemistry and Physics Discuss, v. 15, n. 18, p. 11599-11726, 2015.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 36. | | WENDISCH, M.; PÖSCHL, U.; ANDREAE, M. O.; MACHADO, L. A. T.; ALBRECHT, R.; SCHLAGER, H.; ROSENFELD, D.; MARTIN, S. T.; ABDELMONEM, A.; AFCHINE, A.; ARAUJO, A. C.; ARTAXO, P.; AUFMHOFF, H.; BARBOSA, H. M. J.; BORRMANN, S.; BRAGA, R.; BUCHHOLZ, B.; CECCHINI, M. A.; COSTA, A.; CURTIUS, J.; DOLLNER, M.; DORF, M.; DREILING, V.; EBERT, V.; EHRLICH, A.; EWALD, F.; FISCH, G.; FIX, A.; FRANK, F.; FÜTTERER, D.; HECKL, C.; HEIDELBERG, F.; HÜNEKE, T.; JÄKEL, E.; JÄRVINEN, E.; JURKAT, T.; KANTER, S.; KÄSTNER, U.; KENNTNER, M.; KESSEKMEIER, J.; KLIMACH, T.; KNECHT, M.; KOHL, R.; KÖLLING, T.; KRÄMER, M.; KRÜGER, M.; KRISNA, T. C.; LAVRIC, J. V.; LONGO, K.; MAHNKE, C.; MANZI, A. O.; MAYER, B.; MERTES, S.; MINIKIN, A.; MOLLEKER, S.; MÜNCH, S.; NILIUS, B.; PFEILSTICKER, K.; PÖHLKER, C.; ROIGER, A.; ROSE, D.; ROSENOW, D.; SAUER, D.; SCHNAITER, M.; SCHNEIDER, J.; SCHULZ, C.; SOUZA, R. A. F. de; SPANU, A.; STOCK, P.; VILA, D.; VOIGT, C.; WALSER, A.; WALTER, D.; WEIGEL, R.; WEINZIERL, B.; WERNER, F.; YAMASOE, M. A.; ZIEREIS, H.; ZINNER, T.; ZÖGER, M. Acridicon-Chuva campaign: studying tropical deep convective clouds and precipitation over Amazonia using the New German research aircraft HALO. Bulletin of the American Meteorological Society, v. 97, n. 10, p. 1885-1908, Oct. 2016.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 37. | | ANDREAE, M. O.; ACEVEDO, O. C.; ARAUJO, A.; ARTAXO, P.; BARBOSA, C. G. G.; BARBOSA, H. M. J.; BRITO, J.; CARBONE, S.; CHI, X.; CINTRA, B. B. L.; SILVA, N. F. da; DIAS, N. L.; DIAS-JÚNIOR, C. Q.; DITAS, F.; DITZ, R.; GODOI, A. F. L.; GODOI, R. H. M.; HEIMANN, M.; HOFFMANN, T.; KESSELMEIER, J.; KÖNEMANN, T.; KRÜGER, M. L.; LAVRIC, J. V.; MANZI, A. O.; LOPES, A. P.; MARTINS, D. L.; MIKHAILOV, E. F.; MORAN-ZULOAGA, D.; NELSON, B. W.; NÖLSCHER, A. C.; NOGUEIRA, D. S.; PIEDADE, M. T. F.; PÖHLKER, C.; PÖSCHL, U.; QUESADA, C. A.; RIZZO, L. V.; RO, C.-U.; RUCKTESCHLER, N.; SÁ, L. D. A.; SÁ, M. de O.; SALES, C. B.; SANTOS, R. M. N. dos; SATURNO, J.; SCHÖNGART, J.; SÖRGEL, M.; SOUZA, C. M. de; SOUZA, R. A. F. de; SU, H.; TARGHETTA, N.; TÓTA, J.; TREBS, I.; TRUMBORE, S.; EIJCK, A. van; WALTER, D.; WANG, Z.; WEBER, B.; WILLIAMS, J.; WINDERLICH, J.; WITTMANN, F.; WOLFF, S.; YÁÑEZ-SERRANO, A. M. The Amazon Tall Tower Observatory (ATTO): overview of pilot measurements on ecosystem ecology, meteorology, trace gases, and aerosols. Atmospheric Chemistry and Physics, v. 15, n. 18, p. 10723-10776, 2015.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| Registros recuperados : 37 | |
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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
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
30/09/2014 |
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Data da última atualização: |
19/10/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
CHRISTOFFERSEN, B. O.; RESTREPO-COUPE, N.; ARAIN, M. A.; BAKER, I. T.; CESTARO, B. P.; CIAIS, P.; FISHER, J. B.; GALBRAITH, D.; GUAN, X.; GULDEN, L.; HURK, B. van den; ICHII, K.; IMBUZEIRO, H.; JAIN, A.; LEVINE, N.; MIGUEZ-MACHO, G.; POULTER, B.; ROBERTI, D. R.; SAKAGUCHI, K.; SAHOO, A.; SCHAEFER, K.; SHI, M.; VERBEECK, H.; YANG, Z.-L.; ARAUJO, A. C.; KRUIJT, B.; MANZI, A. O.; ROCHA, H. R. da; RANDOW, C. von; MUZA, M. N.; BORAK, J.; COSTA, M. H.; GONÇALVES, L. G. G. de; ZENG, X.; SALESKA, S. R. |
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Afiliação: |
Bradley O. Christoffersen, University of Arizona; Natalia Restrepo-Coupe, University of Arizona / University of Technology, Sydney, Australia; M Altaf Arain, McMaster University; Ian T. Baker, Colorado State University; Bruno P. Cestaro, USP; Phillippe Ciais, LSCE CEA-CNRS-UVSQ, Orme des Merisiers; Joshua B. Fisher, California Institute of Technology; David Galbraith, University of Oxford / University of Leeds; Xiaodan Guan, The University of Texas at Austin; Lindsey Gulden, The University of Texas at Austin / ExxonMobil Upstream Research Company; Bart van den Hurk, Royal Netherlands Meteorological Institute (KNMI); Kazuhito Ichii, Fukushima University; Hewlley Imbuzeiro, UFV; Atul Jain, University of Illinois at Urbana-Champaign; Naomi Levine, Harvard University; Gonzalo Miguez-Macho, Universidade de Santiago de Compostela; Ben Poulter, Swiss Federal Research Institute WSL; Debora R. Roberti, UFSM; Koichi Sakaguchi, University of Arizona; Alok Sahoo, Center for Research on Environment and Water, IGES; Kevin Schaefer, University of Colorado at Boulder; Mingjie Shi, The University of Texas at Austin; Hans Verbeeck, Ghent University; Zong-Liang Yang, The University of Texas at Austin; ALESSANDRO CARIOCA DE ARAUJO, CPATU; Bart Kruijt, Wageningen University & Research Center; Antonio O. Manzi, INPA; Humberto R. da Rocha, USP; Celso von Randow, INPE; Michel N. Muza, University of Maryland, College Park, Hydrological Sciences Laboratory, NASA Goddard Space Flight Center; Jordan Borak, INPE; Marcos H. Costa, UFV; Luis Gustavo Gonçalves de Gonçalves, University of Maryland, College Park, Hydrological Sciences Laboratory, NASA Goddard Space Flight Center / INPE; Xubin Zeng, University of Arizona; Scott R. Saleska, University of Arizona. |
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Título: |
Mechanisms of water supply and vegetation demand govern the seasonality and magnitude of evapotranspiration in Amazonia and Cerrado. |
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Ano de publicação: |
2014 |
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Fonte/Imprenta: |
Agricultural and Forest Meteorology, v. 191, p. 33-50, June 2014. |
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DOI: |
10.1016/j.agrformet.2014.02.008 |
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Idioma: |
Inglês |
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Conteúdo: |
Evapotranspiration (E) in the Amazon connects forest function and regional climate via its role in precipitation recycling However, the mechanisms regulating water supply to vegetation and its demand for water remain poorly understood, especially during periods of seasonal water deficits In this study, we address two main questions: First, how do mechanisms of water supply (indicated by rooting depth and groundwater) and vegetation water demand (indicated by stomatal conductance and intrinsic water use efficiency) control evapotranspiration (E) along broad gradients of climate and vegetation from equatorial Amazonia to Cerrado, and second, how do these inferred mechanisms of supply and demand compare to those employed by a suite of ecosystem models? We used a network of eddy covariance towers in Brazil coupled with ancillary measurements to address these questions With respect to the magnitude and seasonality of E, models have much improved in equatorial tropical forests by eliminating most dry season water limitation, diverge in performance in transitional forests where seasonal water deficits are greater, and mostly capture the observed seasonal depressions in E at Cerrado However, many models depended universally on either deep roots or groundwater to mitigate dry season water deficits, the relative importance of which we found does not vary as a simple function of climate or vegetation In addition, canopy stomatal conductance (gs) regulates dry season vegetation demand for water at all except the wettest sites even as the seasonal cycle of E follows that of net radiation In contrast, some models simulated no seasonality in gs, even while matching the observed seasonal cycle of E. We suggest that canopy dynamics mediated by leaf phenology may play a significant role in such seasonality, a process poorly represented in models Model bias in gs and E, in turn, was related to biases arising from the simulated light response (gross primary productivity, GPP) or the intrinsic water use efficiency of photosynthesis (iWUE). We identified deficiencies in models which would not otherwise be apparent based on a simple comparison of simulated and observed rates of E. While some deficiencies can be remedied by parameter tuning, in most models they highlight the need for continued process development of belowground hydrology and in particular, the biological processes of root dynamics and leaf phenology, which via their controls on E, mediate vegetation-climate feedbacks in the tropics. MenosEvapotranspiration (E) in the Amazon connects forest function and regional climate via its role in precipitation recycling However, the mechanisms regulating water supply to vegetation and its demand for water remain poorly understood, especially during periods of seasonal water deficits In this study, we address two main questions: First, how do mechanisms of water supply (indicated by rooting depth and groundwater) and vegetation water demand (indicated by stomatal conductance and intrinsic water use efficiency) control evapotranspiration (E) along broad gradients of climate and vegetation from equatorial Amazonia to Cerrado, and second, how do these inferred mechanisms of supply and demand compare to those employed by a suite of ecosystem models? We used a network of eddy covariance towers in Brazil coupled with ancillary measurements to address these questions With respect to the magnitude and seasonality of E, models have much improved in equatorial tropical forests by eliminating most dry season water limitation, diverge in performance in transitional forests where seasonal water deficits are greater, and mostly capture the observed seasonal depressions in E at Cerrado However, many models depended universally on either deep roots or groundwater to mitigate dry season water deficits, the relative importance of which we found does not vary as a simple function of climate or vegetation In addition, canopy stomatal conductance (gs) regulates dry season vegetation demand f... Mostrar Tudo |
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Thesagro: |
Água; Cerrado; Evapotranspiração; Floresta Tropical. |
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Thesaurus NAL: |
Amazonia. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
|
Marc: |
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100 1 $aCHRISTOFFERSEN, B. O.
245 $aMechanisms of water supply and vegetation demand govern the seasonality and magnitude of evapotranspiration in Amazonia and Cerrado.$h[electronic resource]
260 $c2014
520 $aEvapotranspiration (E) in the Amazon connects forest function and regional climate via its role in precipitation recycling However, the mechanisms regulating water supply to vegetation and its demand for water remain poorly understood, especially during periods of seasonal water deficits In this study, we address two main questions: First, how do mechanisms of water supply (indicated by rooting depth and groundwater) and vegetation water demand (indicated by stomatal conductance and intrinsic water use efficiency) control evapotranspiration (E) along broad gradients of climate and vegetation from equatorial Amazonia to Cerrado, and second, how do these inferred mechanisms of supply and demand compare to those employed by a suite of ecosystem models? We used a network of eddy covariance towers in Brazil coupled with ancillary measurements to address these questions With respect to the magnitude and seasonality of E, models have much improved in equatorial tropical forests by eliminating most dry season water limitation, diverge in performance in transitional forests where seasonal water deficits are greater, and mostly capture the observed seasonal depressions in E at Cerrado However, many models depended universally on either deep roots or groundwater to mitigate dry season water deficits, the relative importance of which we found does not vary as a simple function of climate or vegetation In addition, canopy stomatal conductance (gs) regulates dry season vegetation demand for water at all except the wettest sites even as the seasonal cycle of E follows that of net radiation In contrast, some models simulated no seasonality in gs, even while matching the observed seasonal cycle of E. We suggest that canopy dynamics mediated by leaf phenology may play a significant role in such seasonality, a process poorly represented in models Model bias in gs and E, in turn, was related to biases arising from the simulated light response (gross primary productivity, GPP) or the intrinsic water use efficiency of photosynthesis (iWUE). We identified deficiencies in models which would not otherwise be apparent based on a simple comparison of simulated and observed rates of E. While some deficiencies can be remedied by parameter tuning, in most models they highlight the need for continued process development of belowground hydrology and in particular, the biological processes of root dynamics and leaf phenology, which via their controls on E, mediate vegetation-climate feedbacks in the tropics.
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700 1 $aSALESKA, S. R.
773 $tAgricultural and Forest Meteorology$gv. 191, p. 33-50, June 2014.
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