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Registro Completo |
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
20/10/2016 |
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Data da última atualização: |
20/05/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
MALLICK, K.; TREBS, I.; BOEGH, E.; GIUSTARINI, L.; SCHLERF, M.; DREWRY, D. T.; HOFFMANN, L.; RANDOW, C. von; KRUIJT, B.; ARAUJO, A.; SALESKA, S.; EHLERINGER, J. R.; DOMINGUES, T. F.; OMETTO, J. P. H. B.; NOBRE, A. D.; MORAES, O. L. L. de; HAYEK, M.; MUNGER, J. W.; WOFSY, S. C. |
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Afiliação: |
KANISKA MALLICK, Luxembourg Institute of Science and Technology; IVONNE TREBS, Luxembourg Institute of Science and Technology; EVA BOEGH, Roskilde University; LAURA GIUSTARINI, Luxembourg Institute of Science and Technology; MARTIN SCHLERF, Luxembourg Institute of Science and Technology; DARREN DREWRY, California Institute of Technology; LUCIEN HOFFMANN, Luxembourg Institute of Science and Technology; CELSO VON RANDOW, INPE; BART KRUIJT, Wageningen University and Research Centre; ALESSANDRO CARIOCA DE ARAUJO, CPATU; SCOTT SALESKA, University of Arizona; JAMES R. EHLERINGER, University of Utah; TOMAS F. DOMINGUES, USP; JEAN PIERRE H. B. OMETTO, INPE; ANTONIO D. NOBRE, INPE; OSVALDO LUIZ LEAL DE MORAES, Centro Nacional de Monitoramento e Alertas de Desastres Naturais; MATTHEW HAYEK, Harvard University; WILLIAM MUNGER, Harvard University; STEVE WOFSY, Harvard University. |
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Título: |
Canopy-scale biophysical controls of transpiration and evaporation in the Amazon Basin. |
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Ano de publicação: |
2016 |
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Fonte/Imprenta: |
Hydrology and Earth System Science Discussions, 27 Jan. 2016. |
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DOI: |
10.5194/hess-2015-552 |
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Idioma: |
Inglês
Português |
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Conteúdo: |
Canopy and aerodynamic conductances (gC and gA) are two of the key land surface biophysical variables that control the land surface response of land surface schemes in climate models. Their representation is crucial for predicting transpiration (λET) and evaporation (λEE) flux components of the terrestrial latent heat flux (λE), which has important implications for global climate change and water resource management. By physical integration of radiometric surface temperature (TR) into an integrated framework of the Penman?Monteith and Shuttleworth?Wallace models, we present a novel approach to directly quantify the canopy-scale biophysical controls on λET and λEE over multiple plant functional types (PFTs) in the Amazon Basin. Combining data from six LBA (Large-scale Biosphere-Atmosphere Experiment in Amazonia) eddy covariance tower sites and a TR-driven physically based modeling approach, we identified the canopy-scale feedback-response mechanism between gC, λET, and atmospheric vapor pressure deficit (DA), without using any leaf-scale empirical parameterizations for the modeling. The TR-based model shows minor biophysical control on λET during the wet (rainy) seasons where λET becomes predominantly radiation driven and net radiation (RN) determines 75 to 80 % of the variances of λET. However, biophysical control on λET is dramatically increased during the dry seasons, and particularly the 2005 drought year, explaining 50 to 65 % of the variances of λET, and indicates λET to be substantially soil moisture driven during the rainfall deficit phase. Despite substantial differences in gA between forests and pastures, very similar canopy?atmosphere "coupling" was found in these two biomes due to soil moisture-induced decrease in gC in the pasture. This revealed the pragmatic aspect of the TR-driven model behavior that exhibits a high sensitivity of gC to per unit change in wetness as opposed to gA that is marginally sensitive to surface wetness variability. Our results reveal the occurrence of a significant hysteresis between λET and gC during the dry season for the pasture sites, which is attributed to relatively low soil water availability as compared to the rainforests, likely due to differences in rooting depth between the two systems. Evaporation was significantly influenced by gA for all the PFTs and across all wetness conditions. Our analytical framework logically captures the responses of gC and gA to changes in atmospheric radiation, DA, and surface radiometric temperature, and thus appears to be promising for the improvement of existing land?surface?atmosphere exchange parameterizations across a range of spatial scales. MenosCanopy and aerodynamic conductances (gC and gA) are two of the key land surface biophysical variables that control the land surface response of land surface schemes in climate models. Their representation is crucial for predicting transpiration (λET) and evaporation (λEE) flux components of the terrestrial latent heat flux (λE), which has important implications for global climate change and water resource management. By physical integration of radiometric surface temperature (TR) into an integrated framework of the Penman?Monteith and Shuttleworth?Wallace models, we present a novel approach to directly quantify the canopy-scale biophysical controls on λET and λEE over multiple plant functional types (PFTs) in the Amazon Basin. Combining data from six LBA (Large-scale Biosphere-Atmosphere Experiment in Amazonia) eddy covariance tower sites and a TR-driven physically based modeling approach, we identified the canopy-scale feedback-response mechanism between gC, λET, and atmospheric vapor pressure deficit (DA), without using any leaf-scale empirical parameterizations for the modeling. The TR-based model shows minor biophysical control on λET during the wet (rainy) seasons where λET becomes predominantly radiation driven and net radiation (RN) determines 75 to 80 % of the variances of λET. However, biophysical control on λET is dramatically increased during the dry seasons, and particularly the 2005 drought year, explaining... Mostrar Tudo |
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Palavras-Chave: |
Transpiração; Trasnpiração. |
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Thesagro: |
Climatologia; Evaporação. |
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Thesaurus Nal: |
Amazonia. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/149606/1/hess-2015-552.pdf
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/149045/1/hess-20-4237-2016.pdf
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Marc: |
LEADER 03867naa a2200409 a 4500
001 2055915
005 2022-05-20
008 2016 bl uuuu u00u1 u #d
024 7 $a10.5194/hess-2015-552$2DOI
100 1 $aMALLICK, K.
245 $aCanopy-scale biophysical controls of transpiration and evaporation in the Amazon Basin.$h[electronic resource]
260 $c2016
520 $aCanopy and aerodynamic conductances (gC and gA) are two of the key land surface biophysical variables that control the land surface response of land surface schemes in climate models. Their representation is crucial for predicting transpiration (λET) and evaporation (λEE) flux components of the terrestrial latent heat flux (λE), which has important implications for global climate change and water resource management. By physical integration of radiometric surface temperature (TR) into an integrated framework of the Penman?Monteith and Shuttleworth?Wallace models, we present a novel approach to directly quantify the canopy-scale biophysical controls on λET and λEE over multiple plant functional types (PFTs) in the Amazon Basin. Combining data from six LBA (Large-scale Biosphere-Atmosphere Experiment in Amazonia) eddy covariance tower sites and a TR-driven physically based modeling approach, we identified the canopy-scale feedback-response mechanism between gC, λET, and atmospheric vapor pressure deficit (DA), without using any leaf-scale empirical parameterizations for the modeling. The TR-based model shows minor biophysical control on λET during the wet (rainy) seasons where λET becomes predominantly radiation driven and net radiation (RN) determines 75 to 80 % of the variances of λET. However, biophysical control on λET is dramatically increased during the dry seasons, and particularly the 2005 drought year, explaining 50 to 65 % of the variances of λET, and indicates λET to be substantially soil moisture driven during the rainfall deficit phase. Despite substantial differences in gA between forests and pastures, very similar canopy?atmosphere "coupling" was found in these two biomes due to soil moisture-induced decrease in gC in the pasture. This revealed the pragmatic aspect of the TR-driven model behavior that exhibits a high sensitivity of gC to per unit change in wetness as opposed to gA that is marginally sensitive to surface wetness variability. Our results reveal the occurrence of a significant hysteresis between λET and gC during the dry season for the pasture sites, which is attributed to relatively low soil water availability as compared to the rainforests, likely due to differences in rooting depth between the two systems. Evaporation was significantly influenced by gA for all the PFTs and across all wetness conditions. Our analytical framework logically captures the responses of gC and gA to changes in atmospheric radiation, DA, and surface radiometric temperature, and thus appears to be promising for the improvement of existing land?surface?atmosphere exchange parameterizations across a range of spatial scales.
650 $aAmazonia
650 $aClimatologia
650 $aEvaporação
653 $aTranspiração
653 $aTrasnpiração
700 1 $aTREBS, I.
700 1 $aBOEGH, E.
700 1 $aGIUSTARINI, L.
700 1 $aSCHLERF, M.
700 1 $aDREWRY, D. T.
700 1 $aHOFFMANN, L.
700 1 $aRANDOW, C. von
700 1 $aKRUIJT, B.
700 1 $aARAUJO, A.
700 1 $aSALESKA, S.
700 1 $aEHLERINGER, J. R.
700 1 $aDOMINGUES, T. F.
700 1 $aOMETTO, J. P. H. B.
700 1 $aNOBRE, A. D.
700 1 $aMORAES, O. L. L. de
700 1 $aHAYEK, M.
700 1 $aMUNGER, J. W.
700 1 $aWOFSY, S. C.
773 $tHydrology and Earth System Science Discussions, 27 Jan. 2016.
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Registro original: |
Embrapa Amazônia Oriental (CPATU) |
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 | Acesso ao texto completo restrito à biblioteca da Embrapa Caprinos e Ovinos. Para informações adicionais entre em contato com cnpc.biblioteca@embrapa.br. |
Registro Completo
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Biblioteca(s): |
Embrapa Caprinos e Ovinos. |
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Data corrente: |
09/12/2019 |
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Data da última atualização: |
10/12/2019 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
B - 1 |
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Autoria: |
VASCONCELOS, A. M. de; OSTERNO, J. J.; ROGERIO, M. C. P.; FAÇANHA, D. A. E.; LANDIM, A. V.; PINHEIRO, A. A.; SILVEIRA, R. M. F.; FERREIRA, J. B. |
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Afiliação: |
ANGELA MARIA DE VASCONCELOS; JULIANA JUSTINO OSTERNO; MARCOS CLAUDIO PINHEIRO ROGERIO, CNPC; DÉBORA ANDRÉA EVANGELISTA FAÇANHA; ALINE VIEIRA LANDIM; ALICE ANDRIOLI PINHEIRO, CNPC; ROBSON MATEUS FREITAS SILVEIRA; JOSIEL BORGES FERREIRA. |
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Título: |
Adaptive profile of Saanen goats in tropical conditions. |
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Ano de publicação: |
2019 |
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Fonte/Imprenta: |
Biological Rhythm Research, v. 50, 2019. |
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DOI: |
https://doi.org/10.1080/09291016.2019.1603691 |
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Idioma: |
Inglês |
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Conteúdo: |
The objective was to characterize the adaptive profile and thermoregulatory responses of Saanen goats raised under tropical conditions. Twenty dairy goats were used. Its rectal temperature (RT, °C), respiratory rate (RR, breaths min?1), and heart rate (HR, bpm) were collected biweekly for two consecutive years. Individual blood samples were collected for determination of thyroxine (T4; ?g dL?1). All physiological responses were higher in the afternoon, except for RR which was higher in the morning. The RT and RR were higher in the rainy season, and HR and T4 levels had no effect between periods of the year. The RT, HR, RR and T4, in this order of importance, are the most important variables to characterize the adaptive profile of the animals. The thermoregulatory responses during the morning and afternoon shifts were similar, whereas between periods of the year the animals used different mechanisms to maintain homeostasis. Saanen goats mainly use the latent thermoregulation mechanisms in the rainy season as a form of endogenous heat dissipation and the sensitive mechanisms in the dry season. The RT is a physiological variable that presents discriminatory power for evaluation of adaptive aspects in Saanen goats in tropical conditions. |
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Palavras-Chave: |
Thermolysis. |
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Thesaurus NAL: |
Animal adaptation; Dairy goats; Multivariate analysis; Semiarid zones. |
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Categoria do assunto: |
L Ciência Animal e Produtos de Origem Animal |
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Marc: |
LEADER 02060naa a2200277 a 4500
001 2116415
005 2019-12-10
008 2019 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1080/09291016.2019.1603691$2DOI
100 1 $aVASCONCELOS, A. M. de
245 $aAdaptive profile of Saanen goats in tropical conditions.$h[electronic resource]
260 $c2019
520 $aThe objective was to characterize the adaptive profile and thermoregulatory responses of Saanen goats raised under tropical conditions. Twenty dairy goats were used. Its rectal temperature (RT, °C), respiratory rate (RR, breaths min?1), and heart rate (HR, bpm) were collected biweekly for two consecutive years. Individual blood samples were collected for determination of thyroxine (T4; ?g dL?1). All physiological responses were higher in the afternoon, except for RR which was higher in the morning. The RT and RR were higher in the rainy season, and HR and T4 levels had no effect between periods of the year. The RT, HR, RR and T4, in this order of importance, are the most important variables to characterize the adaptive profile of the animals. The thermoregulatory responses during the morning and afternoon shifts were similar, whereas between periods of the year the animals used different mechanisms to maintain homeostasis. Saanen goats mainly use the latent thermoregulation mechanisms in the rainy season as a form of endogenous heat dissipation and the sensitive mechanisms in the dry season. The RT is a physiological variable that presents discriminatory power for evaluation of adaptive aspects in Saanen goats in tropical conditions.
650 $aAnimal adaptation
650 $aDairy goats
650 $aMultivariate analysis
650 $aSemiarid zones
653 $aThermolysis
700 1 $aOSTERNO, J. J.
700 1 $aROGERIO, M. C. P.
700 1 $aFAÇANHA, D. A. E.
700 1 $aLANDIM, A. V.
700 1 $aPINHEIRO, A. A.
700 1 $aSILVEIRA, R. M. F.
700 1 $aFERREIRA, J. B.
773 $tBiological Rhythm Research$gv. 50, 2019.
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Embrapa Caprinos e Ovinos (CNPC) |
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