Patterns and controls of the variability of radiation use efficiency and primary productivity across terrestrial ecosystems

Aim: The controls of gross radiation use efficiency [RUE], the ratio between gross primary productivity [GPP] and the radiation intercepted by terrestrial vegetation, and its spatial and temporal variation are not yet fully understood. Our objectives were to analyse and synthesize the spatial variab...

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Otros Autores: Garbulsky, Martín Fabio, Peñuelas, Josep, Papale, Dario, Ardö, Jonas, Goulden, Michael L., Kiely, Gerard, Richardson, Andrew D., Rotenberg, Eyal, Veenendaal, Elmar M., Filella, Iolanda
Formato: Artículo
Lenguaje:Inglés
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Acceso en línea:http://ri.agro.uba.ar/files/intranet/articulo/2010Garbulsky.pdf
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Aporte de:Registro referencial: Solicitar el recurso aquí
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245 1 0 |a Patterns and controls of the variability of radiation use efficiency and primary productivity across terrestrial ecosystems 
520 |a Aim: The controls of gross radiation use efficiency [RUE], the ratio between gross primary productivity [GPP] and the radiation intercepted by terrestrial vegetation, and its spatial and temporal variation are not yet fully understood. Our objectives were to analyse and synthesize the spatial variability of GPP and the spatial and temporal variability of RUE and its climatic controls for a wide range of vegetation types. Location: A global range of sites from tundra to rain forest. Methods: We analysed a global dataset on photosynthetic uptake and climatic variables from 35 eddy covariance [EC] flux sites spanning between 100 and 2200 mm mean annual rainfall and between -13 and 26°C mean annual temperature. RUE was calculated from the data provided by EC flux sites and remote sensing [MODIS]. Results: Rainfall and actual evapotranspiration [AET] positively influenced the spatial variation of annual GPP, whereas temperature only influenced the GPP of forests. Annual and maximum RUE were also positively controlled primarily by annual rainfall. The main control parameters of the growth season variation of gross RUE varied for each ecosystem type. Overall, the ratio between actual and potential evapotranspiration and a surrogate for the energy balance explained a greater proportion of the seasonal variation of RUE than the vapour pressure deficit [VPD], AET and precipitation. Temperature was important for determining the intra-annual variability of the RUE at the coldest energy-limited sites. Main conclusions: Our analysis supports the idea that the annual functioning of vegetation that is adapted to its local environment is more constrained by water availability than by temperature. The spatial variability of annual and maximum RUE can be largely explained by annual precipitation, more than by vegetation type. The intra-annual variation of RUE was mainly linked to the energy balance and water availability along the climatic gradient. Furthermore, we showed that intra-annual variation of gross RUE is only weakly influenced by VPD and temperature, contrary to what is frequently assumed. Our results provide a better understanding of the spatial and temporal controls of the RUE and thus could lead to a better estimation of ecosystem carbon fixation and better modelling. 
653 0 |a CARBON CYCLE 
653 0 |a CLIMATIC CONTROLS 
653 0 |a EDDY COVARIANCE 
653 0 |a GROSS PRIMARY PRODUCTIVITY 
653 0 |a RADIATION USE EFFICIENCY 
653 0 |a REMOTE SENSING 
653 0 |a TERRESTRIAL VEGETATION 
653 0 |a CARBON FIXATION 
653 0 |a ECOSYSTEM MODELING 
653 0 |a EVAPOTRANSPIRATION 
653 0 |a LIGHT USE EFFICIENCY 
653 0 |a PRIMARY PRODUCTION 
653 0 |a RAINFOREST 
653 0 |a SPATIAL VARIATION 
653 0 |a TEMPORAL VARIATION 
653 0 |a TERRESTRIAL ECOSYSTEM 
653 0 |a TUNDRA 
653 0 |a VEGETATION TYPE 
700 1 |9 17762  |a Garbulsky, Martín Fabio 
700 1 |a Peñuelas, Josep  |9 50629 
700 1 |a Papale, Dario  |9 72093 
700 1 |a Ardö, Jonas  |9 72094 
700 1 |a Goulden, Michael L.  |9 72095 
700 1 |a Kiely, Gerard  |9 14651 
700 1 |a Richardson, Andrew D.  |9 72096 
700 1 |a Rotenberg, Eyal  |9 72097 
700 1 |a Veenendaal, Elmar M.  |9 72098 
700 1 |9 66929  |a Filella, Iolanda 
773 |t Global Ecology and Biogeography  |g Vol.19, no.2 (2010), p.253-267 
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900 |a ^aGarbulsky^bM.F. 
900 |a ^aPeñuelas^bJ. 
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900 |a ^aPeñuelas^bJ. 
900 |a ^aPapale^bD. 
900 |a ^aArdö^bJ. 
900 |a ^aGoulden^bM. L. 
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900 |a ^aRotenberg^bE. 
900 |a ^aVeenendaal^bE. M. 
900 |a ^aFilella^bI. 
900 |a ^aGarbulsky^bM.F.^tUnitat d'Ecofisiologia i Canvi Global - CSIC-CEAB-CREAF, CREAF Centre de Recerca Ecològica i Aplicacions Forestals, Universitat Autònoma de Barcelona, 08193 Bellaterra, Catalunya, Spain 
900 |a ^aPeñuelas^bJ.^tFaculty of Agronomy, University of Buenos Aires, C1417DSE, Buenos Aires, Argentina 
900 |a ^aPapale^bD.^tDepartment of Forest Environment and Resources, University of Tuscia, 01100 Viterbo, Italy 
900 |a ^aArdö^bJ.^tDepartment of Physical Geography and Ecosystems Analysis, Lund University, Lund, Sweden 
900 |a ^aGoulden^bM.L.^tDepartment of Earth System Science, University of California, Irvine, CA 92697-3100, United States 
900 |a ^aKiely^bG.^tCentre for Hydrology, Meteorology and Climate Change, Civil and Environmental Engineering Department, University College Cork, Ireland 
900 |a ^aRichardson^bA.D.^tDepartment of Organismic and Evolutionary Biology, Harvard University, Cambridge, MA 02138, United States 
900 |a ^aRotenberg^bE.^tEnvironmental Sciences and Energy Research, Weizmann Institute of Science, Rehovot 76100, Israel 
900 |a ^aVeenendaal^bE.M.^tNature Conservation and Plant Ecology Group, Wageningen University, 6708 PD Wageningen, Netherlands 
900 |a ^aFilella^bI. 
900 |a ^tGlobal Ecology and Biogeography^cGlobal Ecol. Biogeogr. 
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900 |a 253 
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900 |a Vol. 19, no. 2 
900 |a 267 
900 |a CARBON CYCLE 
900 |a CLIMATIC CONTROLS 
900 |a EDDY COVARIANCE 
900 |a GROSS PRIMARY PRODUCTIVITY 
900 |a RADIATION USE EFFICIENCY 
900 |a REMOTE SENSING 
900 |a TERRESTRIAL VEGETATION 
900 |a CARBON FIXATION 
900 |a ECOSYSTEM MODELING 
900 |a EVAPOTRANSPIRATION 
900 |a LIGHT USE EFFICIENCY 
900 |a PRIMARY PRODUCTION 
900 |a RAINFOREST 
900 |a SPATIAL VARIATION 
900 |a TEMPORAL VARIATION 
900 |a TERRESTRIAL ECOSYSTEM 
900 |a TUNDRA 
900 |a VEGETATION TYPE 
900 |a Aim: The controls of gross radiation use efficiency [RUE], the ratio between gross primary productivity [GPP] and the radiation intercepted by terrestrial vegetation, and its spatial and temporal variation are not yet fully understood. Our objectives were to analyse and synthesize the spatial variability of GPP and the spatial and temporal variability of RUE and its climatic controls for a wide range of vegetation types. Location: A global range of sites from tundra to rain forest. Methods: We analysed a global dataset on photosynthetic uptake and climatic variables from 35 eddy covariance [EC] flux sites spanning between 100 and 2200 mm mean annual rainfall and between -13 and 26°C mean annual temperature. RUE was calculated from the data provided by EC flux sites and remote sensing [MODIS]. Results: Rainfall and actual evapotranspiration [AET] positively influenced the spatial variation of annual GPP, whereas temperature only influenced the GPP of forests. Annual and maximum RUE were also positively controlled primarily by annual rainfall. The main control parameters of the growth season variation of gross RUE varied for each ecosystem type. Overall, the ratio between actual and potential evapotranspiration and a surrogate for the energy balance explained a greater proportion of the seasonal variation of RUE than the vapour pressure deficit [VPD], AET and precipitation. Temperature was important for determining the intra-annual variability of the RUE at the coldest energy-limited sites. Main conclusions: Our analysis supports the idea that the annual functioning of vegetation that is adapted to its local environment is more constrained by water availability than by temperature. The spatial variability of annual and maximum RUE can be largely explained by annual precipitation, more than by vegetation type. The intra-annual variation of RUE was mainly linked to the energy balance and water availability along the climatic gradient. Furthermore, we showed that intra-annual variation of gross RUE is only weakly influenced by VPD and temperature, contrary to what is frequently assumed. Our results provide a better understanding of the spatial and temporal controls of the RUE and thus could lead to a better estimation of ecosystem carbon fixation and better modelling. 
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