Báo cáo khoa học: A generic model of forest canopy conductance dependent on climate, soil water availability and leaf area index
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Tuyển tập các báo cáo nghiên cứu về lâm nghiệp được đăng trên tạp chí lâm nghiệp quốc tế đề tài: A generic model of forest canopy conductance dependent on climate, soil water availability and leaf area index...
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Báo cáo khoa học: "A generic model of forest canopy conductance dependent on climate, soil water availability and leaf area index" 755Ann. For. Sci. 57 (2000) 755–765© INRA, EDP Sciences Original article A generic model of forest canopy conductance dependent on climate, soil water availability and leaf area index André Graniera,*, Denis Loustaub and Nathalie Brédaa a Institut National de la Recherche Agronomique, Unité dÉcophysiologie Forestière, 54280 Champenoux, France b Institut National de la Recherche Agronomique, Unité de Recherches Forestières, BP 45, 33611 Gazinet Cedex, France (Received 2 June 2000; accepted 3 October 2000)Abstract – This paper analyses the variation in tree canopy conductance for water vapour (gc) in order to derive a general expression,including the effects of solar radiation (R), vapour pressure deficit (D), leaf area index (LAI) and extractable soil water. Canopy con-ductance was calculated from transpiration measured in 21 broadleaved and coniferous forest stands, under different climates: tem-perate, mountain, tropical and boreal. Common features in the dependence of gc on climate and on soil water content were exhibited.When soil water was not limiting, gc was shown to increase linearly with LAI in the range 0 to 6 m2 m–2 and reach a plateau value.Besides the positive effect of increasing R and the negative effect of increasing D on gc, it was surprisingly shown that a decrease inextractable soil water induced a similar reduction in gc in various tree species, equally in coniferous and in broadleaved. Based on thesefindings, a general canopy conductance function is proposed.canopy conductance / sap flow / transpiration / species comparison / leaf area index / water stress / model / synthesisRésumé – Un modèle générique de conductance de couverts forestiers dépendant du climat, de la disponibilité en eau dans lesol et de l’indice foliaire. Ce travail réalise lanalyse des facteurs de variation de la conductance du couvert pour la vapeur deau (gc)avec lobjectif den donner une expression générale, prenant en compte les effets du rayonnement global (R), du déficit de saturationde lair (D), de lindice foliaire (LAI) et de la réserve hydrique extractible du sol. La conductance du couvert a été calculée à partir dela transpiration mesurée dans 21 peuplements forestiers feuillus et résineux, sous différents types climatiques : tempéré, montagnard,tropical et boréal. Ce travail a montré, pour ces divers peuplements, une dépendance similaire entre gc et les facteurs climatiques, ainsiquavec la réserve hydrique extractible du sol (REW). En conditions hydriques non limitantes, on observe que gc augmente linéaire-ment avec le LAI entre 0 et 6 m2 m–2, puis atteint un plateau. De façon surprenante, en dehors de leffet positif sur gc de laugmenta-tion de R, et leffet négatif de celle de D, on montre que la diminution de REW a des conséquences similaires sur gc pour diversesespèces forestières, aussi bien feuillues que résineuses. À partir de ces observations, un modèle général de conductance de couvert estproposé ici.conductance de couvert / flux de sève / transpiration / comparaison inter spécifique / indice foliaire / sécheresse / modèle /synthèse* Correspondence and reprintsTél. (33) 03 83 39 40 38 ; Fax. (33) 03 83 39 40 69 ; e-mail: agranier@nancy.inra.fr756 A. Granier et al. 1. INTRODUCTION whole canopy acts as a single layer for water exchange to the atmosphere, even if it has been demonstrated that multilayer models are more suitable for detailed physio- During the last decades, a large number of studies have logical functioning of the forest canopy [39].been conducted, quantifying forest transpiration and itsspatial and temporal variation, under various stand condi- The objectives of this paper are to: 1) compare canopytions (age, species, site, climate), involving different conductance among a large range of forest stands, differ-techniques. High time scale resolution (hour) data can be ing in species composition or in climatic and soil charac-obtained through sap flow measurements [28], which teristics; 2) evaluate the effect of leaf area index as ...
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Báo cáo khoa học: "A generic model of forest canopy conductance dependent on climate, soil water availability and leaf area index" 755Ann. For. Sci. 57 (2000) 755–765© INRA, EDP Sciences Original article A generic model of forest canopy conductance dependent on climate, soil water availability and leaf area index André Graniera,*, Denis Loustaub and Nathalie Brédaa a Institut National de la Recherche Agronomique, Unité dÉcophysiologie Forestière, 54280 Champenoux, France b Institut National de la Recherche Agronomique, Unité de Recherches Forestières, BP 45, 33611 Gazinet Cedex, France (Received 2 June 2000; accepted 3 October 2000)Abstract – This paper analyses the variation in tree canopy conductance for water vapour (gc) in order to derive a general expression,including the effects of solar radiation (R), vapour pressure deficit (D), leaf area index (LAI) and extractable soil water. Canopy con-ductance was calculated from transpiration measured in 21 broadleaved and coniferous forest stands, under different climates: tem-perate, mountain, tropical and boreal. Common features in the dependence of gc on climate and on soil water content were exhibited.When soil water was not limiting, gc was shown to increase linearly with LAI in the range 0 to 6 m2 m–2 and reach a plateau value.Besides the positive effect of increasing R and the negative effect of increasing D on gc, it was surprisingly shown that a decrease inextractable soil water induced a similar reduction in gc in various tree species, equally in coniferous and in broadleaved. Based on thesefindings, a general canopy conductance function is proposed.canopy conductance / sap flow / transpiration / species comparison / leaf area index / water stress / model / synthesisRésumé – Un modèle générique de conductance de couverts forestiers dépendant du climat, de la disponibilité en eau dans lesol et de l’indice foliaire. Ce travail réalise lanalyse des facteurs de variation de la conductance du couvert pour la vapeur deau (gc)avec lobjectif den donner une expression générale, prenant en compte les effets du rayonnement global (R), du déficit de saturationde lair (D), de lindice foliaire (LAI) et de la réserve hydrique extractible du sol. La conductance du couvert a été calculée à partir dela transpiration mesurée dans 21 peuplements forestiers feuillus et résineux, sous différents types climatiques : tempéré, montagnard,tropical et boréal. Ce travail a montré, pour ces divers peuplements, une dépendance similaire entre gc et les facteurs climatiques, ainsiquavec la réserve hydrique extractible du sol (REW). En conditions hydriques non limitantes, on observe que gc augmente linéaire-ment avec le LAI entre 0 et 6 m2 m–2, puis atteint un plateau. De façon surprenante, en dehors de leffet positif sur gc de laugmenta-tion de R, et leffet négatif de celle de D, on montre que la diminution de REW a des conséquences similaires sur gc pour diversesespèces forestières, aussi bien feuillues que résineuses. À partir de ces observations, un modèle général de conductance de couvert estproposé ici.conductance de couvert / flux de sève / transpiration / comparaison inter spécifique / indice foliaire / sécheresse / modèle /synthèse* Correspondence and reprintsTél. (33) 03 83 39 40 38 ; Fax. (33) 03 83 39 40 69 ; e-mail: agranier@nancy.inra.fr756 A. Granier et al. 1. INTRODUCTION whole canopy acts as a single layer for water exchange to the atmosphere, even if it has been demonstrated that multilayer models are more suitable for detailed physio- During the last decades, a large number of studies have logical functioning of the forest canopy [39].been conducted, quantifying forest transpiration and itsspatial and temporal variation, under various stand condi- The objectives of this paper are to: 1) compare canopytions (age, species, site, climate), involving different conductance among a large range of forest stands, differ-techniques. High time scale resolution (hour) data can be ing in species composition or in climatic and soil charac-obtained through sap flow measurements [28], which teristics; 2) evaluate the effect of leaf area index as ...
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