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Assessing parameter variability in a photosynthesis model within and between plant functional types using global Fluxnet eddy covariance data

Identifieur interne : 003E06 ( PascalFrancis/Curation ); précédent : 003E05; suivant : 003E07

Assessing parameter variability in a photosynthesis model within and between plant functional types using global Fluxnet eddy covariance data

Auteurs : M. Groenendijk [Pays-Bas] ; A. J. Dolman [Pays-Bas] ; M. K. Van Der Molen [Pays-Bas] ; R. Leuning [Australie] ; A. Arneth [Suède] ; N. Delpierre [France] ; J. H. C. Gash [Pays-Bas, Royaume-Uni] ; A. Lindroth [Suède] ; A. D. Richardson [États-Unis] ; H. Verbeeck [Belgique] ; G. Wohlfahrt [Autriche]

Source :

RBID : Pascal:11-0032158

Descripteurs français

English descriptors

Abstract

The vegetation component in climate models has advanced since the late 1960s from a uniform prescription of surface parameters to plant functional types (PFTs). PFTs are used in global land-surface models to provide parameter values for every model grid cell. With a simple photosynthesis model we derive parameters for all site years within the Fluxnet eddy covariance data set. We compare the model parameters within and between PFTs and statistically group the sites. Fluxnet data is used to validate the photosynthesis model parameter variation within a PFT classification. Our major result is that model parameters appear more variable than assumed in PFTs. Simulated fluxes are of higher quality when model parameters of individual sites or site years are used. A simplification with less variation in model parameters results in poorer simulations. This indicates that a PFT classification introduces uncertainty in the variation of the photosynthesis and transpiration fluxes. Statistically derived groups of sites with comparable model parameters do not share common vegetation types or climates. A simple PFT classification does not reflect the real photosynthesis and transpiration variation. Although site year parameters give the best predictions, the parameters are generally too specific to be used in a global study. The site year parameters can be further used to explore the possibilities of alternative classification schemes.
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A08 01  1  ENG  @1 Assessing parameter variability in a photosynthesis model within and between plant functional types using global Fluxnet eddy covariance data
A11 01  1    @1 GROENENDIJK (M.)
A11 02  1    @1 DOLMAN (A. J.)
A11 03  1    @1 VAN DER MOLEN (M. K.)
A11 04  1    @1 LEUNING (R.)
A11 05  1    @1 ARNETH (A.)
A11 06  1    @1 DELPIERRE (N.)
A11 07  1    @1 GASH (J. H. C.)
A11 08  1    @1 LINDROTH (A.)
A11 09  1    @1 RICHARDSON (A. D.)
A11 10  1    @1 VERBEECK (H.)
A11 11  1    @1 WOHLFAHRT (G.)
A14 01      @1 VU University Amsterdam, Hydrology and Geo-Environmental Sciences @3 NLD @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 7 aut.
A14 02      @1 CSIRO Marine and Atmospheric Research @2 Canberra @3 AUS @Z 4 aut.
A14 03      @1 Department of Earth and Ecosystem Sciences, Lund University @3 SWE @Z 5 aut. @Z 8 aut.
A14 04      @1 Universite Paris-Sud, Laboratoire Ecologie Systematique et Evolution, UMR8079 @2 Orsay 91405 @3 FRA @Z 6 aut.
A14 05      @1 Centre for Ecology and Hydrology @2 Wallingford @3 GBR @Z 7 aut.
A14 06      @1 Harvard University, Department of Organismic and Evolutionary Biology, HUH, 22 Divinity Avenue @2 Cambridge, MA 02138 @3 USA @Z 9 aut.
A14 07      @1 Laboratory of Plant Ecology, Ghent University, Coupure Links 653 @2 9000 Ghent @3 BEL @Z 10 aut.
A14 08      @1 Institut für Ökologie, Universität Innsbruck @3 AUT @Z 11 aut.
A20       @1 22-38
A21       @1 2011
A23 01      @0 ENG
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C01 01    ENG  @0 The vegetation component in climate models has advanced since the late 1960s from a uniform prescription of surface parameters to plant functional types (PFTs). PFTs are used in global land-surface models to provide parameter values for every model grid cell. With a simple photosynthesis model we derive parameters for all site years within the Fluxnet eddy covariance data set. We compare the model parameters within and between PFTs and statistically group the sites. Fluxnet data is used to validate the photosynthesis model parameter variation within a PFT classification. Our major result is that model parameters appear more variable than assumed in PFTs. Simulated fluxes are of higher quality when model parameters of individual sites or site years are used. A simplification with less variation in model parameters results in poorer simulations. This indicates that a PFT classification introduces uncertainty in the variation of the photosynthesis and transpiration fluxes. Statistically derived groups of sites with comparable model parameters do not share common vegetation types or climates. A simple PFT classification does not reflect the real photosynthesis and transpiration variation. Although site year parameters give the best predictions, the parameters are generally too specific to be used in a global study. The site year parameters can be further used to explore the possibilities of alternative classification schemes.
C02 01  X    @0 002A32C03
C03 01  X  FRE  @0 Paramètre @5 01
C03 01  X  ENG  @0 Parameter @5 01
C03 01  X  SPA  @0 Parámetro @5 01
C03 02  X  FRE  @0 Variabilité @5 02
C03 02  X  ENG  @0 Variability @5 02
C03 02  X  SPA  @0 Variabilidad @5 02
C03 03  X  FRE  @0 Photosynthèse @5 03
C03 03  X  ENG  @0 Photosynthesis @5 03
C03 03  X  SPA  @0 Fotosíntesis @5 03
C03 04  X  FRE  @0 Modélisation @5 04
C03 04  X  ENG  @0 Modeling @5 04
C03 04  X  SPA  @0 Modelización @5 04
C03 05  X  FRE  @0 Utilisation @5 05
C03 05  X  ENG  @0 Use @5 05
C03 05  X  SPA  @0 Uso @5 05
C03 06  X  FRE  @0 Méthode covariance turbulence @5 06
C03 06  X  ENG  @0 Eddy covariance method @5 06
C03 06  X  SPA  @0 Método covariancia turbulencia @5 06
C03 07  X  FRE  @0 Donnée @5 07
C03 07  X  ENG  @0 Data @5 07
C03 07  X  SPA  @0 Dato @5 07
C03 08  X  FRE  @0 Transpiration @5 08
C03 08  X  ENG  @0 Transpiration @5 08
C03 08  X  SPA  @0 Transpiración @5 08
C03 09  X  FRE  @0 Biométéorologie @5 09
C03 09  X  ENG  @0 Biometeorology @5 09
C03 09  X  SPA  @0 Biometeorología @5 09
C03 10  X  FRE  @0 Modèle @5 28
C03 10  X  ENG  @0 Models @5 28
C03 10  X  SPA  @0 Modelo @5 28
C03 11  X  FRE  @0 Mathématiques appliquées @5 29
C03 11  X  ENG  @0 Applied mathematics @5 29
C03 11  X  SPA  @0 Matemáticas aplicadas @5 29
C03 12  X  FRE  @0 <<>> @4 INC @5 68
C07 01  X  FRE  @0 Méthode statistique @5 33
C07 01  X  ENG  @0 Statistical method @5 33
C07 01  X  SPA  @0 Método estadístico @5 33
N21       @1 024
N44 01      @1 OTO
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Pascal:11-0032158

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<div type="abstract" xml:lang="en">The vegetation component in climate models has advanced since the late 1960s from a uniform prescription of surface parameters to plant functional types (PFTs). PFTs are used in global land-surface models to provide parameter values for every model grid cell. With a simple photosynthesis model we derive parameters for all site years within the Fluxnet eddy covariance data set. We compare the model parameters within and between PFTs and statistically group the sites. Fluxnet data is used to validate the photosynthesis model parameter variation within a PFT classification. Our major result is that model parameters appear more variable than assumed in PFTs. Simulated fluxes are of higher quality when model parameters of individual sites or site years are used. A simplification with less variation in model parameters results in poorer simulations. This indicates that a PFT classification introduces uncertainty in the variation of the photosynthesis and transpiration fluxes. Statistically derived groups of sites with comparable model parameters do not share common vegetation types or climates. A simple PFT classification does not reflect the real photosynthesis and transpiration variation. Although site year parameters give the best predictions, the parameters are generally too specific to be used in a global study. The site year parameters can be further used to explore the possibilities of alternative classification schemes.</div>
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<fA08 i1="01" i2="1" l="ENG">
<s1>Assessing parameter variability in a photosynthesis model within and between plant functional types using global Fluxnet eddy covariance data</s1>
</fA08>
<fA11 i1="01" i2="1">
<s1>GROENENDIJK (M.)</s1>
</fA11>
<fA11 i1="02" i2="1">
<s1>DOLMAN (A. J.)</s1>
</fA11>
<fA11 i1="03" i2="1">
<s1>VAN DER MOLEN (M. K.)</s1>
</fA11>
<fA11 i1="04" i2="1">
<s1>LEUNING (R.)</s1>
</fA11>
<fA11 i1="05" i2="1">
<s1>ARNETH (A.)</s1>
</fA11>
<fA11 i1="06" i2="1">
<s1>DELPIERRE (N.)</s1>
</fA11>
<fA11 i1="07" i2="1">
<s1>GASH (J. H. C.)</s1>
</fA11>
<fA11 i1="08" i2="1">
<s1>LINDROTH (A.)</s1>
</fA11>
<fA11 i1="09" i2="1">
<s1>RICHARDSON (A. D.)</s1>
</fA11>
<fA11 i1="10" i2="1">
<s1>VERBEECK (H.)</s1>
</fA11>
<fA11 i1="11" i2="1">
<s1>WOHLFAHRT (G.)</s1>
</fA11>
<fA14 i1="01">
<s1>VU University Amsterdam, Hydrology and Geo-Environmental Sciences</s1>
<s3>NLD</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="02">
<s1>CSIRO Marine and Atmospheric Research</s1>
<s2>Canberra</s2>
<s3>AUS</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="03">
<s1>Department of Earth and Ecosystem Sciences, Lund University</s1>
<s3>SWE</s3>
<sZ>5 aut.</sZ>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="04">
<s1>Universite Paris-Sud, Laboratoire Ecologie Systematique et Evolution, UMR8079</s1>
<s2>Orsay 91405</s2>
<s3>FRA</s3>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="05">
<s1>Centre for Ecology and Hydrology</s1>
<s2>Wallingford</s2>
<s3>GBR</s3>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="06">
<s1>Harvard University, Department of Organismic and Evolutionary Biology, HUH, 22 Divinity Avenue</s1>
<s2>Cambridge, MA 02138</s2>
<s3>USA</s3>
<sZ>9 aut.</sZ>
</fA14>
<fA14 i1="07">
<s1>Laboratory of Plant Ecology, Ghent University, Coupure Links 653</s1>
<s2>9000 Ghent</s2>
<s3>BEL</s3>
<sZ>10 aut.</sZ>
</fA14>
<fA14 i1="08">
<s1>Institut für Ökologie, Universität Innsbruck</s1>
<s3>AUT</s3>
<sZ>11 aut.</sZ>
</fA14>
<fA20>
<s1>22-38</s1>
</fA20>
<fA21>
<s1>2011</s1>
</fA21>
<fA23 i1="01">
<s0>ENG</s0>
</fA23>
<fA43 i1="01">
<s1>INIST</s1>
<s2>11784</s2>
<s5>354000194934860030</s5>
</fA43>
<fA44>
<s0>0000</s0>
<s1>© 2011 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45>
<s0>2 p.3/4</s0>
</fA45>
<fA47 i1="01" i2="1">
<s0>11-0032158</s0>
</fA47>
<fA60>
<s1>P</s1>
<s3>PR</s3>
</fA60>
<fA61>
<s0>A</s0>
</fA61>
<fA64 i1="01" i2="1">
<s0>Agricultural and forest meteorology : (Print)</s0>
</fA64>
<fA66 i1="01">
<s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG">
<s0>The vegetation component in climate models has advanced since the late 1960s from a uniform prescription of surface parameters to plant functional types (PFTs). PFTs are used in global land-surface models to provide parameter values for every model grid cell. With a simple photosynthesis model we derive parameters for all site years within the Fluxnet eddy covariance data set. We compare the model parameters within and between PFTs and statistically group the sites. Fluxnet data is used to validate the photosynthesis model parameter variation within a PFT classification. Our major result is that model parameters appear more variable than assumed in PFTs. Simulated fluxes are of higher quality when model parameters of individual sites or site years are used. A simplification with less variation in model parameters results in poorer simulations. This indicates that a PFT classification introduces uncertainty in the variation of the photosynthesis and transpiration fluxes. Statistically derived groups of sites with comparable model parameters do not share common vegetation types or climates. A simple PFT classification does not reflect the real photosynthesis and transpiration variation. Although site year parameters give the best predictions, the parameters are generally too specific to be used in a global study. The site year parameters can be further used to explore the possibilities of alternative classification schemes.</s0>
</fC01>
<fC02 i1="01" i2="X">
<s0>002A32C03</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE">
<s0>Paramètre</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG">
<s0>Parameter</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA">
<s0>Parámetro</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE">
<s0>Variabilité</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG">
<s0>Variability</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA">
<s0>Variabilidad</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE">
<s0>Photosynthèse</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG">
<s0>Photosynthesis</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA">
<s0>Fotosíntesis</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE">
<s0>Modélisation</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG">
<s0>Modeling</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA">
<s0>Modelización</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE">
<s0>Utilisation</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG">
<s0>Use</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA">
<s0>Uso</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE">
<s0>Méthode covariance turbulence</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG">
<s0>Eddy covariance method</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA">
<s0>Método covariancia turbulencia</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE">
<s0>Donnée</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG">
<s0>Data</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA">
<s0>Dato</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE">
<s0>Transpiration</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG">
<s0>Transpiration</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA">
<s0>Transpiración</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE">
<s0>Biométéorologie</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG">
<s0>Biometeorology</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA">
<s0>Biometeorología</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE">
<s0>Modèle</s0>
<s5>28</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG">
<s0>Models</s0>
<s5>28</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA">
<s0>Modelo</s0>
<s5>28</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE">
<s0>Mathématiques appliquées</s0>
<s5>29</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG">
<s0>Applied mathematics</s0>
<s5>29</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA">
<s0>Matemáticas aplicadas</s0>
<s5>29</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE">
<s0><<>></s0>
<s4>INC</s4>
<s5>68</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE">
<s0>Méthode statistique</s0>
<s5>33</s5>
</fC07>
<fC07 i1="01" i2="X" l="ENG">
<s0>Statistical method</s0>
<s5>33</s5>
</fC07>
<fC07 i1="01" i2="X" l="SPA">
<s0>Método estadístico</s0>
<s5>33</s5>
</fC07>
<fN21>
<s1>024</s1>
</fN21>
<fN44 i1="01">
<s1>OTO</s1>
</fN44>
<fN82>
<s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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