CheneBelgiqueV2, PascalFrancis, Curation, bibRecord, 000117

Radial growth change of temperate tree species in response to altered regional climate and air quality in the period 1901-2008

Identifieur interne : 000117 ( PascalFrancis/Curation ); précédent : 000116; suivant : 000118

Radial growth change of temperate tree species in response to altered regional climate and air quality in the period 1901-2008

Auteurs : Vincent Kint [Belgique] ; Wim Aertsen [Belgique] ; Matteo Campioli [Belgique] ; Dries Vansteenkiste [Belgique] ; Andy Delcloo [Belgique] ; Bart Muys [Belgique]

Source :

Climatic change [ 0165-0009 ] ; 2012.

RBID : Pascal:13-0239608

Descripteurs français

Pascal (Inist)
- Siècle 20eme, Croissance, Arbre forestier, Surveillance écologique, Comparaison interspécifique, Modélisation, Climat, Pollution air, Belgique, Quercus, Fagus, Pinus.
Wicri :
- geographic : Belgique.
- topic : Climat.

English descriptors

KwdEn :
- Air pollution, Belgium, Century 20th, Climate, Environmental monitoring, Fagus, Forest tree, Growth, Interspecific comparison, Modeling, Pinus, Quercus.

Abstract

Both increasing and decreasing 20th century growth trends have been reported in forests throughout Europe, but only for few species and areas suitable modelling techniques have been used to distinguish individual tree growth (operating on a local scale) from growth change due to exogenous factors (operating on a broad geographical scale). This study relates for the first time observed growth changes, in terms of basal area increment (BAI) of dominant trees of pedunculate oak, common beech and Scots pine, in north-west European temperate lowland forests (Flanders) to climate, atmospheric CO₂ and tropospheric O₃ concentrations, N deposition, site quality and forest structure for more than a century (the period 1901-2008), applying mixed models. Growth change during the 20th century is observed for oak (increasing growth) and beech (increasing growth until the 1960s, growth decline afterwards), but not for pine. It was possible to relate growth change of oak and beech to climate time series and N deposition trends. Adding time series for CO₂ and O₃ concentration did not significantly improve model results. For oak and beech a switch from positive to negative growth response with increasing nitrogen deposition throughout time is observed. Growth increase for oak is mainly determined by the interaction between growing season temperature and soil water recharge. It is reasonable to assume that the observed growth trend for oak will continue for as long as early season water availability is not compromised. The decreasing trend in summer relative air humidity observed since the 1960s in the study area can be a main cause of recent beech BAI decrease. A further growth decline of beech can be expected, independent of site quality.

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A03		`1`		`@0 Clim. change`
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A08	`01`	`1`	`ENG`	`@1 Radial growth change of temperate tree species in response to altered regional climate and air quality in the period 1901-2008`
A11	`01`	`1`		`@1 KINT (Vincent)`
A11	`02`	`1`		`@1 AERTSEN (Wim)`
A11	`03`	`1`		`@1 CAMPIOLI (Matteo)`
A11	`04`	`1`		`@1 VANSTEENKISTE (Dries)`
A11	`05`	`1`		`@1 DELCLOO (Andy)`
A11	`06`	`1`		`@1 MUYS (Bart)`
A14	`01`			`@1 Division Forest, Nature and Landscape, Department of Earth and Environmental Sciences, Katholieke Universiteit Leuven, Celestijnenlaan 200E, Box 2411 @2 3001 Leuven @3 BEL @Z 1 aut. @Z 2 aut. @Z 6 aut.`
A14	`02`			`@1 Department of Biology, University of Antwerp, Universiteitsplein 1 @2 2610 Wilrijk @3 BEL @Z 3 aut.`
A14	`03`			`@1 Laboratory of Wood Technology, Department of Forest and Water Management, Ghent University, Coupure Links 653 @2 9000 Ghent @3 BEL @Z 4 aut.`
A14	`04`			`@1 Royal Meteorological Institute of Belgium, Ringlaan 3 @2 1180 Brussels @3 BEL @Z 5 aut.`
A20				`@1 343-363`
A21				`@1 2012`
A23	`01`			`@0 ENG`
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A44				`@0 0000 @1 © 2013 INIST-CNRS. All rights reserved.`
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C01	`01`		`ENG`	@0 Both increasing and decreasing 20th century growth trends have been reported in forests throughout Europe, but only for few species and areas suitable modelling techniques have been used to distinguish individual tree growth (operating on a local scale) from growth change due to exogenous factors (operating on a broad geographical scale). This study relates for the first time observed growth changes, in terms of basal area increment (BAI) of dominant trees of pedunculate oak, common beech and Scots pine, in north-west European temperate lowland forests (Flanders) to climate, atmospheric CO₂ and tropospheric O₃ concentrations, N deposition, site quality and forest structure for more than a century (the period 1901-2008), applying mixed models. Growth change during the 20th century is observed for oak (increasing growth) and beech (increasing growth until the 1960s, growth decline afterwards), but not for pine. It was possible to relate growth change of oak and beech to climate time series and N deposition trends. Adding time series for CO₂ and O₃ concentration did not significantly improve model results. For oak and beech a switch from positive to negative growth response with increasing nitrogen deposition throughout time is observed. Growth increase for oak is mainly determined by the interaction between growing season temperature and soil water recharge. It is reasonable to assume that the observed growth trend for oak will continue for as long as early season water availability is not compromised. The decreasing trend in summer relative air humidity observed since the 1960s in the study area can be a main cause of recent beech BAI decrease. A further growth decline of beech can be expected, independent of site quality.
C02	`01`	`X`		`@0 002A14D02B`
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C03	`01`	`X`	`FRE`	`@0 Siècle 20eme @5 01`
C03	`01`	`X`	`ENG`	`@0 Century 20th @5 01`
C03	`01`	`X`	`SPA`	`@0 Siglo 20 @5 01`
C03	`02`	`X`	`FRE`	`@0 Croissance @5 02`
C03	`02`	`X`	`ENG`	`@0 Growth @5 02`
C03	`02`	`X`	`SPA`	`@0 Crecimiento @5 02`
C03	`03`	`X`	`FRE`	`@0 Arbre forestier @5 03`
C03	`03`	`X`	`ENG`	`@0 Forest tree @5 03`
C03	`03`	`X`	`SPA`	`@0 Arbol forestal @5 03`
C03	`04`	`X`	`FRE`	`@0 Surveillance écologique @5 04`
C03	`04`	`X`	`ENG`	`@0 Environmental monitoring @5 04`
C03	`04`	`X`	`SPA`	`@0 Vigilancia ecológica @5 04`
C03	`05`	`X`	`FRE`	`@0 Comparaison interspécifique @5 05`
C03	`05`	`X`	`ENG`	`@0 Interspecific comparison @5 05`
C03	`05`	`X`	`SPA`	`@0 Comparación interespecífica @5 05`
C03	`06`	`X`	`FRE`	`@0 Modélisation @5 06`
C03	`06`	`X`	`ENG`	`@0 Modeling @5 06`
C03	`06`	`X`	`SPA`	`@0 Modelización @5 06`
C03	`07`	`X`	`FRE`	`@0 Climat @5 07`
C03	`07`	`X`	`ENG`	`@0 Climate @5 07`
C03	`07`	`X`	`SPA`	`@0 Clima @5 07`
C03	`08`	`X`	`FRE`	`@0 Pollution air @5 08`
C03	`08`	`X`	`ENG`	`@0 Air pollution @5 08`
C03	`08`	`X`	`SPA`	`@0 Contaminación aire @5 08`
C03	`09`	`X`	`FRE`	`@0 Belgique @2 NG @5 19`
C03	`09`	`X`	`ENG`	`@0 Belgium @2 NG @5 19`
C03	`09`	`X`	`SPA`	`@0 Belgica @2 NG @5 19`
C03	`10`	`X`	`FRE`	`@0 Quercus @2 NS @5 55`
C03	`10`	`X`	`ENG`	`@0 Quercus @2 NS @5 55`
C03	`10`	`X`	`SPA`	`@0 Quercus @2 NS @5 55`
C03	`11`	`X`	`FRE`	`@0 Fagus @2 NS @5 56`
C03	`11`	`X`	`ENG`	`@0 Fagus @2 NS @5 56`
C03	`11`	`X`	`SPA`	`@0 Fagus @2 NS @5 56`
C03	`12`	`X`	`FRE`	`@0 Pinus @2 NS @5 57`
C03	`12`	`X`	`ENG`	`@0 Pinus @2 NS @5 57`
C03	`12`	`X`	`SPA`	`@0 Pinus @2 NS @5 57`
C07	`01`	`X`	`FRE`	`@0 Europe @2 NG`
C07	`01`	`X`	`ENG`	`@0 Europe @2 NG`
C07	`01`	`X`	`SPA`	`@0 Europa @2 NG`
C07	`02`	`X`	`FRE`	`@0 Facteur milieu @5 26`
C07	`02`	`X`	`ENG`	`@0 Environmental factor @5 26`
C07	`02`	`X`	`SPA`	`@0 Factor medio @5 26`
C07	`03`	`X`	`FRE`	`@0 Fagaceae @2 NS`
C07	`03`	`X`	`ENG`	`@0 Fagaceae @2 NS`
C07	`03`	`X`	`SPA`	`@0 Fagaceae @2 NS`
C07	`04`	`X`	`FRE`	`@0 Dicotyledones @2 NS`
C07	`04`	`X`	`ENG`	`@0 Dicotyledones @2 NS`
C07	`04`	`X`	`SPA`	`@0 Dicotyledones @2 NS`
C07	`05`	`X`	`FRE`	`@0 Angiospermae @2 NS`
C07	`05`	`X`	`ENG`	`@0 Angiospermae @2 NS`
C07	`05`	`X`	`SPA`	`@0 Angiospermae @2 NS`
C07	`06`	`X`	`FRE`	`@0 Spermatophyta @2 NS`
C07	`06`	`X`	`ENG`	`@0 Spermatophyta @2 NS`
C07	`06`	`X`	`SPA`	`@0 Spermatophyta @2 NS`
C07	`07`	`X`	`FRE`	`@0 Coniferales @2 NS`
C07	`07`	`X`	`ENG`	`@0 Coniferales @2 NS`
C07	`07`	`X`	`SPA`	`@0 Coniferales @2 NS`
C07	`08`	`X`	`FRE`	`@0 Gymnospermae @2 NS`
C07	`08`	`X`	`ENG`	`@0 Gymnospermae @2 NS`
C07	`08`	`X`	`SPA`	`@0 Gymnospermae @2 NS`
N21				`@1 224`

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Le document en format XML

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<author><name sortKey="Campioli, Matteo" sort="Campioli, Matteo" uniqKey="Campioli M" first="Matteo" last="Campioli">Matteo Campioli</name>
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<author><name sortKey="Vansteenkiste, Dries" sort="Vansteenkiste, Dries" uniqKey="Vansteenkiste D" first="Dries" last="Vansteenkiste">Dries Vansteenkiste</name>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Air pollution</term>
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<term>Century 20th</term>
<term>Climate</term>
<term>Environmental monitoring</term>
<term>Fagus</term>
<term>Forest tree</term>
<term>Growth</term>
<term>Interspecific comparison</term>
<term>Modeling</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Siècle 20eme</term>
<term>Croissance</term>
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<term>Comparaison interspécifique</term>
<term>Modélisation</term>
<term>Climat</term>
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<term>Belgique</term>
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<front><div type="abstract" xml:lang="en">Both increasing and decreasing 20th century growth trends have been reported in forests throughout Europe, but only for few species and areas suitable modelling techniques have been used to distinguish individual tree growth (operating on a local scale) from growth change due to exogenous factors (operating on a broad geographical scale). This study relates for the first time observed growth changes, in terms of basal area increment (BAI) of dominant trees of pedunculate oak, common beech and Scots pine, in north-west European temperate lowland forests (Flanders) to climate, atmospheric CO<sub>2</sub>
 and tropospheric O<sub>3</sub>
 concentrations, N deposition, site quality and forest structure for more than a century (the period 1901-2008), applying mixed models. Growth change during the 20th century is observed for oak (increasing growth) and beech (increasing growth until the 1960s, growth decline afterwards), but not for pine. It was possible to relate growth change of oak and beech to climate time series and N deposition trends. Adding time series for CO<sub>2</sub>
 and O<sub>3</sub>
 concentration did not significantly improve model results. For oak and beech a switch from positive to negative growth response with increasing nitrogen deposition throughout time is observed. Growth increase for oak is mainly determined by the interaction between growing season temperature and soil water recharge. It is reasonable to assume that the observed growth trend for oak will continue for as long as early season water availability is not compromised. The decreasing trend in summer relative air humidity observed since the 1960s in the study area can be a main cause of recent beech BAI decrease. A further growth decline of beech can be expected, independent of site quality.</div>
</front>
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<fA08 i1="01" i2="1" l="ENG"><s1>Radial growth change of temperate tree species in response to altered regional climate and air quality in the period 1901-2008</s1>
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<fA11 i1="01" i2="1"><s1>KINT (Vincent)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>AERTSEN (Wim)</s1>
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<fA11 i1="03" i2="1"><s1>CAMPIOLI (Matteo)</s1>
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<fA11 i1="04" i2="1"><s1>VANSTEENKISTE (Dries)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>DELCLOO (Andy)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>MUYS (Bart)</s1>
</fA11>
<fA14 i1="01"><s1>Division Forest, Nature and Landscape, Department of Earth and Environmental Sciences, Katholieke Universiteit Leuven, Celestijnenlaan 200E, Box 2411</s1>
<s2>3001 Leuven</s2>
<s3>BEL</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Department of Biology, University of Antwerp, Universiteitsplein 1</s1>
<s2>2610 Wilrijk</s2>
<s3>BEL</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Laboratory of Wood Technology, Department of Forest and Water Management, Ghent University, Coupure Links 653</s1>
<s2>9000 Ghent</s2>
<s3>BEL</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Royal Meteorological Institute of Belgium, Ringlaan 3</s1>
<s2>1180 Brussels</s2>
<s3>BEL</s3>
<sZ>5 aut.</sZ>
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<fA45><s0>3 p.1/4</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>13-0239608</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Climatic change</s0>
</fA64>
<fA66 i1="01"><s0>DEU</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Both increasing and decreasing 20th century growth trends have been reported in forests throughout Europe, but only for few species and areas suitable modelling techniques have been used to distinguish individual tree growth (operating on a local scale) from growth change due to exogenous factors (operating on a broad geographical scale). This study relates for the first time observed growth changes, in terms of basal area increment (BAI) of dominant trees of pedunculate oak, common beech and Scots pine, in north-west European temperate lowland forests (Flanders) to climate, atmospheric CO<sub>2</sub>
 and tropospheric O<sub>3</sub>
 concentrations, N deposition, site quality and forest structure for more than a century (the period 1901-2008), applying mixed models. Growth change during the 20th century is observed for oak (increasing growth) and beech (increasing growth until the 1960s, growth decline afterwards), but not for pine. It was possible to relate growth change of oak and beech to climate time series and N deposition trends. Adding time series for CO<sub>2</sub>
 and O<sub>3</sub>
 concentration did not significantly improve model results. For oak and beech a switch from positive to negative growth response with increasing nitrogen deposition throughout time is observed. Growth increase for oak is mainly determined by the interaction between growing season temperature and soil water recharge. It is reasonable to assume that the observed growth trend for oak will continue for as long as early season water availability is not compromised. The decreasing trend in summer relative air humidity observed since the 1960s in the study area can be a main cause of recent beech BAI decrease. A further growth decline of beech can be expected, independent of site quality.</s0>
</fC01>
<fC02 i1="01" i2="X"><s0>002A14D02B</s0>
</fC02>
<fC02 i1="02" i2="X"><s0>002A14D05C</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Siècle 20eme</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Century 20th</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Siglo 20</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Croissance</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Growth</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Crecimiento</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Arbre forestier</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Forest tree</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Arbol forestal</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="X" l="FRE"><s0>Surveillance écologique</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="ENG"><s0>Environmental monitoring</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="X" l="SPA"><s0>Vigilancia ecológica</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Comparaison interspécifique</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Interspecific comparison</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Comparación interespecífica</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="X" l="FRE"><s0>Modélisation</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="ENG"><s0>Modeling</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="X" l="SPA"><s0>Modelización</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="X" l="FRE"><s0>Climat</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="ENG"><s0>Climate</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="X" l="SPA"><s0>Clima</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Pollution air</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Air pollution</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Contaminación aire</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="X" l="FRE"><s0>Belgique</s0>
<s2>NG</s2>
<s5>19</s5>
</fC03>
<fC03 i1="09" i2="X" l="ENG"><s0>Belgium</s0>
<s2>NG</s2>
<s5>19</s5>
</fC03>
<fC03 i1="09" i2="X" l="SPA"><s0>Belgica</s0>
<s2>NG</s2>
<s5>19</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE"><s0>Quercus</s0>
<s2>NS</s2>
<s5>55</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG"><s0>Quercus</s0>
<s2>NS</s2>
<s5>55</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA"><s0>Quercus</s0>
<s2>NS</s2>
<s5>55</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE"><s0>Fagus</s0>
<s2>NS</s2>
<s5>56</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG"><s0>Fagus</s0>
<s2>NS</s2>
<s5>56</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA"><s0>Fagus</s0>
<s2>NS</s2>
<s5>56</s5>
</fC03>
<fC03 i1="12" i2="X" l="FRE"><s0>Pinus</s0>
<s2>NS</s2>
<s5>57</s5>
</fC03>
<fC03 i1="12" i2="X" l="ENG"><s0>Pinus</s0>
<s2>NS</s2>
<s5>57</s5>
</fC03>
<fC03 i1="12" i2="X" l="SPA"><s0>Pinus</s0>
<s2>NS</s2>
<s5>57</s5>
</fC03>
<fC07 i1="01" i2="X" l="FRE"><s0>Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="ENG"><s0>Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="X" l="SPA"><s0>Europa</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="X" l="FRE"><s0>Facteur milieu</s0>
<s5>26</s5>
</fC07>
<fC07 i1="02" i2="X" l="ENG"><s0>Environmental factor</s0>
<s5>26</s5>
</fC07>
<fC07 i1="02" i2="X" l="SPA"><s0>Factor medio</s0>
<s5>26</s5>
</fC07>
<fC07 i1="03" i2="X" l="FRE"><s0>Fagaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="ENG"><s0>Fagaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="03" i2="X" l="SPA"><s0>Fagaceae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="FRE"><s0>Dicotyledones</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="ENG"><s0>Dicotyledones</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="04" i2="X" l="SPA"><s0>Dicotyledones</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="FRE"><s0>Angiospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="ENG"><s0>Angiospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="05" i2="X" l="SPA"><s0>Angiospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="FRE"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="ENG"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="06" i2="X" l="SPA"><s0>Spermatophyta</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="07" i2="X" l="FRE"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="07" i2="X" l="ENG"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="07" i2="X" l="SPA"><s0>Coniferales</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="08" i2="X" l="FRE"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="08" i2="X" l="ENG"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fC07 i1="08" i2="X" l="SPA"><s0>Gymnospermae</s0>
<s2>NS</s2>
</fC07>
<fN21><s1>224</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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Radial growth change of temperate tree species in response to altered regional climate and air quality in the period 1901-2008

Radial growth change of temperate tree species in response to altered regional climate and air quality in the period 1901-2008

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