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dc.contributor.authorGOURLEZ DE LA MOTTE, Louis
dc.contributor.authorBEAUCLAIRE, Quentin
dc.contributor.authorHEINESCH, Bernard
hal.structure.identifierSILVA [SILVA]
dc.contributor.authorCUNTZ, Mathias
hal.structure.identifierGlobal Change Research Centre [CzechGlobe]
dc.contributor.authorFOLTÝNOVÁ, Lenka
hal.structure.identifierGlobal Change Research Centre [CzechGlobe]
dc.contributor.authorŠIGUT, Ladislav
hal.structure.identifierGlobal Change Research Centre [CzechGlobe]
dc.contributor.authorKOWALSKA, Natalia
hal.structure.identifierEuropean Commission - Joint Research Centre [Ispra] [JRC]
dc.contributor.authorMANCA, Giovanni
hal.structure.identifierEuropean Commission - Joint Research Centre [Ispra] [JRC]
dc.contributor.authorBALLARIN, Ignacio Goded
hal.structure.identifierUniversité Catholique de Louvain = Catholic University of Louvain [UCL]
dc.contributor.authorVINCKE, Caroline
hal.structure.identifierUniversity of Antwerp [UA]
dc.contributor.authorROLAND, Marilyn
hal.structure.identifierDanmarks Tekniske Universitet = Technical University of Denmark [DTU]
dc.contributor.authorIBROM, Andreas
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorLOUSTEAU, Denis
hal.structure.identifierGeorg-August-University of Göttingen = Georg-August-Universität Göttingen
dc.contributor.authorSIEBICKE, Lukas
hal.structure.identifierResearch Institute for Nature and Forest [INBO]
dc.contributor.authorNEIRYINK, Johan
dc.contributor.authorLONGDOZ, Bernard
dc.date.accessioned2024-04-08T11:53:11Z
dc.date.available2024-04-08T11:53:11Z
dc.date.issued2020-10-26
dc.identifier.issn0962-8436
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/195519
dc.description.abstractEnSevere drought events are known to cause important reductions of gross primary productivity (GPP) in forest ecosystems. However, it is still unclear whether this reduction originates from stomatal closure (Stomatal Origin Limitation) and/or non-stomatal limitations (Non-SOL). In this study, we investigated the impact of edaphic drought in 2018 onGPPand its origin (SOL, NSOL) using a dataset of 10 European forest ecosystem flux towers. In all stations whereGPPreductions were observed during the drought, these were largely explained by declines in the maximum apparent canopy scale carboxylation rateV(CMAX,APP)(NSOL) when the soil relative extractable water content dropped below around 0.4. Concurrently, we found that the stomatal slope parameter (G(1), related to SOL) of the Medlynet al. unified optimization model linking vegetation conductance andGPPremained relatively constant. These results strengthen the increasing evidence that NSOL should be included in stomatal conductance/photosynthesis models to faithfully simulate bothGPPand water fluxes in forest ecosystems during severe drought. This article is part of the theme issue 'Impacts of the 2018 severe drought and heatwave in Europe: from site to continental scale'.
dc.language.isoen
dc.publisherRoyal Society, The
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/
dc.subject.enPhotosynthesis
dc.subject.enForest
dc.subject.enStomatal conductance
dc.subject.enmodel
dc.subject.enDrought
dc.subject.enEddy covariance
dc.title.enNon-stomatal processes reduce gross primary productivity in temperate forest ecosystems during severe edaphic drought
dc.typeArticle de revue
dc.identifier.doi10.1098/rstb.2019.0527
dc.subject.halSciences de l'environnement
bordeaux.journalPhilosophical Transactions of the Royal Society B: Biological Sciences
bordeaux.page1-11
bordeaux.volume375
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.issue1810
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-02957456
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-02957456v1
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