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hal.structure.identifierCentre de Recherche sur la Biodiversité et l'Environnement [CRBE]
dc.contributor.authorHES, Gabriel
hal.structure.identifierUniversität Bern = University of Bern = Université de Berne [UNIBE]
dc.contributor.authorVANDERKELEN, Inne
hal.structure.identifierNational Center for Atmospheric Research [Boulder] [NCAR]
dc.contributor.authorFISHER, Rosie
hal.structure.identifierCentre de Recherche sur la Biodiversité et l'Environnement [CRBE]
dc.contributor.authorCHAVE, Jérôme
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorOGÉE, Jérôme
hal.structure.identifierUniversität Bern = University of Bern = Université de Berne [UNIBE]
dc.contributor.authorL DAVIN, Edouard
dc.date.accessioned2024-04-08T11:37:43Z
dc.date.available2024-04-08T11:37:43Z
dc.date.issued2024-01-30
dc.identifier.issn1748-9326
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/195010
dc.description.abstractEnThe forest understory experiences temperature variations that are dampened compared to adjacent open areas, allowing the development of a forest microclimate and associated ecological conditions. It is however unclear to what extent forests will maintain this buffering effect under increasing global warming. Providing reliable projections of future forest microclimates is therefore crucial to anticipate climate change impacts on forest biodiversity, and to identify corresponding conservation strategies. Recent empirical studies suggest that the buffering of air temperature extremes in forest understory compared to open land could increase with global warming, albeit at a slower rate than macroclimate temperatures. Here, we investigate the trend of this temperature buffering effect in a high-emission global warming scenario, using the process-based Land Surface Model CLM5.1. We find biome-dependant buffering trends with strongest values in tropical forests where buffering increases for every degree of global warming by 0.1 • C for maximum soil temperature, and by 0.2 • C for maximum canopy air temperature. In boreal regions, forest microclimate exhibits a strong seasonality and the effect of global warming is more uncertain. Thus, our results highlight the importance of tropical forest canopies in particular, in maintaining hospitable conditions for understory species while increasing their climate debt under global warming. Our research also illustrates the potential and limitations of Land Surface Models to simulate forest microclimate, and calls for further collaborations between Earth system modelers and ecologists to jointly question climate and biosphere dynamics.
dc.description.sponsorshipImpact de la gestion forestière et du changement climatique sur le microclimat en sous-bois - ANR-21-CE32-0012
dc.language.isoen
dc.publisherIOP Publishing
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.subject.enCommunity Land Model
dc.subject.enforest modeling
dc.subject.entemperature buffering
dc.subject.entropical biodiversity
dc.subject.enclimate change
dc.subject.enLand Surface Model
dc.subject.ensoil temperature
dc.title.enProjecting future forest microclimate using a land surface model
dc.typeArticle de revue
dc.identifier.doi10.1088/1748-9326/ad1f04
dc.subject.halSciences de l'environnement
bordeaux.journalEnvironmental Research Letters
bordeaux.page024030
bordeaux.volume19
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.issue2
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-04467792
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-04467792v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Environmental%20Research%20Letters&rft.date=2024-01-30&rft.volume=19&rft.issue=2&rft.spage=024030&rft.epage=024030&rft.eissn=1748-9326&rft.issn=1748-9326&rft.au=HES,%20Gabriel&VANDERKELEN,%20Inne&FISHER,%20Rosie&CHAVE,%20J%C3%A9r%C3%B4me&OG%C3%89E,%20J%C3%A9r%C3%B4me&rft.genre=article


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