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dc.rights.licenseopenen_US
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSGUBIN, Giovanni
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSWINGEDOUW, Didier
dc.contributor.authorDAYON, Gildas
dc.contributor.authorGARCÍA DE CORTÁZAR-ATAURI, Iñaki
hal.structure.identifierEcophysiologie et Génomique Fonctionnelle de la Vigne [UMR EGFV]
dc.contributor.authorOLLAT, Nathalie
IDREF: 126740062
dc.contributor.authorPAGÉ, Christian
hal.structure.identifierEcophysiologie et Génomique Fonctionnelle de la Vigne [UMR EGFV]
dc.contributor.authorVAN LEEUWEN, Cornelis
ORCID: 0000-0002-9428-0167
IDREF: 200518208
dc.date.accessioned2020-04-08T12:52:10Z
dc.date.available2020-04-08T12:52:10Z
dc.date.issued2018
dc.identifier.issn0168-1923en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/4177
dc.description.abstractEnTardive frosts, i.e. frost events occurring after grapevine budburst, are a significant risk for viticultural practices, which have recently caused substantial yield losses over different winegrowing regions of France, e.g. in 2016 and 2017. So far, it is unclear whether the frequency of late frosts events is destined to increase or decrease under future climatic conditions. Here, we assess the risk of tardive frosts for the French vineyards throughout the 21st century by analyzing temperature projections from eight climate models and their statistical regional down scaling. Our approach consists in comparing the statistical occurrences of the last frost (day of the year) and the characteristic budburst date for nine grapevine varieties as simulated by three different phenological models. Climate models qualitatively agree in projecting a gradual increase in temperature all over the France, which generally produces both an earlier characteristic last frost day and an earlier characteristic budburst date. However, the latter notably depends on the specific phenological model, implying a large uncertainty in assessing the risk exposure. Overall, we identified Alsace, Burgundy and Champagne as the most vulnerable regions, where the probability of tardive frost is projected to significantly increase throughout the 21st century for two out of three phenological models. The third phenological model produces opposite results, but the comparison between simulated budburst dates and observed records over the last 60 years suggests its lower reliability. Nevertheless, for a more trustworthy risk assessment, the validity of the budburst models should be accurately tested also for warmer climate conditions, in order to narrow down the associated large uncertainty.
dc.language.isoENen_US
dc.subjectGelée Tardive
dc.subjectChangement climatique
dc.subjectVitis Vinifera
dc.subjectPhénologie
dc.subject.enClimate Change
dc.subject.enVitis Vinifera L.
dc.subject.enGeneral Circulation Model
dc.subject.enStatistical Downscaling
dc.subject.enPhenological Model
dc.subject.enSpring Frost
dc.title.enThe risk of tardive frost damage in French vineyards in a changing climate
dc.title.alternativeAgric. for. metereol.en_US
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.agrformet.2017.12.253en_US
dc.subject.halSciences du Vivant [q-bio]/Biologie végétaleen_US
bordeaux.journalAgricultural and Forest Meteorologyen_US
bordeaux.page226-242en_US
bordeaux.volume250-251en_US
bordeaux.hal.laboratoriesEcophysiologie et Génomique Fonctionnelle de la Vigne (EGFV) - UMR 1287en_US
bordeaux.institutionBordeaux Sciences Agroen_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
hal.identifierhal-02536952
hal.version1
hal.date.transferred2020-04-08T12:52:16Z
hal.exporttrue
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