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dc.contributor.authorTejedor, Ernestoes_ES
dc.contributor.authorSerrano-Notivoli, Robertoes_ES
dc.contributor.authorLuis, Martín dees_ES
dc.contributor.authorSaz-Sánchez, Miguel Ángeles_ES
dc.contributor.authorHartl, Claudiaes_ES
dc.contributor.authorGeorge, Scott Stes_ES
dc.contributor.authorBüntgen, Ulfes_ES
dc.contributor.authorLiebhold, Andrew M.es_ES
dc.contributor.authorVuille, Mathiases_ES
dc.contributor.authorEsper, Janes_ES
dc.date.accessioned2020-06-29T09:33:58Z-
dc.date.available2020-06-29T09:33:58Z-
dc.date.issued2020-07-
dc.identifier.citationTejedor E, Serrano-Notivoli R, de Luis M, Saz MA, Hartl C, George S, Büntgen U, Liebhold AM, Vuille M, Esper J. A global perspective on the climate‐driven growth synchrony of neighbouring trees. Global Ecology and Biogeography 29 (7): 1114-1125 (2020)es_ES
dc.identifier.issn1466-822X-
dc.identifier.urihttp://hdl.handle.net/10261/215458-
dc.description2 .pdf files: File 1. Author's article final version, Post-Print (19 Pags.- 4 Figs.- 2 Tabls.). File 2. Supplementary Materials (3 Figs.- 2 Tabls.- 1 Model Equation).es_ES
dc.description.abstractAim Previous work demonstrated the global variability of synchrony in tree growth within populations, that is, the covariance of the year‐to‐year variability in growth of individual neighbouring trees. However, there is a lack of knowledge about the causes of this variability and its trajectories through time. Here, we examine whether climate can explain variation in within‐population synchrony (WPS) across space but also through time and we develop models capable of explaining this variation. These models can be applied to the global tree cover under current and future climate change scenarios. Location Global. Time period 1901–2012. Major taxa studied Trees. Methods We estimated WPS values from a global tree‐ring width database consisting of annual growth increment measurements from multiple trees at 3,579 sites. We used generalized linear mixed effects models to infer the drivers of WPS variability and temporal trends of global WPS. We then predicted WPS values across the global extent of tree cover. Finally, we applied our model to predict future WPS based on the RCP 8.5 (2045–2065 period) emission scenario. Results Areas with the highest WPS are characterized by a combination of environments with both high mean annual temperature (>10°C) and low precipitation (<300 mm). Average WPS across all temperate forests has decreased historically and will continue to decrease. Potential implications of these patterns include changes in forest dynamics, such as higher tree growth and productivity and an increase in carbon sequestration. In contrast, the WPS of tropical forests of Central and South America will increase in the near future owing to reduced annual precipitation. Main conclusions Climate explains WPS variability in space and time. We suggest that WPS might have value as an integrative ecological measure of the level of environmental stress to which forests are subjected and therefore holds potential for diagnosing effects of global climate change on tree growth.es_ES
dc.description.sponsorshipE.T. and M.V. were partially supported by National Science Foundation ‐ Partnership in International Research and Education (OISE‐1743738) and National Science Foundation ‐ Paleo Perspectives on Climate Change (AGS‐1702439). R.S.‐N. is funded by a “Juan de la Cierva” postdoctoral grant FJCI‐2017‐31595. E.T., M.S., R.S.‐N. and M.D.L. are supported by the Government of Aragón through the “Program of research groups” (group H38, “Clima, Agua, Cambio Global y Sistemas Naturales”). A.L. was supported by grant EVA4.0, No. CZ.02.1.01/0.0/0.0/16_019/0000803, financed by OP RDE and by the U.S. Department of Agriculture Forest Service.es_ES
dc.language.isoenges_ES
dc.publisherJohn Wiley & Sonses_ES
dc.relation.isversionofPostprintes_ES
dc.rightsopenAccesses_ES
dc.subjectSynchronyes_ES
dc.subjecttree-ringes_ES
dc.subjecttree stress indicatores_ES
dc.subjectGlobales_ES
dc.titleA global perspective on the climate‐driven growth synchrony of neighbouring treeses_ES
dc.typeartículoes_ES
dc.identifier.doi10.1111/geb.13090-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttps://doi.org/10.1111/geb.13090es_ES
dc.identifier.e-issn1466-8238-
dc.embargo.terms2021-07-31es_ES
dc.contributor.funderNational Science Foundation (US)es_ES
dc.contributor.funderGobierno de Aragónes_ES
dc.contributor.funderDepartment of Agriculture (US)es_ES
dc.relation.csices_ES
oprm.item.hasRevisionno ko 0 false*
dc.identifier.funderhttp://dx.doi.org/10.13039/501100010067es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/100000001es_ES
dc.identifier.funderhttp://dx.doi.org/10.13039/100000199es_ES
dc.contributor.orcidSerrano Notivoli, Roberto [0000-0001-7663-1202]es_ES
dc.type.coarhttp://purl.org/coar/resource_type/c_6501es_ES
item.openairetypeartículo-
item.grantfulltextopen-
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
item.languageiso639-1en-
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Serrano-NotivoliR_GlobEcolBiogeog-SuppMat_2020.pdf2. Supplementary Materials1,02 MBAdobe PDFVista previa
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