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dc.contributor.authorAndreu-Hayles, Laia-
dc.contributor.authorGutiérrez, Emilia-
dc.contributor.authorMacías, Marc-
dc.contributor.authorRibas, Montserrat-
dc.contributor.authorBosch, Oriol-
dc.contributor.authorCamarero, Jesús Julio-
dc.date.accessioned2011-05-05T12:11:45Z-
dc.date.available2011-05-05T12:11:45Z-
dc.date.issued2007-04-
dc.identifier.citationGlobal Change Biology 13(4): 804-815 (2007)es_ES
dc.identifier.issn1354-1013-
dc.identifier.urihttp://hdl.handle.net/10261/35320-
dc.description12 páginas, 9 figuras, 1 tabla.es_ES
dc.description.abstractTree populations located at the geographical distribution limit of the species may provide valuable information about tree-growth response to changes on climatic conditions. We established nine Pinus nigra, 12 P. sylvestris and 17 P. uncinata tree-ring width chronologies along the eastern and northern Iberian Peninsula, where these species are found at the edge of their natural range. Tree-growth variability was analyzed using principal component analysis (PCA) for the period 1885–1992. Despite the diversity of species, habitats and climatic regimes, a common macroclimatic signal expressed by the first principal component (PC1) was found. Moreover, considering the PC1 scores as a regional chronology, significant relations were established with Spanish meteorological data. The shared variance held by the tree chronologies, the frequency of narrow rings and the interannual growth variability (sensitivity) increased markedly during the studied period. This shows an enhancement of growth synchrony among forests indicating that climate might have become more limiting to growth. Noticeably, an upward abrupt shift in common variability at the end of the first half of the 20th century was detected. On the other hand, moving-interval response functions showed a change in the growth–climate relationships during the same period. The relationship between growth and late summer/autumn temperatures of the year before growth (August–September, negative correlation, and November, positive correlation) became stronger. Hence, water stress increase during late summer previous to tree growth could be linked to the larger growth synchrony among sites, suggesting that climate was driving the growth pattern changes. This agrees with the upward trend in temperature observed in these months. Moreover, the higher occurrence of extreme years and the sensitivity increase in the second half of the 20th century were in agreement with an increment in precipitation variability during the growing period. Precipitation variability was positively related to tree-growth variability, but negatively to radial growth. In conclusion, a change in tree-growth pattern and in the climatic response of the studied forests was detected since the mid-20th century and linked to an increase in water stress. These temporal trends were in agreement with the observed increase in warmer conditions and in precipitation variability.es_ES
dc.description.sponsorshipData were collected during the CICyT Spanish project (Contract AMB95-0160); EU ForMAT project (Contract ENV4-CT97-0641) and EU ISONET project (Contract EV K2-2001-00237).es_ES
dc.language.isoenges_ES
dc.publisherWiley-Blackwelles_ES
dc.rightsclosedAccesses_ES
dc.subjectClimatic variabilityes_ES
dc.subjectDendroclimatologyes_ES
dc.subjectGlobal warminges_ES
dc.subjectGrowth pattern changees_ES
dc.subjectIberian Peninsulaes_ES
dc.subjectPinus nigraes_ES
dc.subjectP. sylvestrises_ES
dc.subjectP. uncinataes_ES
dc.subjectSpecies distribution limites_ES
dc.subjectWater stresses_ES
dc.titleClimate increases regional tree-growth variability in Iberian pine forestses_ES
dc.typeartículoes_ES
dc.identifier.doi10.1111/j.1365-2486.2007.01322.x-
dc.description.peerreviewedPeer reviewedes_ES
dc.relation.publisherversionhttp://dx.doi.org/10.1111/j.1365-2486.2007.01322.xes_ES
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