- Growth trends and climate responses of Norway spruce along elevationa…
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Growth trends and climate responses of Norway spruce along elevational gradients in East-Central Europe

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    SYSNO ASEP0473130
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleGrowth trends and climate responses of Norway spruce along elevational gradients in East-Central Europe
    Author(s) Ponočná, T. (CZ)
    Spyt, B. (PL)
    Kaczka, R. J. (PL)
    Büntgen, Ulf (UEK-B) RID, ORCID, SAI
    Treml, V. (CZ)
    Number of authors5
    Source TitleTrees: structure and function. - : Springer - ISSN 0931-1890
    Roč. 30, č. 5 (2016), s. 1633-1646
    Number of pages14 s.
    Languageeng - English
    CountryDE - Germany
    Keywordsabies l. karst. ; tree-ring chronologies ; basal area increment ; radial growth ; forest growth ; altitudinal gradient ; sudetes mountains ; northern europe ; tatra mountains ; alps ; climate change ; mountain forests ; picea abies ; radial growth ; rree rings ; trend preservation
    Subject RIVGK - Forestry
    R&D ProjectsEE2.3.20.0248 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Institutional supportRVO:67179843 - RVO:67179843
    UT WOS000384406000014
    EID SCOPUS84963649859
    DOI https://doi.org/10.1007/s00468-016-1396-3
    AnnotationDecadal growth variability of Norway spruce increases with elevation. Recent temperature sensitivity and growth enhancement are limited to trees growing in the zone adjacent to timberline. Growth trends and climate responses of forest trees along elevational gradients are not fully understood. A deeper insight is, however, fundamental for predicting ecosystem functioning and productivity under future climate change. Supplementary to the effects of elevation and regional provenance on tree growth are sample depth, uneven representation of sample age and varying site conditions. Furthermore, there is only a limited number of studies addressing growth changes along elevational gradients, while at the same time applying tree-ring standardization methods that are sensitive to trend preservation. Here, we introduce 12 novel tree-ring width chronologies of Norway spruce (Picea abies[L.] Karst.) from four elevational belts encompassing montane forests and the local timberline in three regions in East-Central Europe between 15A degrees and 19A degrees E. Each chronology is characterized by sufficient sample replication and a comparable age structure between 1906 and 2010. Tree growth near timberline revealed substantial medium-frequency variability and sharply increasing ring widths since the 1980s. Medium-frequency growth variability of lower elevation trees was, however, relatively small, and growth rates over the last decade were either stable or even decreased. During the last four decades, Norway spruce from higher elevations exhibited a reduced response to autumn temperatures preceding ring formation. In contrast, trees from the lower-montane zone increased their sensitivity to drought during the same time. Our results emphasize not only different but also instable growth trends and climate responses of forest trees along altitudinal gradients, which should be considered in future forest management strategies.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2017
Number of the records: 1  

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