Number of the records: 1  

Past millennium hydroclimate variability from Corsican pine tree-ring chronologies

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    SYSNO ASEP0559665
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitlePast millennium hydroclimate variability from Corsican pine tree-ring chronologies
    Author(s) Esper, Jan (UEK-B) SAI, ORCID, RID
    Hartl, C. (DE)
    Konter, O. (DE)
    Reinig, F. (DE)
    Roemer, P. (DE)
    Huneau, F. (FR)
    Lebre, S. (FR)
    Szymczak, S. (DE)
    Braeuning, A. (DE)
    Büntgen, Ulf (UEK-B) RID, ORCID, SAI
    Number of authors10
    Source TitleBoreas. - : Wiley - ISSN 0300-9483
    Roč. 51, č. 3 (2022), s. 621-636
    Number of pages16 s.
    Languageeng - English
    CountryUS - United States
    Keywordssummer temperature ; reconstruction ; drought reconstruction ; climate reconstruction ; iberian range ; large-scale ; growth ; sensitivity ; network ; signals ; width
    Subject RIVEF - Botanics
    OECD categoryPlant sciences, botany
    R&D ProjectsEF16_019/0000797 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Research InfrastructureCzeCOS III - 90123 - Ústav výzkumu globální změny AV ČR, v. v. i.
    Method of publishingOpen access
    Institutional supportUEK-B - RVO:86652079
    UT WOS000730929400001
    EID SCOPUS85121341690
    DOI10.1111/bor.12574
    AnnotationPalaeoclimatic evidence is necessary to place the current warming and drying trends of the Mediterranean region in a long-term perspective of pre-industrial variability. Annually resolved and absolutely dated climate proxies that extend back into medieval times are, however, limited to a few sites only. Here we present a network of long ring width chronologies from Pinus nigra tree-line sites in northern Corsica (France) that cohere exceptionally well over centuries and support the development of a single high-elevation pine chronology extending back to 974 CE. We apply various detrending methods to these data to retain high-to-low frequency ring width variability and scale the resulting chronologies against instrumental precipitation and drought observations to produce hydroclimate reconstructions for the last millennium. Proxy calibration and transfer are challenged by a lack of high-elevation meteorological data, however, limiting our understanding of precipitation changes in sub-alpine tree-line environments. Our new reconstructions extend beyond existing records and provide evidence for low-frequency precipitation variability in the central-western Mediterranean from 974-2016 CE. Comparison with a European scale drought reconstruction network shows that regional predictor chronologies are needed to accurately estimate long-term hydroclimate variability on Corsica.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2023
    Electronic addresshttps://onlinelibrary.wiley.com/doi/10.1111/bor.12574
Number of the records: 1  

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