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A tree ring-based hydroclimate reconstruction for eastern Europe reveals large-scale teleconnection patterns

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    SYSNO ASEP0561609
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleA tree ring-based hydroclimate reconstruction for eastern Europe reveals large-scale teleconnection patterns
    Author(s) Roibu, C. C. (RO)
    Nagavciuc, V. (RO)
    Ionita, M. (DE)
    Popa, I. (RO)
    Horodnic, S.A. (RO)
    Mursa, A. (RO)
    Büntgen, Ulf (UEK-B) RID, ORCID, SAI
    Number of authors7
    Source TitleClimate Dynamics. - : Springer - ISSN 0930-7575
    Roč. 59, č. 3 (2022)
    Number of pages16 s.
    Languageeng - English
    CountryUS - United States
    KeywordsClimate reconstructions ; Dendroclimatology ; Drought extremes ; Eastern Europe ; Teleconnection patterns ; Tree rings ; Beech
    Subject RIVDG - Athmosphere Sciences, Meteorology
    OECD categoryMeteorology and atmospheric sciences
    Research InfrastructureCzeCOS III - 90123 - Ústav výzkumu globální změny AV ČR, v. v. i.
    Method of publishingOpen access
    Institutional supportUEK-B - RVO:86652079
    UT WOS000777360700002
    EID SCOPUS85127399720
    DOI10.1007/s00382-022-06255-8
    AnnotationWe present a new beech (Fagus sylvatica L.) tree-ring width composite chronology from five natural low-elevation forests in eastern Romania, which represent the species' continental distribution limit. Our regional beech chronology reflects April-June hydroclimate variability in form of the Standardized Precipitation Evapotranspiration Index over large parts of Romania, Ukraine, and the Republic of Moldova, for which high-resolution paleoclimatic evidence is broadly missing. Most of the reconstructed hydroclimatic extremes back to 1768 CE are confirmed by documentary evidences, and a robust association is found with large-scale atmospheric circulation patterns in the Northern Hemisphere and sea surface temperatures over the North Atlantic. Reconstructed pluvials coincide with a high-pressure system over the North Atlantic Ocean and north-western Europe, and with a low-pressure system over south-western, central and eastern Europe, whereas historical droughts coincide with a high-pressure system over Europe and a low-pressure system over the central part of the Atlantic Ocean. Our study demonstrates the potential to produce well-replicated, multi-centennial beech chronologies for eastern Europe to reconstruct regional hydroclimate variation and better understand the causes and consequences of large-scale teleconnection patterns.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2023
    Electronic addresshttps://link.springer.com/article/10.1007/s00382-022-06255-8
Number of the records: 1  

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