Number of the records: 1  

Different maximum latewood density and blue intensity measurements techniques reveal similar results

  1. 1.
    SYSNO ASEP0496018
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JČlánek ve WOS
    TitleDifferent maximum latewood density and blue intensity measurements techniques reveal similar results
    Author(s) Kaczka, R. J. (PL)
    Spyt, B. (PL)
    Janecka, K. (DE)
    Beil, I. (DE)
    Büntgen, Ulf (UEK-B) RID, ORCID, SAI
    Scharnweber, T. (DE)
    Nievergelt, D. (CH)
    Wilmking, M. (DE)
    Number of authors8
    Source TitleDendrochronologia. - : Elsevier - ISSN 1125-7865
    Roč. 49, JUN (2018), s. 94-101
    Number of pages8 s.
    Languageeng - English
    CountryIT - Italy
    Keywordssummer temperature-variations ; tree-ring chronologies ; wood density ; paleoclimate proxy ; giant mountains ; picea-abies ; climate ; growth ; reconstruction ; width ; Climate reconstruction ; Dendrochronology ; Maximum Wood Density ; Blue intensity ; Norway spruce ; Tatra Mountains
    Subject RIVDB - Geology ; Mineralogy
    OECD categoryPhysical geography
    R&D ProjectsLO1415 GA MŠMT - Ministry of Education, Youth and Sports (MEYS)
    Institutional supportUEK-B - RVO:86652079
    UT WOS000433995400011
    EID SCOPUS85044724653
    DOI10.1016/j.dendro.2018.03.005
    AnnotationAnnually resolved and absolutely dated Maximum Latewood Density (MXD) and Blue Intensity (BI) measurements are frequently used for reconstructing summer temperature variability over the last centuries to millennia. A direct comparison of the outcome of both methods using similar material is needed due to how quickly this method is being adopted. The application of slightly different measuring systems (hardware) and analysis tools (software) in tandem with different wood samples and preparation procedures further challenges any straightforward assessment. Here we process 26 Norway spruce samples from the upper timberline in the Polish Tatra Mountains with the six most frequently used MXD and BI applications. Although offset is found in the raw MXD and BI data (0.04-0.13 g/cm(3) and 0.45-1.58 dimensionless blue intensity), interannual and longer-term fluctuations are significantly (p < 0.01) positively correlated between all MXD and BI time-series. Our results emphasize the potential of faster and cheaper, as well as overall more user-friendly techniques to generate reliable MXD surrogates for high-frequency dendroclimatological studies. Although the correlations between MXD and BI were lower than within MXD and BI, the results of growth-climate response performed for both proxies show only marginal differences. The obtained level-offset further questions the suitability of joining different density surrogates for developing long-term composite chronologies to reconstruct low-frequency climate variability.
    WorkplaceGlobal Change Research Institute
    ContactNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Year of Publishing2019
Number of the records: 1  

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