Počet záznamů: 1  

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

  1. 1.
    SYSNO ASEP0496018
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevDifferent maximum latewood density and blue intensity measurements techniques reveal similar results
    Tvůrce(i) 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)
    Celkový počet autorů8
    Zdroj.dok.Dendrochronologia. - : Elsevier - ISSN 1125-7865
    Roč. 49, JUN (2018), s. 94-101
    Poč.str.8 s.
    Jazyk dok.eng - angličtina
    Země vyd.IT - Itálie
    Klíč. slovasummer 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
    Vědní obor RIVDB - Geologie a mineralogie
    Obor OECDPhysical geography
    CEPLO1415 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy
    Institucionální podporaUEK-B - RVO:86652079
    UT WOS000433995400011
    EID SCOPUS85044724653
    DOI10.1016/j.dendro.2018.03.005
    AnotaceAnnually 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.
    PracovištěÚstav výzkumu globální změny
    KontaktNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Rok sběru2019
Počet záznamů: 1  

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