Signals and memory in tree-ring width and density data
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F15%3A00473315" target="_blank" >RIV/86652079:_____/15:00473315 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.dendro.2015.07.001" target="_blank" >http://dx.doi.org/10.1016/j.dendro.2015.07.001</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.dendro.2015.07.001" target="_blank" >10.1016/j.dendro.2015.07.001</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Signals and memory in tree-ring width and density data
Popis výsledku v původním jazyce
It has been suggested that maximum latewood density (MXD) should be used instead of tree-ring width (TRW) data to reconstruct post-volcanic cooling effects. A thorough assessment of high frequency signals and potentially differing memory effects in long MXD and TRW chronologies, in response to large volcanic eruptions, is still missing, however. We here present a compilation of MXD and TRW chronologies from 11 sites in the Northern Hemisphere, covering the past 750+ years, and containing significant June-August temperature signals. Basic assessment of the data using Superposed Epoch Analysis reveals a temporally extended response in TRW, by 2-3 years, to large volcanic eruptions, though post-volcanic cooling patterns vary considerably within the Northern Hemisphere network Comparison with instrumental temperature data demonstrates the TRW chronologies underestimate cold conditions associated with large volcanic eruptions, a bias that is mitigated in the MXD data. While species composition (pine, spruce, larch) has no detectable influence on the cooling patterns, trees from high latitude sites (>60 degrees N) indicate a stronger and delayed (1-2 years) response to large eruptions, compared to the lower latitude sites (<60 degrees N). These basic findings caution against using TRW data for quantitatively estimating post-volcanic cooling and for comparison against the simulated climate effects of volcanic eruptions in models.
Název v anglickém jazyce
Signals and memory in tree-ring width and density data
Popis výsledku anglicky
It has been suggested that maximum latewood density (MXD) should be used instead of tree-ring width (TRW) data to reconstruct post-volcanic cooling effects. A thorough assessment of high frequency signals and potentially differing memory effects in long MXD and TRW chronologies, in response to large volcanic eruptions, is still missing, however. We here present a compilation of MXD and TRW chronologies from 11 sites in the Northern Hemisphere, covering the past 750+ years, and containing significant June-August temperature signals. Basic assessment of the data using Superposed Epoch Analysis reveals a temporally extended response in TRW, by 2-3 years, to large volcanic eruptions, though post-volcanic cooling patterns vary considerably within the Northern Hemisphere network Comparison with instrumental temperature data demonstrates the TRW chronologies underestimate cold conditions associated with large volcanic eruptions, a bias that is mitigated in the MXD data. While species composition (pine, spruce, larch) has no detectable influence on the cooling patterns, trees from high latitude sites (>60 degrees N) indicate a stronger and delayed (1-2 years) response to large eruptions, compared to the lower latitude sites (<60 degrees N). These basic findings caution against using TRW data for quantitatively estimating post-volcanic cooling and for comparison against the simulated climate effects of volcanic eruptions in models.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
EH - Ekologie – společenstva
OECD FORD obor
—
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Dendrochronologia
ISSN
1125-7865
e-ISSN
—
Svazek periodika
35
Číslo periodika v rámci svazku
OCT
Stát vydavatele periodika
IT - Italská republika
Počet stran výsledku
9
Strana od-do
62-70
Kód UT WoS článku
000362926500008
EID výsledku v databázi Scopus
2-s2.0-84937713273