Climate sensitivity of high- and low-elevation Larix decidua MXD chronologies from the Tatra Mountains

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F20%3A00524414" target="_blank" >RIV/86652079:_____/20:00524414 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/20:00116941

Výsledek na webu

<a href="https://www.sciencedirect.com/science/article/pii/S1125786520300126?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S1125786520300126?via%3Dihub</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.dendro.2020.125674" target="_blank" >10.1016/j.dendro.2020.125674</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Climate sensitivity of high- and low-elevation Larix decidua MXD chronologies from the Tatra Mountains

Popis výsledku v původním jazyce

Maximum latewood density (MXD) measurements from high-elevation/-latitude sites are an important proxy for summer temperature reconstructions. Here, we present 201 MXD series from living larch (Larix decidua Mill.) trees that were growing at around 850 and 1450 m a.s.l. in the Slovakian Tatra Mountains, together with 56 MXD series from historical timbers of the same species and region. We explore the climate signal at the high- and low-elevation sites and assess the effects of varying temperature and precipitation regimes on MXD formation. Ranging from spring temperature to summer precipitation, the elevation-specific climate sensitivity suggests that the MXD measurements from living and relict sources should not be merged for paleoclimatic studies. This finding emphasizes the challenge of attributing a predominant climate factor that controls wood formation across a wide range of historical constructions. A better understanding of the 'true' climate signal requires more samples during the period of overlap between the living and historical trees.

Název v anglickém jazyce

Climate sensitivity of high- and low-elevation Larix decidua MXD chronologies from the Tatra Mountains

Popis výsledku anglicky

Maximum latewood density (MXD) measurements from high-elevation/-latitude sites are an important proxy for summer temperature reconstructions. Here, we present 201 MXD series from living larch (Larix decidua Mill.) trees that were growing at around 850 and 1450 m a.s.l. in the Slovakian Tatra Mountains, together with 56 MXD series from historical timbers of the same species and region. We explore the climate signal at the high- and low-elevation sites and assess the effects of varying temperature and precipitation regimes on MXD formation. Ranging from spring temperature to summer precipitation, the elevation-specific climate sensitivity suggests that the MXD measurements from living and relict sources should not be merged for paleoclimatic studies. This finding emphasizes the challenge of attributing a predominant climate factor that controls wood formation across a wide range of historical constructions. A better understanding of the 'true' climate signal requires more samples during the period of overlap between the living and historical trees.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

40102 - Forestry

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2020

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Dendrochronologia

ISSN

1125-7865

e-ISSN

—

Svazek periodika

60

Číslo periodika v rámci svazku

APR 2020

Stát vydavatele periodika

IT - Italská republika

Počet stran výsledku

9

Strana od-do

125674

Kód UT WoS článku

000524972400004

EID výsledku v databázi Scopus

2-s2.0-85079366063