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Thermal characteristics of alpine treelines in Central Europe north of the Alps

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F16%3A10322449" target="_blank" >RIV/00216208:11310/16:10322449 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=TRN_De8HhA" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=TRN_De8HhA</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.3354/cr01370" target="_blank" >10.3354/cr01370</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Thermal characteristics of alpine treelines in Central Europe north of the Alps

  • Popis výsledku v původním jazyce

    Alpine treeline ecotones north of the Alps in Central Europe occur in 11 mountain ranges, including the Harz Mountains (Germany), mountain chains of the High Sudetes (Czech Republic and Poland) and the Western Carpathians (Czech Republic, Poland and Slovakia). These mountains are characterized by pronounced maritime-continental gradients, large differences in the mass elevation effect, and varying distance between the treeline and summits. We evaluated how these factors influence treeline temperatures and thus treeline elevation. We compared various treeline temperature metrics for all mountain ranges in the study region both among the mountain ranges and with treeline temperatures in the Alps. Our results show that treelines along the 50th parallel increase their elevation by approximately 94 m per 100 km towards the east, a reflection of a rise in elevation of isotherms of growing season temperatures along the maritime-continental gradient and with increasing mass elevation effect. Among the majority of evaluated mountain ranges, growing season treeline temperatures did not differ significantly, suggesting identical thermal limitation of tree growth in these ranges. However, we identified 4 regions (the Harz, Králický Sněžník, Hrubý Jeseník and Velká Fatra Mountains) where the uppermost tree stands are situated below the common treeline isotherm, an indication that trees are limited by other factors (e.g. biomass loss). Based on a comparison of various treeline temperature metrics, we suggest that to reliably describe treeline climates in regions with pronounced maritime-continental gradients, it is necessary to use metrics capturing the entire growing season. Such metrics show that treeline temperatures in the study region are similar to those in the Alps.

  • Název v anglickém jazyce

    Thermal characteristics of alpine treelines in Central Europe north of the Alps

  • Popis výsledku anglicky

    Alpine treeline ecotones north of the Alps in Central Europe occur in 11 mountain ranges, including the Harz Mountains (Germany), mountain chains of the High Sudetes (Czech Republic and Poland) and the Western Carpathians (Czech Republic, Poland and Slovakia). These mountains are characterized by pronounced maritime-continental gradients, large differences in the mass elevation effect, and varying distance between the treeline and summits. We evaluated how these factors influence treeline temperatures and thus treeline elevation. We compared various treeline temperature metrics for all mountain ranges in the study region both among the mountain ranges and with treeline temperatures in the Alps. Our results show that treelines along the 50th parallel increase their elevation by approximately 94 m per 100 km towards the east, a reflection of a rise in elevation of isotherms of growing season temperatures along the maritime-continental gradient and with increasing mass elevation effect. Among the majority of evaluated mountain ranges, growing season treeline temperatures did not differ significantly, suggesting identical thermal limitation of tree growth in these ranges. However, we identified 4 regions (the Harz, Králický Sněžník, Hrubý Jeseník and Velká Fatra Mountains) where the uppermost tree stands are situated below the common treeline isotherm, an indication that trees are limited by other factors (e.g. biomass loss). Based on a comparison of various treeline temperature metrics, we suggest that to reliably describe treeline climates in regions with pronounced maritime-continental gradients, it is necessary to use metrics capturing the entire growing season. Such metrics show that treeline temperatures in the study region are similar to those in the Alps.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10508 - Physical geography

Návaznosti výsledku

  • Projekt

  • Návaznosti

    S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2016

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    Climate Research

  • ISSN

    0936-577X

  • e-ISSN

  • Svazek periodika

    68

  • Číslo periodika v rámci svazku

    1

  • Stát vydavatele periodika

    DE - Spolková republika Německo

  • Počet stran výsledku

    12

  • Strana od-do

    1-12

  • Kód UT WoS článku

    000376370600001

  • EID výsledku v databázi Scopus

    2-s2.0-84964053393