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The role of climate-fuel feedbacks on Holocene biomass burning in upper- montane Carpathian forests

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985939%3A_____%2F20%3A00533898" target="_blank" >RIV/67985939:_____/20:00533898 - isvavai.cz</a>

  • Alternative codes found

    RIV/60460709:41320/20:84608 RIV/00216208:11310/20:10424479

  • Result on the web

    <a href="https://doi.org/10.1016/j.gloplacha.2020.103264" target="_blank" >https://doi.org/10.1016/j.gloplacha.2020.103264</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.gloplacha.2020.103264" target="_blank" >10.1016/j.gloplacha.2020.103264</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The role of climate-fuel feedbacks on Holocene biomass burning in upper- montane Carpathian forests

  • Original language description

    Over the past few decades, mean summer temperatures within the Carpathian Mountains have increased by as much as 2 °C leading to a projected increased forest fire risk. Currently, there are no paleofire records from the Western Carpathians that provide the long-term range of natural variability to contextualise the response of upper-montane forests to future environmental change and disturbance regimes. We present the first high-re- solution Holocene fire history record from the upper-montane ecotone from the High Tatra Mountains, Slovakia, as well as provide a regional synthesis of pan-Carpathian drivers of biomass burning in upper-montane forests. Our results illustrate that forest composition and density both greatly influence biomass burning, creating two different climate-fuel feedbacks. First, warmer conditions in the early Holocene, coupled with generally higher abundances of Pinus sp., either P. cembra and/or P. mugo/sylvestris, created a positive climate-fuel relationship that resulted in higher amounts of biomass burning. Second, cooler and wetter late Holocene conditions led to denser Picea abies upper-montane forests, creating a negative climate-fuel feedback that reduced biomass burning in upper-montane forests across the Carpathians. Given that warmer and drier conditions are expected across the entire Carpathian region in the future, our results illustrate how future climate change could po- tentially create a positive climate-fuel relationship within upper-montane forests dominated by Picea abies and Pinus cembra and/or P. mugo/sylvestris.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10611 - Plant sciences, botany

Result continuities

  • Project

    <a href="/en/project/GA16-06915S" target="_blank" >GA16-06915S: Holocene disturbance dynamics in European Picea abies (Norway spruce) forests: Implications for conservation and management</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2020

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Global and Planetary Change

  • ISSN

    0921-8181

  • e-ISSN

  • Volume of the periodical

    193

  • Issue of the periodical within the volume

    OCT 2020

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    17

  • Pages from-to

    1-17

  • UT code for WoS article

    000579856400007

  • EID of the result in the Scopus database

    2-s2.0-85087732734