Vše

Co hledáte?

Vše
Projekty
Výsledky výzkumu
Subjekty

Rychlé hledání

  • Projekty podpořené TA ČR
  • Významné projekty
  • Projekty s nejvyšší státní podporou
  • Aktuálně běžící projekty

Chytré vyhledávání

  • Takto najdu konkrétní +slovo
  • Takto z výsledků -slovo zcela vynechám
  • “Takto můžu najít celou frázi”

Forest regeneration within the treeline ecotone in the Giant Mountains under climate change

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F17%3A00485242" target="_blank" >RIV/86652079:_____/17:00485242 - isvavai.cz</a>

  • Výsledek na webu

  • DOI - Digital Object Identifier

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Forest regeneration within the treeline ecotone in the Giant Mountains under climate change

  • Popis výsledku v původním jazyce

    Natural regeneration of mountain spruce forests began in the Giant Mountains 25 years ago after a reductionnof severe and long-enduring air pollution. This process has been influenced by climatic change.nThe aim of our contribution was to present background data for the potential elevational shift of sprucenregeneration under conditions of climate change. These upslope shifts may also depend on constraintsnsuch as climate extremes, unfavourable soil conditions, absence of ectomycorrhizal symbionts, and lack ofnmicrosites suitable for seedlings. Since 2014, we have studied the main driving factors affecting Norwaynspruce regeneration, and in particular soil conditions, ectomycorrhizal symbionts, ground vegetation cover,nand forest health, in six transects across the treeline ecotone located on a NW-to-NE transect throughnthe Giant Mountains. Microclimatic measurements showed that the mean difference in growing seasonntemperature between the montane spruce forests and forests at the treeline was −0.54°C. The modelnHADGEM2 predicted that in 20 years the temperature at the treeline will be similar to the current one atnmontane elevations. The difference in prevailing soil types between the montane spruce forests and forestsnat the current treeline (i.e. podzol vs. ranker type) could be an important factor limiting success of thenupslope spreading of spruce. Furthermore, areas covered by microsites favourable for natural spruce regeneration,nespecially spruce litter patches, decaying wood, mosses, and Avenella flexuosa stands, werenshown to decrease with increasing elevation. It is likely that spruce will move upslope in response to climatenchange, but the process is likely to be slow or even blocked for some periods, especially by unfavourablensoil conditions and climatic extremes.

  • Název v anglickém jazyce

    Forest regeneration within the treeline ecotone in the Giant Mountains under climate change

  • Popis výsledku anglicky

    Natural regeneration of mountain spruce forests began in the Giant Mountains 25 years ago after a reductionnof severe and long-enduring air pollution. This process has been influenced by climatic change.nThe aim of our contribution was to present background data for the potential elevational shift of sprucenregeneration under conditions of climate change. These upslope shifts may also depend on constraintsnsuch as climate extremes, unfavourable soil conditions, absence of ectomycorrhizal symbionts, and lack ofnmicrosites suitable for seedlings. Since 2014, we have studied the main driving factors affecting Norwaynspruce regeneration, and in particular soil conditions, ectomycorrhizal symbionts, ground vegetation cover,nand forest health, in six transects across the treeline ecotone located on a NW-to-NE transect throughnthe Giant Mountains. Microclimatic measurements showed that the mean difference in growing seasonntemperature between the montane spruce forests and forests at the treeline was −0.54°C. The modelnHADGEM2 predicted that in 20 years the temperature at the treeline will be similar to the current one atnmontane elevations. The difference in prevailing soil types between the montane spruce forests and forestsnat the current treeline (i.e. podzol vs. ranker type) could be an important factor limiting success of thenupslope spreading of spruce. Furthermore, areas covered by microsites favourable for natural spruce regeneration,nespecially spruce litter patches, decaying wood, mosses, and Avenella flexuosa stands, werenshown to decrease with increasing elevation. It is likely that spruce will move upslope in response to climatenchange, but the process is likely to be slow or even blocked for some periods, especially by unfavourablensoil conditions and climatic extremes.

Klasifikace

  • Druh

    D - Stať ve sborníku

  • CEP obor

  • OECD FORD obor

    40102 - Forestry

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • Návaznosti

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2017

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název statě ve sborníku

    Quo vaditis agriculture, forestry and society under global change? Conference proceeding

  • ISBN

    978-80-87902-22-6

  • ISSN

  • e-ISSN

  • Počet stran výsledku

    5

  • Strana od-do

    86-90

  • Název nakladatele

    Global change research institute

  • Místo vydání

    Brno

  • Místo konání akce

    Velké Karlovice

  • Datum konání akce

    2. 10. 2017

  • Typ akce podle státní příslušnosti

    EUR - Evropská akce

  • Kód UT WoS článku