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
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DOI - Digital Object Identifier
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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
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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
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e-ISSN
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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
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