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”

Climate change in Arctic terrestrial ecosystems with particular attention to the vegetation of Svalbard

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F25%3A43928201" target="_blank" >RIV/62156489:43410/25:43928201 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/00216224:14310/25:00143504

  • Výsledek na webu

    <a href="https://doi.org/10.5817/CPR2025-S-5" target="_blank" >https://doi.org/10.5817/CPR2025-S-5</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5817/CPR2025-S-5" target="_blank" >10.5817/CPR2025-S-5</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Climate change in Arctic terrestrial ecosystems with particular attention to the vegetation of Svalbard

  • Popis výsledku v původním jazyce

    In the last four decades, warming in the Arctic has been much faster than in the rest of the World. The average air temperature in the Arctic has already risen at a rate of almost four times the global average. On average, the Arctic is now approximately 3 degrees C warmer than it was in 1980. Different Arctic regions - Svalbard in particular - warm faster than any other region on Earth. Such warming has consequences for terrestrial ecosystems. Since plant growth and development are closely linked to the temperature of spring and summer, the early onset of vegetation is one of the most remarkable consequences. Moreover, recent evidence from satellite data suggests there is a temperature-induced increase in growth rate and biomass production of Svalbard vegetation; plant species that dominate the tundra communities are growing taller and more densely. In this chapter, we present an analysis of climatic characteristics recorded at the Adventdalen weather station (operated by The University Centre in Svalbard) with particular attention to vegetation cover. In Adventdalen, community types form five groups of vegetation: (a) sparsely vegetated areas on dry subsoil, (b) sparsely vegetated areas on moist substrate, (c) densely vegetated areas on dry substrate, (d) densely vegetated areas on substrate and (e) areas of organic material. The period of 2011-2020 was analysed, and relations between climatic drivers were evaluated. The presented data support the idea of fast ongoing warming of the Svalbard terrestrial ecosystems.

  • Název v anglickém jazyce

    Climate change in Arctic terrestrial ecosystems with particular attention to the vegetation of Svalbard

  • Popis výsledku anglicky

    In the last four decades, warming in the Arctic has been much faster than in the rest of the World. The average air temperature in the Arctic has already risen at a rate of almost four times the global average. On average, the Arctic is now approximately 3 degrees C warmer than it was in 1980. Different Arctic regions - Svalbard in particular - warm faster than any other region on Earth. Such warming has consequences for terrestrial ecosystems. Since plant growth and development are closely linked to the temperature of spring and summer, the early onset of vegetation is one of the most remarkable consequences. Moreover, recent evidence from satellite data suggests there is a temperature-induced increase in growth rate and biomass production of Svalbard vegetation; plant species that dominate the tundra communities are growing taller and more densely. In this chapter, we present an analysis of climatic characteristics recorded at the Adventdalen weather station (operated by The University Centre in Svalbard) with particular attention to vegetation cover. In Adventdalen, community types form five groups of vegetation: (a) sparsely vegetated areas on dry subsoil, (b) sparsely vegetated areas on moist substrate, (c) densely vegetated areas on dry substrate, (d) densely vegetated areas on substrate and (e) areas of organic material. The period of 2011-2020 was analysed, and relations between climatic drivers were evaluated. The presented data support the idea of fast ongoing warming of the Svalbard terrestrial ecosystems.

Klasifikace

  • Druh

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

  • CEP obor

  • OECD FORD obor

    10618 - Ecology

Návaznosti výsledku

  • Projekt

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    Czech Polar Reports

  • ISSN

    1805-0689

  • e-ISSN

    1805-0697

  • Svazek periodika

    15

  • Číslo periodika v rámci svazku

    S

  • Stát vydavatele periodika

    CZ - Česká republika

  • Počet stran výsledku

    16

  • Strana od-do

    94-109

  • Kód UT WoS článku

    001656303100005

  • EID výsledku v databázi Scopus