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”

Shrubs shed light on 20th century Greenland Ice Sheet melting

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F70883521%3A28160%2F17%3A63516822" target="_blank" >RIV/70883521:28160/17:63516822 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/60460709:41320/17:75632

  • Výsledek na webu

    <a href="http://dx.doi.org/10.1111/bor.12244" target="_blank" >http://dx.doi.org/10.1111/bor.12244</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1111/bor.12244" target="_blank" >10.1111/bor.12244</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Shrubs shed light on 20th century Greenland Ice Sheet melting

  • Popis výsledku v původním jazyce

    The Greenland Ice Sheet (GrIS) is a key element of the global climate system and thus knowledge about its melting in the past is desirable. However, GrIS-melt records only date back until 1979 and climate data based reconstructions covering the 20th century differ with respect to absolute values. To extend our knowledge about the Greenland Ice Sheet we examined the potential of shrub ring-widths and wood-anatomy as proxies for GrIS-melt. We found significant correlations between shrub cell-wall thickness and regional melt derived from passive microwave satellite brightness for 7% of the total GrIS area. A respective transfer function calibrated over the period 1979 to 2007 successfully passed model calibration-verification tests and explained 42% of GrIS-melt variability. Consequently, the first GrIS-melt reconstruction based on shrub wood-anatomy covering the period 1909 to 2012 is presented and compared against two temperature-based reconstructions. For the period prior to 1930 the new reconstruction contrasts with existing literature but generally confirms that most recent record melt rates are amongst the highest since the early 20th century. We discuss the sensitivity of shrubs to several influencing factors besides summer temperature as possible reason for the observed differences and highlight the potential of using shrubs as multi-parameter proxies within a network to increase our knowledge about 20th century Greenland Ice Sheet dynamics.

  • Název v anglickém jazyce

    Shrubs shed light on 20th century Greenland Ice Sheet melting

  • Popis výsledku anglicky

    The Greenland Ice Sheet (GrIS) is a key element of the global climate system and thus knowledge about its melting in the past is desirable. However, GrIS-melt records only date back until 1979 and climate data based reconstructions covering the 20th century differ with respect to absolute values. To extend our knowledge about the Greenland Ice Sheet we examined the potential of shrub ring-widths and wood-anatomy as proxies for GrIS-melt. We found significant correlations between shrub cell-wall thickness and regional melt derived from passive microwave satellite brightness for 7% of the total GrIS area. A respective transfer function calibrated over the period 1979 to 2007 successfully passed model calibration-verification tests and explained 42% of GrIS-melt variability. Consequently, the first GrIS-melt reconstruction based on shrub wood-anatomy covering the period 1909 to 2012 is presented and compared against two temperature-based reconstructions. For the period prior to 1930 the new reconstruction contrasts with existing literature but generally confirms that most recent record melt rates are amongst the highest since the early 20th century. We discuss the sensitivity of shrubs to several influencing factors besides summer temperature as possible reason for the observed differences and highlight the potential of using shrubs as multi-parameter proxies within a network to increase our knowledge about 20th century Greenland Ice Sheet dynamics.

Klasifikace

  • Druh

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

  • CEP obor

  • OECD FORD obor

    10511 - Environmental sciences (social aspects to be 5.7)

Návaznosti výsledku

  • Projekt

  • Návaznosti

    V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

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 periodika

    Boreas: an international journal of quaternary research

  • ISSN

    0300-9483

  • e-ISSN

  • Svazek periodika

    46

  • Číslo periodika v rámci svazku

    4

  • Stát vydavatele periodika

    US - Spojené státy americké

  • Počet stran výsledku

    11

  • Strana od-do

    667-677

  • Kód UT WoS článku

    000412097800005

  • EID výsledku v databázi Scopus