Počet záznamů: 1  

Climate control of terrestrial carbon exchange across biomes and continents

  1. 1.
    SYSNO ASEP0383149
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevClimate control of terrestrial carbon exchange across biomes and continents
    Tvůrce(i) Yi, C. (US)
    Ricciuto, D. (US)
    Marek, Michal V. (UEK-B) RID, ORCID, SAI
    Celkový počet autorů151
    Zdroj.dok.Environmental Research Letters. - : Institute of Physics Publishing - ISSN 1748-9326
    Roč. 5, č. 3 (2010), s. 034007
    Poč.str.16 s.
    Jazyk dok.eng - angličtina
    Země vyd.GB - Velká Británie
    Klíč. slovaNEE ; climate control ; terrestrial carbon sequestration ; temperature ; dryness ; eddy flux ; biomes ; photosynthesis ; respiration ; global carbon cycle
    Vědní obor RIVEH - Ekologie - společenstva
    CEZAV0Z60870520 - UEK-B (2005-2011)
    UT WOS000282273700008
    DOI10.1088/1748-9326/5/3/034007
    AnotaceUnderstanding the relationships between climate and carbon exchange by terrestrial ecosystems is critical to predict future levels of atmospheric carbon dioxide because of the potential accelerating effects of positive climate-carbon cycle feedbacks. However, directly observed relationships between climate and terrestrial CO2 exchange with the atmosphere across biomes and continents are lacking. Here we present data describing the relationships between net ecosystem exchange of carbon (NEE) and climate factors as measured using the eddy covariance method at 125 unique sites in various ecosystems over six continents with a total of 559 site-years. We find that NEE observed at eddy covariance sites is (1) a strong function of mean annual temperature at mid-and high-latitudes, (2) a strong function of dryness at mid-and low-latitudes, and (3) a function of both temperature and dryness around the mid-latitudinal belt (45 degrees N). The sensitivity of NEE to mean annual temperature breaks down at similar to 16 degrees C (a threshold value of mean annual temperature), above which no further increase of CO2 uptake with temperature was observed and dryness influence overrules temperature influence.
    PracovištěÚstav výzkumu globální změny
    KontaktNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Rok sběru2013
Počet záznamů: 1  

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