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Potential carbon emissions dominated by carbon dioxide from thawed permafrost soils

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F16%3A43890946" target="_blank" >RIV/60076658:12310/16:43890946 - isvavai.cz</a>

  • Result on the web

    <a href="http://www.nature.com/nclimate/journal/v6/n10/full/nclimate3054.html" target="_blank" >http://www.nature.com/nclimate/journal/v6/n10/full/nclimate3054.html</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1038/NCLIMATE3054" target="_blank" >10.1038/NCLIMATE3054</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Potential carbon emissions dominated by carbon dioxide from thawed permafrost soils

  • Original language description

    Increasing temperatures in northern high latitudes are causing permafrost to thaw(1), making large amounts of previously frozen organic matter vulnerable to microbial decomposition(2). Permafrost thaw also creates a fragmented landscape of drier and wetter soil conditions(3,4) that determine the amount and form (carbon dioxide (CO2), or methane (CH4)) of carbon (C) released to the atmosphere. The rate and form of C release control the magnitude of the permafrost C feedback, so their relative contribution with a warming climate remains unclear(5,6). We quantified the effect of increasing temperature and changes from aerobic to anaerobic soil conditions using 25 soil incubation studies from the permafrost zone. Here we show, using two separate meta-analyses, that a 10 degrees C increase in incubation temperature increased C release by a factor of 2.0 (95% confidence interval (CI), 1.8 to 2.2). Under aerobic incubation conditions, soils released 3.4 (95% CI, 2.2 to 5.2) times more C than under anaerobic conditions. Even when accounting for the higher heat trapping capacity of CH4, soils released 2.3 (95% CI, 1.5 to 3.4) times more C under aerobic conditions. These results imply that permafrost ecosystems thawing under aerobic conditions and releasing CO2 will strengthen the permafrost C feedback more than waterlogged systems releasing CO2 and CH4 for a given amount of C.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    EH - Ecology - communities

  • OECD FORD branch

Result continuities

  • Project

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2016

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Nature Climate Change

  • ISSN

    1758-678X

  • e-ISSN

  • Volume of the periodical

    6

  • Issue of the periodical within the volume

    10

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    4

  • Pages from-to

    950-953

  • UT code for WoS article

    000388292800019

  • EID of the result in the Scopus database