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
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
EH - Ecology - communities
OECD FORD branch
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Result continuities
Project
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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
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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
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