Pathway-dependent fate of permafrost region carbon

Permafrost soils in the high northern latitudes contain a substantial amount of carbon which is not decomposed due to frozen conditions. Climate change will lead to a thawing of at least part of the permafrost, implying that the stored carbon will become accessible to decomposition and be released t...

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Bibliographic Details
Published in:Environmental Research Letters
Main Authors: Thomas Kleinen, Victor Brovkin
Format: Article in Journal/Newspaper
Language:English
Published: IOP Publishing 2018
Subjects:
permafrost carbon
climate change
land surface modelling
carbon balance
CO2 fertilisation
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Science
Q
Physics
QC1-999
permafrost
Online Access:https://doi.org/10.1088/1748-9326/aad824
https://doaj.org/article/ad7d89a4a2df49698f0a08dfb0841987
Description
Summary:Permafrost soils in the high northern latitudes contain a substantial amount of carbon which is not decomposed due to frozen conditions. Climate change will lead to a thawing of at least part of the permafrost, implying that the stored carbon will become accessible to decomposition and be released to the atmosphere. We use a land surface model to quantify the amount of carbon released up until 2300 and determine the net carbon balance of the northern hemisphere permafrost region under climate warming following the RCP scenarios 2.6, 4.5, and 8.5. Here we show for the first time that the net carbon balance of the permafrost region is not just strongly dependent on the overall warming, but also on the CO _2 concentration pathway. As a result moderate warming scenarios may counterintuitively lead to lower net carbon emissions from the permafrost region than low warming scenarios.

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