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Permafrost carbon−climate feedback is sensitive to deep soil carbon decomposability but not deep soil nitrogen dynamics

Permafrost soils contain enormous amounts of organic carbon whose stability is contingent on remaining frozen. With future warming, these soils may release carbon to the atmosphere and act as a positive feedback to climate change. Significant uncertainty remains on the postthaw carbon dynamics of pe...

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Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Proc Natl Acad Sci U S A
Prif Awduron: Koven, Charles D., Lawrence, David M., Riley, William J.
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: National Academy of Sciences 2015
Pynciau:
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC4378430/
https://ncbi.nlm.nih.gov/pubmed/25775603
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1415123112
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