Evidence for non-steady-state carbon emissions from snow-scoured alpine tundra

High-latitude warming is capable of accelerating permafrost degradation and the decomposition of previously frozen carbon. The existence of an analogous high-altitude feedback, however, has yet to be directly evaluated. We address this knowledge gap by coupling a radiocarbon-based model to 7 years (...

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Detalles Bibliográficos
Autores principales: Knowles, John F., Blanken, Peter D., Lawrence, Corey R., Williams, Mark W.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6428862/
https://www.ncbi.nlm.nih.gov/pubmed/30898997
http://dx.doi.org/10.1038/s41467-019-09149-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6428862/
https://www.ncbi.nlm.nih.gov/pubmed/30898997
http://dx.doi.org/10.1038/s41467-019-09149-2

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