Controls of soil organic matter on soil thermal dynamics in the northern high latitudes

Permafrost warming and potential soil carbon (SOC) release after thawing may amplify climate change, yet model estimates of present-day and future permafrost extent vary widely, partly due to uncertainties in simulated soil temperature. Here, we derive thermal diffusivity, a key parameter in the soi...

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Detalles Bibliográficos
Autores principales: Zhu, Dan, Ciais, Philippe, Krinner, Gerhard, Maignan, Fabienne, Jornet Puig, Albert, Hugelius, Gustaf
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/PMC6639258/
https://www.ncbi.nlm.nih.gov/pubmed/31320647
http://dx.doi.org/10.1038/s41467-019-11103-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6639258/
https://www.ncbi.nlm.nih.gov/pubmed/31320647
http://dx.doi.org/10.1038/s41467-019-11103-1

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