Detecting the permafrost carbon feedback: talik formation and increased cold-season respiration as precursors to sink-to-source transitions

Thaw and release of permafrost carbon (C) due to climate change is likely to offset increased vegetation C uptake in northern high-latitude (NHL) terrestrial ecosystems. Models project that this permafrost C feedback may act as a slow leak, in which case detection and attribution of the feedback may...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Parazoo, Nicholas C., Koven, Charles D., Lawrence, David M., Romanovsky, Vladimir, Miller, Charles E.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1435105
https://www.osti.gov/biblio/1435105
https://doi.org/10.5194/tc-12-123-2018